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Sample records for cape breton highlands

  1. The spatial and seasonal variation of nitrogen dioxide and sulfur dioxide in Cape Breton Highlands National Park, Canada, and the association with lichen abundance

    NASA Astrophysics Data System (ADS)

    Gibson, Mark D.; Heal, Mathew R.; Li, Zhengyan; Kuchta, James; King, Gavin H.; Hayes, Alex; Lambert, Sheldon

    2013-01-01

    Over 200,000 tourists per year visit Cape Breton Highlands National Park, Nova Scotia, Canada. The forests within the park are home to many rare epiphytic lichens, the species diversity of which has declined in some areas. The primary motivation for this study was to gain insight into the concentrations and potential local and long-range sources of air pollution, but its association with lichen species diversity was also examined. Ogawa passive diffusion samplers were used to measure nitrogen dioxide (NO2) and sulfur dioxide (SO2) in the park at 19 sites in the winter and 20 sites in the summer of 2011. An improvement in the sensitivity of the sampler analytical protocol was developed. The mean concentrations in the park of winter and summer NO2 (0.81 and 0.16 ppb) and SO2 (0.24 and 0.21 ppb) are not at levels known to be phytotoxic to lichen. The NO2 concentrations in winter were significantly (p = 0.001) higher than those in summer whilst the SO2 concentrations did not differ significantly between winter and summer (p = 0.429). Highest NO2 concentrations in both seasons were observed in the Grand Anse Valley, presumably due to the steep road, emissions from the Pleasant Bay community at the foot of the valley and the enclosed topography of this area reducing dispersion of primary emissions. The SO2 concentrations in the park tended to be greater at elevated sites than valley sites, consistent with dispersion from long-range, rather than local, sources for this pollutant. Significant predictors in a multilinear regression for an index of air purity (lichen based measure of air quality) were lichen species number (p = 0.009), forest old growth index (p = 0.001) and distance from roads (p < 0.001) (model R2 = 0.8, model p = 0.004). The study suggests that local sources of pollution (roads emissions) are adversely associated with lichen species diversity in this National Park, compared with long-range transport, and that monitoring programs such as a lichen

  2. First record of Anguillicoloides crassus (Nematoda) in American eels (Anguilla rostrata) in Canadian estuaries, Cape Breton, Nova Scotia.

    PubMed

    Rockwell, L S; Jones, K M M; Cone, D K

    2009-04-01

    In the summer of 2007, American eels, Anguilla rostrata, from 2 localities on Cape Breton Island, were found to be infected with the swim bladder nematode Anguillicoloides crassus. This is the first documented report of this highly invasive parasite in Canadian waters. More than half of the yellow eels in Mira River (6 of 10), and 1 eel (of 5) from Sydney Harbour were infected. Parasite intensity ranged from 1 to 11 worms per eel. The occurrence of A. crassus at these 2 localities suggests the need for a more extensive survey on the distribution of this exotic parasite in eel populations throughout Cape Breton Island. PMID:18767906

  3. Tectono-stratigraphic terranes in Cape Breton Island, Nova Scotia: Implications for the configuration of the northern Appalachian orogen

    SciTech Connect

    Barr, S.M.; Raeside, R.P. )

    1989-09-01

    Cape Breton Island is divided into four terranes on the basis of contrasts in pre-Carboniferous geology. The Blair River Complex in the north is an exposure of North American Grenvillian basement, analogous to the Humber zone basement in Newfoundland. Ordovician to Devonian metavolcanic, metasedimentary, gneissic, and granitic rocks of the Aspy terrane are correlative with parts of the Gander terrane of Newfoundland and New Brunswick. The Bras d'Or terrane, characterized by low-pressure gneisses, a carbonate-clastic platform sequence, and later Precambrian-Early Cambrian plutons, may be correlative with units previously included in the Gander terrane in southern Newfoundland and the Avalon terrane in southern New Brunswick. The Mira terrane in southeastern Cape Breton Island, including late Precambrian to Early Cambrian volcanic and sedimentary sequences and fossiliferous Cambrian-Ordovician units, is clearly part of the Avalon terrane. Therefore, with the exception of the Dunnage terrane, which is not represented in Cape Breton Island, the terranes of Newfoundland continue through Cape Breton Island. They are offset to the northwest to the mainland part of the Appalachian orogen in New Brunswick.

  4. Career Decision Making in the Shadow of Economic Downturn: A Study of Cape Breton High School Students.

    ERIC Educational Resources Information Center

    Chisholm, Joe; Edmunds, Alan

    2001-01-01

    Examines differences in levels of career decision-making self-efficacy in Cape Breton high school students who lived in communities with recent closures of mining and steel industries compared to students from communities with no such closures. Students demonstrated considerable confidence in their career decision-making abilities implying that…

  5. Paleomagnetic Progress in Peri-Gondwanan Terranes of Cape Breton Island, Nova Scotia

    NASA Astrophysics Data System (ADS)

    Grunow, A. M.; Thompson, M. D.; Barr, S. M.; White, C. E.

    2009-05-01

    Paleopoles from primary Ediacaran magnetization directions established the Gondwanan origin of northern Appalachian Avalonian terranes, but magnetic overprints in the same rocks also provide useful tectonic information. Thus, in the Southeastern New England Avalon Zone, virtual geomagnetic poles (VGPs) calculated from magnetic B and C components in both 595 Ma Lynn-Mattapan volcanic rocks and 490-488 Ma Nahant Gabbro track mid- and late Paleozoic segments of the North American apparent polar wander path (APWP), suggesting the influence of Acadian and Neo-Acadian accretionary events. We report here on multi- vectorial magnetizations in pilot samples from Cape Breton Island, Nova Scotia where the Bras d'Or and Mira terranes represent both Ganderian and Avalonian elements transferred from Gondwana. Overprint relationships in these terranes may constrain their amalgamation with each other as well their docking with Laurentia. As in southeastern New England, secondary remanences can be identified in Cape Breton Island as consistent magnetization directions in rocks of differing ages. The S- to SSE-trending and gently downward pointing direction reported in 1985 by Johnson and Van der Voo in Middle Cambrian sedimentary rocks of the Bourinot Group (Bras d'Or terrane), for example, is also present in the 563 Ma Main à Dieu Formation and in 620 Ma Chisholm Brook Granite and East Bay Hill rhyolite (Mira terrane). This magnetization represents the C component already found around Boston, MA. The resulting VGPs in both areas occupy positions on the North American APWP consistent with a Neo-Acadian overprint, possibly related to the docking of the Meguma terrane against previously accreted Avalonia. Other overprint directions encountered in this investigation give rise to VGPs that do not coincide with the North American APWP, hence appear to reflect tectonic events independent of Laurentia. One such cluster comprising both Mira and Bras d'Or VGPs includes the paleopole also

  6. U-Pb zircon date from Avalonian Cape Breton Island and geochronologic calibration of the early Ordovician

    USGS Publications Warehouse

    Landing, E.; Bowring, S.A.; Fortey, R.A.; Davidek, K.L.

    1997-01-01

    A U-Pb zircon date of 483 + 1 Ma is recorded from an uppermost Tremadoc K-bentonite from the Chesley Drive Group on McLeod Brook, eastern Cape Breton Island. The associated fauna, with the trilobite Peltocare rotundifrons, is also known from the Reversing Falls section in Saint John, New Brunswick, and the traditional reference of the latter section to the Arenig is incorrect. A 483 + 1 Ma age is significantly older than a U-Pb zircon age reported from the classical base of the Arenig Series in north Wales and about 10 Ma older than strata regarded herein as upper Arenig in central Newfoundland. If the global standard for the base of the Arenig is defined at the Tetragraptus approximatus Zone base, then the base of the type Arenig in Wales is younger than the latter horizon. The McLeod Brook occurrence is from an uppermost Tremadoc (Hunnebergian Stage) interval that has been removed below the unconformity in north Wales. The age of the Tremadoc-Arenig series boundary remains uncertain; however, a tentative estimate that it is significantly younger than 483 Ma is suggested by fossil evidence.

  7. Pb and O isotopic constraints on the source of granitic rocks from Cape Breton Island, Nova Scotia, Canada

    USGS Publications Warehouse

    Ayuso, R.A.; Barr, S.M.; Longstaffe, F.J.

    1996-01-01

    Pb isotopic compositions of leached feldspars from twenty-three plutons in Cape Breton Island can be divided into two groups: anorthosite, syenite, and granite in the Blair River Complex, which have the least radiogenic compositions on the Island, and granitic rocks from terranes (Aspy, Bras d'Or, and Mira) to the south. Pb isotopic data for the Blair River Complex (206Pb/204Pb = 17.399-18.107; 207Pb/204Pb = 15.505-15.560; 208Pb/204Pb = 36.689-37.733) are consistent with an old source region ultimately derived from the mantle and contaminated by sialic crust. Oxygen isotopic compositions of syenite in the Blair River Complex (??18O = +8.0 to +8.5 permil) are slightly higher than anorthosite (+7.0 to +8.3 permil); a Silurian granite in the Blair River Complex has ??18O = +7.5 permil. Cambrian to Devonian plutons in the Aspy, Bras d'Or, and Mira terranes are more radiogenic (206Pb/204Pb = 18.192-18.981; 207Pb/204Pb = 15.574-15.712; 208Pb/ 204Pb =37.815-38.936) than the Blair River Complex and were generated from source regions having a predominant crustal Pb signature (high ??). The ??18O values of granites and granodiorites in the Aspy terrane (+7.5 to +9.2 permil; avg = +8.6 permil) and Bras d'Or (+3.7 to +11.3 permil; avg = +9.4 permil) are also consistent with involvement of sialic crust. Many Late Proterozoic granites from the Mira terrane have anomalously low ??18O values (+0.2 to +5.9 permil), perhaps produced from protoliths that had undergone hydrothermal alteration prior to melting. Paleozoic granitic rocks from the Aspy, Bras d'Or, and Mira terranes cannot be uniquely distinguished on the basis of their Pb and O isotopic compositions. The granitic rocks could have been generated during terrane amalgamation from combinations of unradiogenic (Grenville-like) and more radiogenic (Avalon-like) sources.

  8. Changing Breton Responses to Death.

    ERIC Educational Resources Information Center

    Badone, Ellen

    1988-01-01

    Based on fieldwork conducted in Brittany, France, during 1983 and 1984, discusses changes in Breton responses to death which have accompanied modernization and economic development. Suggests that familiarity with death and acceptance of it are being replaced by the "denial of death" characteristic of contemporary Western culture. Notes parallel…

  9. Broadcast Media in Breton: Dawn at Last?

    ERIC Educational Resources Information Center

    Moal, Stefan

    2000-01-01

    Discusses to what extent the broadcast media in the Breton language has acted as a vital link to language maintenance in Brittany. Highlights the background context of the Breton language, reasons for its decline, and what the broadcast media can do to help reverse language shift. (Author/VWL)

  10. Neurology and surrealism: André Breton and Joseph Babinski.

    PubMed

    Haan, Joost; Koehler, Peter J; Bogousslavsky, Julien

    2012-12-01

    Before he became the initiator of the surrealist movement, André Breton (1896-1966) studied medicine and worked as a student in several hospitals and as a stretcher bearer at the front during World War I. There he became interested in psychiatric diseases such as hysteria and psychosis, which later served as a source of inspiration for his surrealist writings and thoughts, in particular on automatic writing. Breton worked under Joseph Babinski at La Pitié, nearby La Salpêtrière, and became impressed by the 'sacred fever' of the famous neurologist. In this article, we describe the relationship between Breton and Babinski and try to trace back whether not only Breton's psychiatric, but also his neurological experiences, have influenced surrealism. We hypothesize that Breton left medicine in 1920 partly as a consequence of his stay with Babinski. PMID:22685227

  11. Death of a Language, Birth of an Identity: Brittany and the Bretons.

    ERIC Educational Resources Information Center

    Jones, Mari C.

    1998-01-01

    Discusses the language situation in the region of Brittany in France, where the Breton language, a Celtic rather than Romance language, is dying out but a Breton ethnic identity is growing. (Author/JL)

  12. Cape Verde.

    PubMed

    1986-10-01

    This summary background paper for the Cape Verde Islands, by the U.S. State Department, includes geography, people, history, government, politics, economy and foreign relations. Cape Verde, located 650 km west of Senegal, has 10 volcanic islands inhabited by 339,000 people of combined African and Portuguese descent. The annual growth rate is 1.4%, although numbers of Cape Verdeans emigrate or work abroad. Per capita income is about $350; resources include volcanic rock, fish, salt, ship repair and light industry, subsistence and tropical agricultural products, although there has been a drought since 1968. Cape Verde has been independent since 1975. There is one political party, and a constitutional government. The country is nonaligned, and is on good terms with many other nations, accepting foreign aid from several sources. A significant proportion of the GNP derives from Cape Verde nationals working abroad.

  13. Archive of bathymetry and backscatter data collected in 2014 nearshore Breton and Gosier Islands, Breton National Wildlife Refuge, Louisiana

    USGS Publications Warehouse

    DeWitt, Nancy T.; Fredericks, Jake J.; Flocks, James G.; Miselis, Jennifer L.; Locker, Stanley D.; Kindinger, Jack G.; Bernier, Julie C.; Kelso, Kyle W.; Reynolds, Billy J.; Wiese, Dana S.; Browning, Trevor

    2016-08-01

    As part of the Barrier Island Monitoring Project, scientists from the U.S. Geological Survey (USGS) St. Petersburg Coastal and Marine Science Center conducted nearshore geophysical surveys off Breton and Gosier Islands, Louisiana, in July and August of 2014. To assist the United States Fish and Wildlife Service (USFWS) with restoration planning efforts, the USGS was tasked with answering fundamental questions about the physical environment of the southern Chandeleur Islands, including the geology, morphology, and oceanography. Baseline data needed to answer these questions were either insufficient or missing. The USGS conducted a comprehensive geologic investigation in the summer of 2014, collecting geophysical and sedimentological data.Breton Island, located at the southern end of the Chandeleur Island chain in southeastern Louisiana, was recognized as a natural, globally significant nesting sanctuary for several bird species and was established as the Breton National Wildlife Refuge (NWR) in 1904. The areal extent of Breton Island has diminished 90 percent since 1920. Land loss is attributed to ongoing relative sea-level rise, diminished sediment supply, and storm impacts. The bird population on Breton Island has also declined over the years, most notably after Hurricane George in 1998 and after Hurricane Katrina in 2015; the latter completely submerged the island. Despite decreasing habitable acreage, migratory seabirds continue to return and nest on Breton Island. To prevent the island from being submerged in the future, and to protect, stabilize, and provide more nesting and foraging areas for the bird population, the USFWS proposed a restoration effort to rebuild Breton Island to its pre-Katrina footprint.This data series serves as an archive of processed interferometric swath and single-beam bathymetry data, and side-scan sonar data, collected in the nearshore of Breton and Gosier Islands, NWR, Louisiana. The data were collected during two USGS cruises (USGS

  14. Archive of bathymetry and backscatter data collected in 2014 nearshore Breton and Gosier Islands, Breton National Wildlife Refuge, Louisiana

    USGS Publications Warehouse

    DeWitt, Nancy T.; Fredericks, Jake J.; Flocks, James G.; Miselis, Jennifer L.; Locker, Stanley D.; Kindinger, Jack G.; Bernier, Julie C.; Kelso, Kyle W.; Reynolds, Billy J.; Wiese, Dana S.; Browning, Trevor

    2016-01-01

    As part of the Barrier Island Monitoring Project, scientists from the U.S. Geological Survey (USGS) St. Petersburg Coastal and Marine Science Center conducted nearshore geophysical surveys off Breton and Gosier Islands, Louisiana, in July and August of 2014. To assist the United States Fish and Wildlife Service (USFWS) with restoration planning efforts, the USGS was tasked with answering fundamental questions about the physical environment of the southern Chandeleur Islands, including the geology, morphology, and oceanography. Baseline data needed to answer these questions were either insufficient or missing. The USGS conducted a comprehensive geologic investigation in the summer of 2014, collecting geophysical and sedimentological data.Breton Island, located at the southern end of the Chandeleur Island chain in southeastern Louisiana, was recognized as a natural, globally significant nesting sanctuary for several bird species and was established as the Breton National Wildlife Refuge (NWR) in 1904. The areal extent of Breton Island has diminished 90 percent since 1920. Land loss is attributed to ongoing relative sea-level rise, diminished sediment supply, and storm impacts. The bird population on Breton Island has also declined over the years, most notably after Hurricane George in 1998 and after Hurricane Katrina in 2015; the latter completely submerged the island. Despite decreasing habitable acreage, migratory seabirds continue to return and nest on Breton Island. To prevent the island from being submerged in the future, and to protect, stabilize, and provide more nesting and foraging areas for the bird population, the USFWS proposed a restoration effort to rebuild Breton Island to its pre-Katrina footprint.This data series serves as an archive of processed interferometric swath and single-beam bathymetry data, and side-scan sonar data, collected in the nearshore of Breton and Gosier Islands, NWR, Louisiana. The data were collected during two USGS cruises (USGS

  15. Cape Cod

    Atmospheric Science Data Center

    2014-05-15

    ... Image Cape Cod extends over 50 miles into the Atlantic Ocean. Its rugged coastline, dangerous sand bars and rip tides, and ever ... over the land and "puffy" cumulus clouds are over the ocean. The effects of the warm ocean water are evident in the lack of snow near ...

  16. Cape Verde

    NASA Technical Reports Server (NTRS)

    2007-01-01

    This Mars Exploration Rover Opportunity Pancam 'super resolution' mosaic of the approximately 6 m (20 foot) high cliff face of the Cape Verde promontory was taken by the rover from inside Victoria Crater, during the rover's descent into Duck Bay. Super-resolution is an imaging technique which utilizes information from multiple pictures of the same target in order to generate an image with a higher resolution than any of the individual images. Cape Verde is a geologically rich outcrop and is teaching scientists about how rocks at Victoria crater were modified since they were deposited long ago. This image complements super resolution mosaics obtained at Cape St. Mary and Cape St. Vincent and is consistent with the hypothesis that Victoria crater is located in the middle of what used to be an ancient sand dune field. Many rover team scientists are hoping to be able to eventually drive the rover closer to these layered rocks in the hopes of measuring their chemistry and mineralogy.

    This is a Mars Exploration Rover Opportunity Panoramic Camera image mosaic acquired on sols 1342 and 1356 (November 2 and 17, 2007), and was constructed from a mathematical combination of 64 different blue filter (480 nm) images.

  17. I Remember Highlander

    ERIC Educational Resources Information Center

    Williams-Hawkins, Maria

    2016-01-01

    "I Remember Highlander" reflects on the life choices of Marion Barry and Herman Henning Jr., fraternity brothers who sought the same goal but took different paths. The essay examines cultural and family situations that shaped lives and decisions.

  18. Analysis of seafloor change at Breton Island, Gosier Shoals, and surrounding waters, 1869–2014, Breton National Wildlife Refuge, Louisiana

    USGS Publications Warehouse

    Flocks, James G.; Terrano, Joseph F.

    2016-08-01

    Characterizing bathymetric change in coastal environments is an important component in understanding shoreline evolution, especially along barrier island platforms. Bathymetric change is a function of the regional sediment budget, long-term wave and current patterns, and episodic impact from high-energy events such as storms. Human modifications may also cause changes in seafloor elevation. This study, conducted by the U.S. Geological Survey in collaboration with the U.S. Fish and Wildlife Service, evaluates bathymetric and volumetric change and sediment characteristics around Breton Island and Gosier Shoals located offshore of the Mississippi River Delta in Louisiana. This area has been affected by significant storm events such as Hurricane Katrina in 2005. Sedimentation patterns at Breton Island and offshore have also been modified by the excavation of a shipping channel north of the island. Four time periods are considered that encompass these episodes and include long-term change and short-term storm recovery: 1869–2014, 1869–1920, 1920–2014, and 2007–2014. Finally, sediment characteristics are reported in the context of seafloor elevation.

  19. Stratigraphy and morphology of the barrier platform of Breton Island, Louisiana: deltaic, marine and human influences

    USGS Publications Warehouse

    Flocks, James G.; Kindinger, Jack G.; Miselis, Jennifer L.; Locker, Stanley D.

    2015-01-01

    Breton Island, located at the southern end of the Chandeleur Islands, Louisiana, is part of the Breton National Wildlife Refuge (NWR). Breton NWR is recognized as an important bird habitat and is host to one of Louisiana's largest historical brown pelican nesting colonies. Loss of island area through relative sea-level rise, storm impact, and impeded and diminishing sediment supply is reducing the available habitat, and restoration is necessary if the island is to remain emergent. Physical investigation of the Breton Island platform has provided new insight into the geologic framework. The data reveal a complex system that is undergoing both long-term and short-term change. Results of the study help to resolve uncertainties in island evolution and will assist in effective restoration of the island.

  20. Cape fearless.

    PubMed

    1998-01-01

    This article describes the Ilita Labantu (IL) group in South Africa, that is working to reduce child abuse and violence against women. The group started in 1989, with the aim of reducing child rape and sexual assaults in five townships in Cape Town. Child rape is perpetuated by myths sustained by witch doctors and indigenous medicine that promote child rape as a cure-all for symptoms ranging from poverty to AIDS. IL has four satellite groups that educate rape and abuse victims and potential victims. It is assumed that girls are potential victims because of their early unawareness that gender is tied to some patterns of behavior. IL trained mass media groups to educate the general public. IL distributes public information materials on how to identify domestic violence and abuse and how to identify potential rapists within households. Materials are distributed to individuals in community programs and in training programs. Child survivors make presentations in playgroups in a nonthreatening way. IL interacts with courts of law, police stations, hospitals, and schools. The group refers 25-35 cases per day. The group is working on setting up private rooms in police stations where rape victims can make confidential complaints without public attention. IL also works to promote the use of alternative strategies for solving family conflicts.

  1. The Ozark Highlands

    USGS Publications Warehouse

    Ethridge, Max

    2009-01-01

    The Ozark Highlands include diverse topographic, geologic, soil, and hydrologic conditions that support a broad range of habitat types. The landscape features rugged uplands - some peaks higher than 2,500 feet above sea level - with exposed rock and varying soil depths and includes extensive areas of karst terrain. The Highlands are characterized by extreme biological diversity and high endemism (uniqueness of species). Vegetation communities are dominated by open oak-hickory and shortleaf pine woodlands and forests. Included in this vegetation matrix is an assemblage of various types of fens, forests, wetlands, fluvial features, and carbonate and siliceous glades. An ever-growing human population in the Ozark Highlands has become very dependent on reservoirs constructed on major rivers in the region and, in some cases, groundwater for household and public water supply. Because of human population growth in the Highlands and increases in industrial and agricultural activities, not only is adequate water quantity an issue, but maintaining good water quality is also a challenge. Point and nonpoint sources of excessive nutrients are an issue. U.S. Geological Survey (USGS) partnership programs to monitor water quality and develop simulation tools to help stakeholders better understand strategies to protect the quality of water and the environment are extremely important. The USGS collects relevant data, conducts interpretive studies, and develops simulation tools to help stakeholders understand resource availability and sustainability issues. Stakeholders dependent on these resources are interested in and benefit greatly from evolving these simulation tools (models) into decision support systems that can be used for adaptive management of water and ecological resources. The interaction of unique and high-quality biological and hydrologic resources and the effects of stresses from human activities can be evaluated best by using a multidisciplinary approach that the USGS

  2. The Cape element in the Afrotemperate flora: from Cape to Cairo?

    PubMed

    Galley, Chloe; Bytebier, Benny; Bellstedt, Dirk U; Linder, H Peter

    2007-02-22

    The build-up of biodiversity is the result of immigration and in situ speciation. We investigate these two processes for four lineages (Disa, Irideae p.p., the Pentaschistis clade and Restionaceae) that are widespread in the Afrotemperate flora. These four lineages may be representative of the numerous clades which are species rich in the Cape and also occur in the highlands of tropical Africa. It is as yet unclear in which direction the lineages spread. Three hypotheses have been proposed: (i) a tropical origin with a southward migration towards the Cape, (ii) a Cape origin with a northward migration into tropical Africa, and (iii) vicariance. None of these hypotheses has been thoroughly tested. We reconstruct the historical biogeography of the four lineages using likelihood optimization onto molecular phylogenies. We find that tropical taxa are nested within a predominantly Cape clade. There is unidirectional migration from the Cape into the Drakensberg and from there northwards into tropical Africa. The amount of in situ diversification differs between areas and clades. Dating estimates show that the migration into tropical East Africa has occurred in the last 17 Myr, consistent with the Mio-Pliocene formation of the mountains in this area.

  3. Creating Highlander Wherever You Are

    ERIC Educational Resources Information Center

    Williams, Susan; Mullett, Cathy

    2016-01-01

    Highlander Research and Education Center serves as a catalyst for grassroots organizing and movement building. This article focuses on an interview with education coordinator Susan Williams who has worked at Highlander for 26 years. We discuss how others can and do create powerful popular education experiences anywhere, whether they have a…

  4. Cape Cod, Massachusetts, USA

    NASA Technical Reports Server (NTRS)

    1990-01-01

    Cape Cod, Massachusetts, USA (42.0N, 70.5W) is a national seashore recreation area with many fine resorts and summer estate homes. Geologically, the cape is a deposit of earth and stone called a terminal moraine, left by the great Pleistocene glaciers of about 20,000 years ago. The through canal at the base of the cape is a manmade feature for waterborne traffic and is part of the Intercoastal Canal network. The cape actually begins south of the canal.

  5. Analysis of shoreline and geomorphic change for Breton Island, Louisiana, from 1869 to 2014

    USGS Publications Warehouse

    Terrano, Joseph F.; Flocks, James G.; Smith, Kathryn E. L.

    2016-04-19

    Many barrier islands in the United States are eroding and losing elevation substantively because of storm surge, waves, and sea-level changes. This is particularly true for the deltaic barrier system in Louisiana. Breton Island is near the mouth of the Mississippi River at the southern end of the Chandeleur barrier island chain in southeast Louisiana. This report expands on previous geomorphic studies of Breton Island by incorporating additional historic and recent datasets. Multiple analyses focus on longand short-term shoreline change, as well as episodic events and anthropogenic modification. Analyses periods include long term (1869–2014), long-term historic (1869–1950), post-Mississippi River-Gulf Outlet (1950–2014), pre/post-Hurricane Katrina (2004–5), and recent (2005–14). In addition to shoreline change, barrier island geomorphology is evaluated using island area, elevation, and sediment volume change. In the long term (1869–2014), Breton Island was affected by landward transgression, island narrowing, and elevation loss. Major storm events exacerbated the long-term trends. In the recent period (2005–14), Breton Island eroded at a slower rate than in the long-term and gained area and total sediment volume. The recent accretion is likely because of the lack of major storms since Hurricane Katrina in 2005.

  6. Cape Cod, Massachusetts, USA

    NASA Technical Reports Server (NTRS)

    1990-01-01

    This view of Cape Cod, Massachusetts, USA (42.0N, 70.5W) is a detailed look at the national seashore recreation area with its many fine resorts and summer estate homes. Geologically, the cape is a deposit of earth and stone called a terminal moraine, left by the great Pleistocene glaciers of about 20,000 years ago.

  7. Cape Cod, Massachusetts, USA

    NASA Technical Reports Server (NTRS)

    1990-01-01

    This view of Cape Cod, Massachusetts, USA (42.0N, 70.0W) is a detailed look at the national seashore recreation area with its many fine resorts and summer estate homes. Geologically, the cape is a deposit of earth and stone called a terminal moraine, left by the great Pleistocene glaciers of about 20,000 years ago.

  8. Crater Highlands, Tanzania

    NASA Technical Reports Server (NTRS)

    2006-01-01

    The Shuttle Radar Topography Mission (SRTM), flown aboard Space Shuttle Endeavour in February 2000, acquired elevation measurements for nearly all of Earth's landmass between 60oN and 56oS latitudes. For many areas of the world SRTM data provide the first detailed three-dimensional observation of landforms at regional scales. SRTM data were used to generate this view of the Crater Highlands along the East African Rift in Tanzania. Landforms are depicted with colored height and shaded relief, using a vertical exaggeration of 2X and a southwestwardly look direction.

    Lake Eyasi is depicted in blue at the top of the image, and a smaller lake occurs in Ngorongoro Crater. Near the image center, elevations peak at 3648 meters (11,968 feet) at Mount Loolmalasin, which is south of Ela Naibori Crater. Kitumbeine (left) and Gelai (right) are the two broad mountains rising from the rift lowlands. Mount Longido is seen in the lower left, and the Meto Hills are in the right foreground.

    Tectonics, volcanism, landslides, erosion and deposition -- and their interactions -- are all very evident in this view. The East African Rift is a zone of spreading between the African (on the west) and Somali (on the east) crustal plates. Two branches of the rift intersect here in Tanzania, resulting in distinctive and prominent landforms. One branch trends nearly parallel the view and includes Lake Eyasi and the very wide Ngorongoro Crater. The other branch is well defined by the lowlands that trend left-right across the image (below center, in green). Volcanoes are often associated with spreading zones where magma, rising to fill the gaps, reaches the surface and builds cones. Craters form if a volcano explodes or collapses. Later spreading can fracture the volcanoes, which is especially evident on Kitumbeine and Gelai Mountains (left and right, respectively, lower center).

    The Crater Highlands rise far above the adjacent savannas, capture moisture from passing air masses

  9. Ranks and relationships in Highland ponies and Highland Cows.

    PubMed

    Clutton-Brock, T H; Greenwood, P J; Powell, R P

    1976-06-01

    Recent studies of primates have questioned the importance of dominance hierarchies in groups living under natural conditions. In a herd of Highland ponies and one of Highland cattle grazing under free-range conditions on the Isle of Rhum (Inner Hebrides) well defined hierarchies were present. The provision of food produced a marked increase in the frequency of agonistic interactions but had no effect on the rank systems of the two herds. While rank was clearly important in affecting the distribution of agonistic interactions, it was poorly related to behaviour in non-agonistic situations. PMID:961125

  10. Panorama from 'Cape Verde'

    NASA Technical Reports Server (NTRS)

    2007-01-01

    NASA's Mars Exploration Rover Opportunity captured this vista of 'Victoria Crater' from the viewpoint of 'Cape Verde,' one of the promontories that are part of the scalloped rim of the crater. Opportunity drove onto Cape Verde shortly after arriving at the rim of Victoria in September 2006. The view combines hundreds of exposures taken by the rover's panoramic camera (Pancam). The camera began taking the component images during Opportunity's 970th Martian day, or sol, on Mars (Oct. 16, 2006). Work on the panorama continued through the solar conjunction period, when Mars was nearly behind the sun from Earth's perspective and communications were minimized. Acquisition of images for this panorama was completed on Opportunity's 991st sol (Nov. 7, 2006).

    The top of Cape Verde is in the immediate foreground at the center of the image. To the left and right are two of the more gradually sloped bays that alternate with the cliff-faced capes or promontories around the rim of the crater. 'Duck Bay,' where Opportunity first reached the rim, is to the right. Beyond Duck Bay counterclockwise around the rim, the next promontory is 'Cabo Frio,' about 150 meters (500 feet) from the rover. On the left side of the panorama is 'Cape St. Mary,' the next promontory clockwise from Cape Verde and about 40 meters (130 feet) from the rover. The vantage point atop Cape Verde offered a good view of the rock layers in the cliff face of Cape St. Mary, which is about 15 meters or 50 feet tall. By about two weeks after the Pancam finished collecting the images for this panorama, Opportunity had driven to Cape St. Mary and was photographing Cape Verde's rock layers.

    The far side of the crater lies about 800 meters (half a mile) away, toward the southeast.

    This approximately true-color view combines images taken through three of the Pancam's filters, admitting light with wavelengths centered at 750 nanometers (near infrared), 530 nanometers (green) and 430 nanometers (violet).

  11. Malaria in Highlands of Ecuador since 1900

    PubMed Central

    Hunter, Fiona F.

    2012-01-01

    A recent epidemic of malaria in the highlands of Bolivia and establishment of multiple Anopheles species mosquitoes in the highlands of Ecuador highlights the reemergence of malaria in the Andes Mountains in South America. Because malaria was endemic to many highland valleys at the beginning of the 20th century, this review outlines the 20th century history of malaria in the highlands of Ecuador, and focuses on its incidence (e.g., geographic distribution) and elimination from the northern highland valleys of Pichincha and Imbabura and the role of the Guayaquil to Quito railway in creating highland larval habitat and inadvertently promoting transportation of the vector and parasite. Involvement of control organizations in combating malaria in Ecuador is also outlined in a historical context. PMID:22469234

  12. Perils of correlating CUSUM-transformed variables to infer ecological relationships (Breton et al. 2006; Glibert 2010)

    USGS Publications Warehouse

    Cloern, James E.; Jassby, Alan D.; Carstensen, Jacob; Bennett, William A.; Kimmerer, Wim; Mac Nally, Ralph; Schoellhamer, David H.; Winder, Monika

    2012-01-01

    We comment on a nonstandard statistical treatment of time-series data first published by Breton et al. (2006) in Limnology and Oceanography and, more recently, used by Glibert (2010) in Reviews in Fisheries Science. In both papers, the authors make strong inferences about the underlying causes of population variability based on correlations between cumulative sum (CUSUM) transformations of organism abundances and environmental variables. Breton et al. (2006) reported correlations between CUSUM-transformed values of diatom biomass in Belgian coastal waters and the North Atlantic Oscillation, and between meteorological and hydrological variables. Each correlation of CUSUM-transformed variables was judged to be statistically significant. On the basis of these correlations, Breton et al. (2006) developed "the first evidence of synergy between climate and human-induced river-based nitrate inputs with respect to their effects on the magnitude of spring Phaeocystis colony blooms and their dominance over diatoms."

  13. CAPE Outlook. Number 379

    ERIC Educational Resources Information Center

    Council for American Private Education, 2012

    2012-01-01

    Outlook is CAPE's monthly newsletter. Each issue is packed with information relating to private education: new legislation and regulations, the most recent research, court rulings, national trends, federal initiatives, private school news briefs, and much more. This issue contains the following articles: (1) Report Examines Charter School/Catholic…

  14. Measurements of SO2 concentration and atmospheric structure in Delta and Breton wildlife refuges

    SciTech Connect

    Hsu, S.A.

    1995-04-01

    A field program designed to measure the ambient concentrations of SO2 as well as pertinent meteorological parameters was conducted during the summer of 1993. Three stations were established in the EPA Class 1 areas of Breton and Delta Wildlife Refuges near the mouth of the Mississippi River. It was found that the SO2 concentration measured throughout the monitoring duration was only 2% of the National maximum allowable once per year. The passage of a weak cold front in September showed that the SO2 concentrations were higher when the wind blew from land to the Gulf than under normal summer conditions when the wind blew from the Gulf toward land.

  15. 33 CFR 80.525 - Cape Lookout, NC to Cape Fear, NC.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false Cape Lookout, NC to Cape Fear, NC... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.525 Cape Lookout, NC to Cape Fear... southeast side of the Inlet. (g) Except as provided elsewhere in this section from Cape Lookout to Cape...

  16. 33 CFR 80.525 - Cape Lookout, NC to Cape Fear, NC.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false Cape Lookout, NC to Cape Fear, NC... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.525 Cape Lookout, NC to Cape Fear...) Except as provided elsewhere in this section from Cape Lookout to Cape Fear, lines drawn parallel...

  17. 33 CFR 80.525 - Cape Lookout, NC to Cape Fear, NC.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Cape Lookout, NC to Cape Fear, NC... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.525 Cape Lookout, NC to Cape Fear...) Except as provided elsewhere in this section from Cape Lookout to Cape Fear, lines drawn parallel...

  18. 33 CFR 80.525 - Cape Lookout, NC to Cape Fear, NC.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Cape Lookout, NC to Cape Fear, NC... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.525 Cape Lookout, NC to Cape Fear... southeast side of the Inlet. (g) Except as provided elsewhere in this section from Cape Lookout to Cape...

  19. 33 CFR 80.525 - Cape Lookout, NC to Cape Fear, NC.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false Cape Lookout, NC to Cape Fear, NC... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.525 Cape Lookout, NC to Cape Fear... southeast side of the Inlet. (g) Except as provided elsewhere in this section from Cape Lookout to Cape...

  20. The Cape Mendocino tsunami

    USGS Publications Warehouse

    Gonzalez, F.I.; Bernard, E. N.

    1992-01-01

    The Cape Mendocino earthquake of April 25, 1992, generated a tsunami recorded by NOAA (National Oceanic and Atmospheric Administration) sea level gauges in California, Oregon, and Hawaii. The accompanying figure shows the tsunami waveforms acquired at twelve of these stations. the table that follows identifies these stations and gives preliminary estimates of the tsunami travel time from the source region to selected West Coast stations. 

  1. Language Attitudes and Community Engagement: Diwan--The Breton Immersion High School through the Eyes of Its Pupils

    ERIC Educational Resources Information Center

    Dolowy-Rybinska, Nicole

    2016-01-01

    This article is based on long-term participant observation and interviews with pupils and graduates of the Diwan immersion high school in Brittany, France. With reference to the theory of "communities of practice," this article shows how the education in the Breton immersion school can influence a knowledge of the minority language and…

  2. 76 FR 27970 - Safety Zone; Cape Charles Fireworks, Cape Charles Harbor, Cape Charles, VA.

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-05-13

    ... in Cape Charles, VA in support of the Fourth of July Fireworks event. This action is necessary to... public dockets in the January 17, 2008, issue of the Federal Register (73 FR 3316). Public Meeting We do... notice. Basis and Purpose On July 3, 2011 the Town of Cape Charles will sponsor a fireworks display...

  3. Carbon Balance of the Breton Classical Plots over Half a Century

    SciTech Connect

    Izaurralde, R Cesar C. ); Mcgill, William B.; Robertson, J A.; Juma, N G.; Thurston, J J.

    2001-02-01

    We related C input and management to soil organic C (SOC) dynamics over 51 yr (1939-1990). We used two rotations from the Breton Classical Plots at Breton, Canada, on a Typic Cryoboralf: (i) wheat (Triticum aestivum L.)-fallow (WF) and (ii) wheat-oat (Avena sativa L.)-barley (Hordeum vulgare L.)-hay (primarily alfalfa, Medicago sativa L.)-hay (WOBHH), in factorial combination with three fertility levels: no added fertilizer[Nil], N-P-K-S fertilizers[F], and farmyard manure[M]. Net aboveground C productivity (NAGCP, kg ha-1 yr-1) averaged 576 in WF-Nil and 1078 in WF-F and SOC decreased in both, but NAGCP averaged 1208 in WF-M, where SOC increased. A NAGCP of 853 in WOBHH-Nil maintained SOC, while both 1831 in WOBHH-F and 1714 in WOBHH-M increased SOC. After 51 yr, WOBHH-M had 25 Mg ha-1 more SOC than did WF-Nil. Because of contrasting decay rates and root/shoot ratios, C input needed to maintain the original SOC was twofold greater in WF than in WOBHH, which required a fourfold in crease in NAGCP to attain these inputs. A three-compartment model fitted to the data suggested loss of C from the active compartments and gain of C by the passive compartments. Inputs of C that maintained SOC over 51 yr would lead to a steady state of 2.9 times more C than in 1939, an d26% higher than the native SOC content. Return of 30% of the crop C as manure would sustain SOC sequestration in all WOBHH rotations with NAGCP> 400 kg ha-1 yr-1 and in those WF rotations with NAGCP> 1000 kg ha-1 yr-1.

  4. 75 FR 60840 - Highland Capital Management, L.P. and Highland Funds I; Notice of Application

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-10-01

    ... From the Federal Register Online via the Government Publishing Office SECURITIES AND EXCHANGE COMMISSION Highland Capital Management, L.P. and Highland Funds I; Notice of Application September 27, 2010. AGENCY: Securities and Exchange Commission (``Commission''). ACTION: Notice of an application under section 6(c) of the Investment Company Act...

  5. Relating large-scale climate variability to local species abundance: ENSO forcing and shrimp in Breton Sound, Louisiana, USA

    USGS Publications Warehouse

    Piazza, Bryan P.; LaPeyre, Megan K.; Keim, B.D.

    2010-01-01

    Climate creates environmental constraints (filters) that affect the abundance and distribution of species. In estuaries, these constraints often result from variability in water flow properties and environmental conditions (i.e. water flow, salinity, water temperature) and can have significant effects on the abundance and distribution of commercially important nekton species. We investigated links between large-scale climate variability and juvenile brown shrimp Farfantepenaeus aztecus abundance in Breton Sound estuary, Louisiana (USA). Our goals were to (1) determine if a teleconnection exists between local juvenile brown shrimp abundance and the El Niño Southern Oscillation (ENSO) and (2) relate that linkage to environmental constraints that may affect juvenile brown shrimp recruitment to, and survival in, the estuary. Our results identified a teleconnection between winter ENSO conditions and juvenile brown shrimp abundance in Breton Sound estuary the following spring. The physical connection results from the impact of ENSO on winter weather conditions in Breton Sound (air pressure, temperature, and precipitation). Juvenile brown shrimp abundance effects lagged ENSO by 3 mo: lower than average abundances of juvenile brown shrimp were caught in springs following winter El Niño events, and higher than average abundances of brown shrimp were caught in springs following La Niña winters. Salinity was the dominant ENSO-forced environmental filter for juvenile brown shrimp. Spring salinity was cumulatively forced by winter river discharge, winter wind forcing, and spring precipitation. Thus, predicting brown shrimp abundance requires incorporating climate variability into models.

  6. Chemistry of the Apollo 11 highland component

    NASA Technical Reports Server (NTRS)

    Laul, J. C.; Papike, J. J.; Simon, S. B.; Shearer, C. K.

    1983-01-01

    Thirty-eight Apollo 11 lunar highland fragments from coarse fines 10085 have been subjected to petrologic and chemical study. Six major chemical groups are identified: (a) high-K KREEP; (b) anorthosite with a 10X chondrite positive Eu anomaly and anorthosite with 30X positive Eu anomaly; (c) ANT; (d) LKFM; (e) anorthositic gabbro with no Eu anomaly, with a positive Eu anomaly, and with a negative Eu anomaly; and (f) dominant Highland component, 2X-10X chondrite with a positive 10X-14X Eu anomaly. Newly recognized groups are presented based on the REE patterns: (a) ANT group with 5X La and a 22X positive Eu anomaly; (b) 10X flat with 14X positive Eu anomaly; and (c) 2-3X flat with a 10X positive Eu anomaly. The highland suite is very low in K and REE, and is overall quite similar to the Apollo 16 suite.

  7. Rock types present in lunar highland soils

    NASA Technical Reports Server (NTRS)

    Reid, A. M.

    1974-01-01

    Several investigators have studied soils from the lunar highlands with the objective of recognizing the parent rocks that have contributed significant amounts of material to these soils. Comparing only major element data, and thus avoiding the problems induced by individual classifications, these data appear to converge on a relatively limited number of rock types. The highland soils are derived from a suite of highly feldspathic rocks comprising anorthositic gabbros (or norites), high alumina basalts, troctolites, and less abundant gabbroic (or noritic) anorthosites, anorthosites, and KREEP basalts.

  8. 27 CFR 9.115 - Ozark Highlands.

    Code of Federal Regulations, 2013 CFR

    2013-04-01

    ... OF THE TREASURY ALCOHOL AMERICAN VITICULTURAL AREAS Approved American Viticultural Areas § 9.115 Ozark Highlands. (a) Name. The name of the viticultural area described in this section is “Ozark... viticultural area are three U.S.G.S. maps of the 1:250,000 series. They are titled: (1) Rolla,...

  9. 27 CFR 9.115 - Ozark Highlands.

    Code of Federal Regulations, 2014 CFR

    2014-04-01

    ... OF THE TREASURY ALCOHOL AMERICAN VITICULTURAL AREAS Approved American Viticultural Areas § 9.115 Ozark Highlands. (a) Name. The name of the viticultural area described in this section is “Ozark... viticultural area are three U.S.G.S. maps of the 1:250,000 series. They are titled: (1) Rolla,...

  10. A Report on the Highlander Folk School.

    ERIC Educational Resources Information Center

    Cassara, Beverly B.

    The Highlander Folk School was founded as an alternative kind of education with no academic admission requirements, no examinations or grades, and no set curriculum. Hard times were caused by lack of funds and the radical nature of its purpose--to help poor people know their rights and stand up for them. As an undergraduate, Myles Horton, its…

  11. Highland Elementary School. Learning by Example Series.

    ERIC Educational Resources Information Center

    Fager, Jennifer

    As part of a series of stories about real-world schools that have achieved substantial success in school improvement over multiple-year periods, this report provides an in-depth look at one school's efforts to improve student learning. The school profiled is Highland Elementary School, located in Salem, Oregon, serving a student population of…

  12. 27 CFR 9.159 - Yorkville Highlands.

    Code of Federal Regulations, 2011 CFR

    2011-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2011-04-01 2011-04-01 false Yorkville Highlands. 9.159 Section 9.159 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU, DEPARTMENT..., California. The boundary is as follows: (1) The beginning point is Benchmark 680, located in Section 30,...

  13. 27 CFR 9.159 - Yorkville Highlands.

    Code of Federal Regulations, 2012 CFR

    2012-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2012-04-01 2012-04-01 false Yorkville Highlands. 9.159 Section 9.159 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU, DEPARTMENT..., California. The boundary is as follows: (1) The beginning point is Benchmark 680, located in Section 30,...

  14. 27 CFR 9.159 - Yorkville Highlands.

    Code of Federal Regulations, 2014 CFR

    2014-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2014-04-01 2014-04-01 false Yorkville Highlands. 9.159 Section 9.159 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU, DEPARTMENT..., California. The boundary is as follows: (1) The beginning point is Benchmark 680, located in Section 30,...

  15. 27 CFR 9.159 - Yorkville Highlands.

    Code of Federal Regulations, 2013 CFR

    2013-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2013-04-01 2013-04-01 false Yorkville Highlands. 9.159 Section 9.159 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU, DEPARTMENT..., California. The boundary is as follows: (1) The beginning point is Benchmark 680, located in Section 30,...

  16. 27 CFR 9.159 - Yorkville Highlands.

    Code of Federal Regulations, 2010 CFR

    2010-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2010-04-01 2010-04-01 false Yorkville Highlands. 9.159 Section 9.159 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU, DEPARTMENT..., California. The boundary is as follows: (1) The beginning point is Benchmark 680, located in Section 30,...

  17. Human malaria in the highlands of Yemen

    PubMed Central

    AL-Mekhlafi, A M; AL-Mekhlafi, H M; Mahdy, M A K; Azazy, A A; Fong, M Y

    2011-01-01

    Between June 2008 and March 2009, a cross-sectional study of human malaria was carried out in four governorates of Yemen, two (Taiz and Hodiedah) representing the country’s highlands and the others (Dhamar and Raymah) the country’s coastal plains/foothills. The main aims were to determine the prevalences of Plasmodium infection among 455 febrile patients presenting for care at participating health facilities and to investigate the potential risk factors for such infection. Malarial infection was detected in 78 (17·1%) of the investigated patients and was more likely to be detected among the febrile patients from the highlands than among those presenting in the coastal plains/foothills (22·6% v.13·9%; χ2 = 10·102; P = 0·018). Binary logistic-regression models identified low household income [odds ratio (OR) = 13·52; 95% confidence interval (CI) = 2·62–69·67; P = 0·002], living in a household with access to a water pump (OR = 4·18; CI = 1·60–10·96; P = 0·004) and living in a household near a stream (OR = 4·43; CI = 1·35–14·56; P = 0·014) as significant risk factors for malarial infection in the highlands. Low household income was the only significant risk factor identified for such infection in the coastal plains and foothills (OR = 8·20; CI = 1·80–37·45; P = 0·007). It is unclear why febrile patients in the highlands of Yemen are much more likely to be found to have malarial infection than their counterparts from the coastal plains and foothills. Although it is possible that malarial transmission is relatively intense in the highlands, it seems more likely that, compared with those who live at lower altitudes, those who live in the highlands are less immune to malaria, and therefore more likely to develop febrile illness following malarial infection. Whatever the cause of the symptomatic malarial infection commonly found in the highlands of Yemen, it is a matter of serious

  18. Human malaria in the highlands of Yemen.

    PubMed

    Al-Mekhlafi, A M; Al-Mekhlafi, H M; Mahdy, M A K; Azazy, A A; Fong, M Y

    2011-04-01

    Between June 2008 and March 2009, a cross-sectional study of human malaria was carried out in four governorates of Yemen, two (Taiz and Hodiedah) representing the country's <span class="hlt">highlands</span> and the others (Dhamar and Raymah) the country's coastal plains/foothills. The main aims were to determine the prevalences of Plasmodium infection among 455 febrile patients presenting for care at participating health facilities and to investigate the potential risk factors for such infection. Malarial infection was detected in 78 (17·1%) of the investigated patients and was more likely to be detected among the febrile patients from the <span class="hlt">highlands</span> than among those presenting in the coastal plains/foothills (22·6% v.13·9%; χ(2)=10·102; P=0·018). Binary logistic-regression models identified low household income [odds ratio (OR)=13·52; 95% confidence interval (CI)=2·62-69·67; P=0·002], living in a household with access to a water pump (OR=4·18; CI=1·60-10·96; P=0·004) and living in a household near a stream (OR=4·43; CI=1·35-14·56; P=0·014) as significant risk factors for malarial infection in the <span class="hlt">highlands</span>. Low household income was the only significant risk factor identified for such infection in the coastal plains and foothills (OR = 8·20; CI=1·80-37·45; P=0·007). It is unclear why febrile patients in the <span class="hlt">highlands</span> of Yemen are much more likely to be found to have malarial infection than their counterparts from the coastal plains and foothills. Although it is possible that malarial transmission is relatively intense in the <span class="hlt">highlands</span>, it seems more likely that, compared with those who live at lower altitudes, those who live in the <span class="hlt">highlands</span> are less immune to malaria, and therefore more likely to develop febrile illness following malarial infection. Whatever the cause of the symptomatic malarial infection commonly found in the <span class="hlt">highlands</span> of Yemen, it is a matter of serious concern that should be addressed in the national strategy to control malaria.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3364268','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3364268"><span id="translatedtitle">Measuring Changes in Consumer Resource Availability to Riverine Pulsing in <span class="hlt">Breton</span> Sound, Louisiana, USA</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Piazza, Bryan P.; La Peyre, Megan K.</p> <p>2012-01-01</p> <p>Resource pulses are thought to structure communities and food webs through the assembly of consumers. Aggregated consumers represent a high quality resource subsidy that becomes available for trophic transfer during and after the pulse. In estuarine systems, riverine flood pulses deliver large quantities of basal resources and make high quality habitat available for exploitation by consumers. These consumers represent a change in resources that may be available for trophic transfer. We quantified this increased consumer resource availability (nekton density, biomass, energy density) provided by riverine flood pulsing in <span class="hlt">Breton</span> Sound, Louisiana, USA. We used water level differences between an area subject to two experimental riverine flood pulses (inflow) and a reference area not receiving inflow to identify the percentage of nekton standing stock and energy density that may be attributable solely to riverine pulsing and may represent a consumer resource subsidy. Riverine pulsing accounted for more than 60% of resident nekton density (ind m−2), biomass (g m−2), and energy density (cal m−2) on the flooded marsh surface during two experimental pulse events in 2005. Our results document the potential subsidy of resident nekton standing stock from a riverine flood pulse available for export to subtidal habitats. Given predicted large scale changes in river discharge globally, this approach could provide a useful tool for quantifying the effects of changes in riverine discharge on consumer resource availability. PMID:22666363</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-06-17/pdf/2010-14580.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-06-17/pdf/2010-14580.pdf"><span id="translatedtitle">75 FR 34479 - <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-06-17</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on July...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_1");'>1</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li class="active"><span>3</span></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_3 --> <div id="page_4" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="61"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-02-03/pdf/2010-2233.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-02-03/pdf/2010-2233.pdf"><span id="translatedtitle">75 FR 5622 - <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-02-03</p> <p>... <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission AGENCY.... App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on March 22, 2010 at 1...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-08-12/pdf/2010-19865.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-08-12/pdf/2010-19865.pdf"><span id="translatedtitle">75 FR 48990 - <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-08-12</p> <p>... <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission AGENCY.... App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on September 13, 2010, at 1...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-10-18/pdf/2010-26134.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-10-18/pdf/2010-26134.pdf"><span id="translatedtitle">75 FR 63854 - <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-10-18</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-07-26/pdf/2011-18830.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-07-26/pdf/2011-18830.pdf"><span id="translatedtitle">76 FR 44606 - <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-07-26</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory.... 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on September...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-10-25/pdf/2011-27595.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-10-25/pdf/2011-27595.pdf"><span id="translatedtitle">76 FR 66082 - <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-10-25</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-02-17/pdf/2012-3726.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-02-17/pdf/2012-3726.pdf"><span id="translatedtitle">77 FR 9699 - <span class="hlt">Cape</span> Cod National Seashore Advisory Commission; <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-02-17</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore Advisory Commission; <span class="hlt">Cape</span> Cod National Seashore, South... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on March...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-04-19/pdf/2010-8972.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-04-19/pdf/2010-8972.pdf"><span id="translatedtitle">75 FR 20380 - <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, Massachusetts; <span class="hlt">Cape</span> Cod National Seashore Advisory...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-04-19</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore; South Wellfleet, Massachusetts; <span class="hlt">Cape</span> Cod National... (Pub. L. 92-463, 86 Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-12-14/pdf/2010-31309.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-12-14/pdf/2010-31309.pdf"><span id="translatedtitle">75 FR 77900 - <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-12-14</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-12-29/pdf/2011-33399.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-12-29/pdf/2011-33399.pdf"><span id="translatedtitle">76 FR 81965 - <span class="hlt">Cape</span> Cod National Seashore Advisory Commission; <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-12-29</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore Advisory Commission; <span class="hlt">Cape</span> Cod National Seashore, South... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-02-15/pdf/2011-3256.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-02-15/pdf/2011-3256.pdf"><span id="translatedtitle">76 FR 8768 - <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-02-15</p> <p>... National Park Service <span class="hlt">Cape</span> Cod National Seashore, South Wellfleet, MA; <span class="hlt">Cape</span> Cod National Seashore Advisory... Stat. 770, 5 U.S.C. App 1, Section 10) of a meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on March...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-530.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-530.pdf"><span id="translatedtitle">33 CFR 165.530 - Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. 165.530 Section 165.530 Navigation and Navigable Waters COAST GUARD... § 165.530 Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. (a) Location. The following area...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-530.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-530.pdf"><span id="translatedtitle">33 CFR 165.530 - Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. 165.530 Section 165.530 Navigation and Navigable Waters COAST GUARD... § 165.530 Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. (a) Location. The following area...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-530.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-530.pdf"><span id="translatedtitle">33 CFR 165.530 - Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. 165.530 Section 165.530 Navigation and Navigable Waters COAST GUARD... § 165.530 Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. (a) Location. The following area...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-530.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-530.pdf"><span id="translatedtitle">33 CFR 165.530 - Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2010-07-01 2010-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. 165.530 Section 165.530 Navigation and Navigable Waters COAST GUARD... § 165.530 Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. (a) Location. The following area...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-530.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-530.pdf"><span id="translatedtitle">33 CFR 165.530 - Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. 165.530 Section 165.530 Navigation and Navigable Waters COAST GUARD... § 165.530 Safety Zone: <span class="hlt">Cape</span> Fear and Northeast <span class="hlt">Cape</span> Fear Rivers, NC. (a) Location. The following area...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09082&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09082&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> St. Mary' from '<span class="hlt">Cape</span> Verde'</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> St. Mary' from the from the vantage point of '<span class="hlt">Cape</span> Verde,' the next promontory counterclockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> St. Mary combines several exposures taken by the rover's panoramic camera into an approximately true-color mosaic. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. Near the base of the <span class="hlt">Cape</span> St. Mary cliff are layers with a pattern called 'crossbedding,' intersecting with each other at angles, rather than parallel to each other. Large-scale crossbedding can result from material being deposited as wind-blown dunes. <p/> The images combined into this mosaic were taken during the 970th Martian day, or sol, of Opportunity's Mars-surface mission (Oct. 16, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09085&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09085&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> St. Mary' from '<span class="hlt">Cape</span> Verde' (False Color)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> St. Mary' from the from the vantage point of '<span class="hlt">Cape</span> Verde,' the next promontory counterclockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> St. Mary combines several exposures taken by the rover's panoramic camera into a false-color mosaic. Contrast has been adjusted to improve the visibility of details in shaded areas. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. Near the base of the <span class="hlt">Cape</span> St. Mary cliff are layers with a pattern called 'crossbedding,' intersecting with each other at angles, rather than parallel to each other. Large-scale crossbedding can result from material being deposited as wind-blown dunes. <p/> The images combined into this mosaic were taken during the 970th Martian day, or sol, of Opportunity's Mars-surface mission (Oct. 16, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters. The false color enhances subtle color differences among materials in the rocks and soils of the scene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09083&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09083&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> St. Mary' from '<span class="hlt">Cape</span> Verde' (Altered Contrast)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> St. Mary' from the from the vantage point of '<span class="hlt">Cape</span> Verde,' the next promontory counterclockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> St. Mary combines several exposures taken by the rover's panoramic camera into an approximately true-color mosaic with contrast adjusted to improve the visibility of details in shaded areas. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. Near the base of the <span class="hlt">Cape</span> St. Mary cliff are layers with a pattern called 'crossbedding,' intersecting with each other at angles, rather than parallel to each other. Large-scale crossbedding can result from material being deposited as wind-blown dunes. <p/> The images combined into this mosaic were taken during the 970th Martian day, or sol, of Opportunity's Mars-surface mission (Oct. 16, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19740040096&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528metamorphic%2Brock%2529','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19740040096&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528metamorphic%2Brock%2529"><span id="translatedtitle">Pyroxene poikiloblastic rocks from the lunar <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bence, A. E.; Papike, J. J.; Sueno, S.; Delano, J. W.</p> <p>1973-01-01</p> <p>The results of detailed petrographic, X-ray, electron microprobe, ion probe, and Ar-40/Ar-39 age studies of pyroxene poikiloblastic breccias, an important lunar <span class="hlt">highlands</span> lithology, are interpreted to indicate that high grade metamorphic recrystallization occurred over wide regions of the moon at about 4.0 G.y. This metamorphism was probably related to a period of high meteorite influx at that time. The temperatures achieved were highly variable but in some cases were sufficiently intense to cause varying degrees of partial melting of the precursor <span class="hlt">highlands</span> breccias. A complete spectrum of metamorphic grades from only slight recrystallization to virtually complete melting would be expected in such a model. Such a spectrum is observed in the Apollo 16 rocks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20050174655','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20050174655"><span id="translatedtitle">Impact Crater Deposits in the Martian <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mest, S. C.; Crown, D. a.</p> <p>2005-01-01</p> <p>The martian <span class="hlt">highlands</span> of Noachis Terra (20-30 deg S, 20-50 deg E), Tyrrhena Terra (0-30 deg S, 50- 100 deg E) and Terra Cimmeria (0-60 deg S, 120-170 deg E) preserve long and complex histories of degradation, but the relative effects of such factors as fluvial, eolian, and mass wasting processes have not been well constrained. The effects of this degradation are best observed on large (D greater than 10 km) impact craters that characterize the ancient <span class="hlt">highlands</span>. Some craters exhibit distinct interior deposits, but precise origins of these deposits are enigmatic; infilling may occur by sedimentary (e.g., fluvial, lacustrine, eolian), mass wasting and (or) volcanic processes.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_4 --> <div id="page_5" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="81"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMEP24A..07H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMEP24A..07H"><span id="translatedtitle">Controls on wetland loss during large magnitude storms: a case study in <span class="hlt">Breton</span> Sound, LA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Howes, N. C.; Hughes, Z. J.; Fitzgerald, D.; Georgiou, I. Y.; Kulp, M. A.; Miner, M. D.; Smith, J. M.; Barras, J. A.</p> <p>2010-12-01</p> <p>In 2005, the storm surge and wave field associated with Hurricanes Katrina and Rita eroded 527 km^2 of wetlands within the Louisiana coastal plain. Low salinity wetlands were preferentially eroded, while higher salinity wetlands remained largely intact and unchanged. Field studies were undertaken in <span class="hlt">Breton</span> Sound, Louisiana, where both the low and high salinity wetlands experienced very similar hydrodynamic conditions during Hurricane Katrina. This site provides a natural case to study the causes of the observed land loss patterns. We observe geotechnical differences between soil profiles in high and low salinity wetlands, as controlled by vegetation, and which result in differential erosion. Low salinity wetlands contain a weak zone at a depth of ~30 cm below the marsh surface; this coincides with the base of rooting and has shear strengths as low as 500-1450 Pa. High salinity wetlands display deeper rooting, have no identifiable weak zone, and shear strengths exceed 4500 Pa throughout the upper soil profile. Results from a model (STWAVE-ADCIRC) are used to establish the hydrodynamic conditions during Hurricane Katrina (storm surge, wave height, and wave period). We calculate the potential shear stresses exerted by waves, accounting for the interaction between the oscillatory flow and the vegetation. Calculated shear stresses were in the range 425-3600 Pa, values sufficient to cause widespread erosion of the low salinity wetlands, but not the high salinity wetlands, corresponding with the observed patterns of land loss. A conceptual model is developed to illustrate the influence of rooting type and depth on the strength profile of wetlands soils and their susceptibility to erosion during large magnitude storms. These findings have implications for wetland restoration schemes involving freshwater diversions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/ds/0799/title.html','USGSPUBS'); return false;" href="https://pubs.usgs.gov/ds/0799/title.html"><span id="translatedtitle">Baseline coastal oblique aerial photographs collected from Pensacola, Florida, to <span class="hlt">Breton</span> Islands, Louisiana, February 7, 2012</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Morgan, Karen L.M.; Krohn, M. Dennis; Doran, Kara; Guy, Kristy K.</p> <p>2013-01-01</p> <p>The U.S. Geological Survey (USGS) conducts baseline and storm response photography missions to document and understand the changes in vulnerability of the Nation's coasts to extreme storms (Morgan, 2009). On February 7, 2012, the USGS conducted an oblique aerial photographic survey from Pensacola, Fla., to <span class="hlt">Breton</span> Islands, La., aboard a Piper Navajo Chieftain at an altitude of 500 feet (ft) and approximately 1,000 ft offshore. This mission was flown to collect baseline data for assessing incremental changes since the last survey, and the data can be used in the assessment of future coastal change. The photographs provided here are Joint Photographic Experts Group (JPEG) images. The photograph locations are an estimate of the position of the aircraft and do not indicate the location of the feature in the images (see the Navigation Data page). These photos document the configuration of the barrier islands and other coastal features at the time of the survey. The header of each photo is populated with time of collection, Global Positioning System (GPS) latitude, GPS longitude, GPS position (latitude and longitude), keywords, credit, artist (photographer), caption, copyright, and contact information using EXIFtools (Subino and others, 2012). Photographs can be opened directly with any JPEG-compatible image viewer by clicking on a thumbnail on the contact sheet. Table 1 provides detailed information about the assigned location, name, data, and time the photograph was taken along with links to the photograph. In addition to the photographs, a Google Earth Keyhole Markup Language (KML) file is provided and can be used to view the images by clicking on the marker and then clicking on either the thumbnail or the link above the thumbnail. The KML files were created using the photographic navigation files (see the Photos and Maps page).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780057195&hterms=Gabbro&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DGabbro','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780057195&hterms=Gabbro&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DGabbro"><span id="translatedtitle">The lunar <span class="hlt">highland</span> melt-rock suite</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Vaniman, D. T.; Papike, J. J.</p> <p>1978-01-01</p> <p>Size can be used as a criterion to select 18 large (larger than 1 cm) samples from among 148 melt-rock fragments of all sizes. This selection provides a suite of large samples which represent the important chemical variants among <span class="hlt">highland</span> melt rocks; each large sample has enough material for a number of sample-destructive studies, as well as for future reference. Cluster analysis of the total data base of 148 <span class="hlt">highland</span> melt rocks shows six distinct groups: anorthosite, gabbroic anorthosite, anorthositic gabbro ('<span class="hlt">highland</span> basalt'), low K Fra Mauro, intermediate-K Fra Mauro, and high-K. Large samples are available for four of the melt-rock groups (gabbroic anorthosite, anorthositic gabbro, low-K Fra Mauro, and intermediate-K Fra Mauro). This sample selection reveals two subgroups of anorthositic gabbro (one anorthite-poor with negative Eu anomaly and one anorthite-rich without Eu anomaly). There is a sharp distinction between those Apollo 16 melt rocks and glasses which have both been classified as 'gabbroic anorthosite'.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2015/1055','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2015/1055"><span id="translatedtitle">Effects of proposed sediment borrow pits on nearshore wave climate and longshore sediment transport rate along <span class="hlt">Breton</span> Island, Louisiana</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dalyander, Patricia (Soupy); Mickey, Rangley C.; Long, Joseph W.; Flocks, James G.</p> <p>2015-01-01</p> <p>As part of a plan to preserve bird habitat on <span class="hlt">Breton</span> Island, the southernmost extent of the Chandeleur Islands and part of the <span class="hlt">Breton</span> National Wildlife Refuge in Louisiana, the U.S. Fish and Wildlife Service plans to increase island elevation with sand supplied from offshore resources. Proposed sand extraction sites include areas offshore where the seafloor morphology suggests suitable quantities of sediment may be found. Two proposed locations east and south of the island, between 5.5–9 kilometers from the island in 3–6 meters of water, have been identified. Borrow pits are perturbations to shallow-water bathymetry and thus can affect the wave field in a variety of ways, including alterations in sediment transport and new erosional or accretional patterns along the beach. A scenario-based numerical modeling strategy was used to assess the effects of the proposed offshore borrow pits on the nearshore wave field. Effects were assessed over a range of wave conditions and were gaged by changes in significant wave height and wave direction inshore of the borrow sites, as well as by changes in the calculated longshore sediment transport rate. The change in magnitude of the calculated sediment transport rate with the addition of the two borrow pits was an order of magnitude less than the calculated baseline transport rate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=richard+AND+bruce&pg=7&id=ED444922','ERIC'); return false;" href="http://eric.ed.gov/?q=richard+AND+bruce&pg=7&id=ED444922"><span id="translatedtitle">Connect, Combine, Communicate: Revitalizing the Arts in Canadian Schools. Selected Papers from the National Symposium on Arts Education (<span class="hlt">Cape</span> <span class="hlt">Breton</span>, Sydney, Nova Scotia, Canada, August 1997).</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Roberts, Brian A., Ed.</p> <p></p> <p>The National Symposium on Arts Education 1997 provided an opportunity for arts educators, professional artists, and representatives from government agencies to discuss common concerns and to develop strategies for strengthening the arts in Canadian schools. This collection of papers from the symposium addresses many questions about the future of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA02633&hterms=thanksgiving&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dthanksgiving','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA02633&hterms=thanksgiving&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dthanksgiving"><span id="translatedtitle">MISR Looks at <span class="hlt">Cape</span> Cod</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2000-01-01</p> <p><p/>Each year in late November the United States observes the Thanksgiving holiday, commemorating the harvest festival celebrated by the Plymouth colonists and the Native Americans who helped them survive the devastating winter of 1620. Plymouth, Massachusetts, where the Mayflower Pilgrims landed, is located on the west side of <span class="hlt">Cape</span> Cod Bay, shown in this MISR vertical-viewing (nadir) camera image. This nearly cloud-free picture was acquired on April 13, 2000 during Terra orbit 1708.<p/>South of the distinctively-shaped <span class="hlt">Cape</span> Cod are Nantucket Island and Martha's Vineyard. Further west is Block Island, south of Narragansett Bay, Rhode Island. Montauk Point on the eastern tip of Long Island, New York, is visible at the lower left. On the mainland, Providence and Boston appear as gray patches. Jutting out from the Massachusetts coastline, northeast of Boston, is <span class="hlt">Cape</span> Ann, location of the city of Gloucester, which was settled soon after the Pilgrim's arrival in Plymouth. Gloucester is the oldest fishing port in the eastern United States.<p/>MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19920030332&hterms=rocks+minerals&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Drocks%2Bminerals','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19920030332&hterms=rocks+minerals&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Drocks%2Bminerals"><span id="translatedtitle">Mineral compositions in pristine lunar <span class="hlt">highland</span> rocks and the diversity of <span class="hlt">highland</span> magmatism</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bersch, Michael G.; Taylor, G. J.; Keil, Klaus; Norman, Marc D.</p> <p>1991-01-01</p> <p>High precision electron microprobe analyses of olivine and pyroxene in pristine lunar <span class="hlt">highland</span> rocks confirm the dichotomy between ferroan anorthosites and the Mg-suite. Ferroan-anorthosites plot as coherent trends, consistent with formation in a complex global magma system. Lack of coherent compositional trends in the Mg-suite rocks indicates derivation from numerous magmas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title46-vol1/pdf/CFR-2013-title46-vol1-sec7-55.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title46-vol1/pdf/CFR-2013-title46-vol1-sec7-55.pdf"><span id="translatedtitle">46 CFR 7.55 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-10-01</p> <p>... 46 Shipping 1 2013-10-01 2013-10-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. 7.55 Section 7.55 Shipping COAST GUARD, DEPARTMENT OF HOMELAND SECURITY PROCEDURES APPLICABLE TO THE PUBLIC BOUNDARY LINES Atlantic Coast § 7.55 <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. (a) A line drawn from Rudee Inlet Jetty Light “2”...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title46-vol1/pdf/CFR-2014-title46-vol1-sec7-55.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title46-vol1/pdf/CFR-2014-title46-vol1-sec7-55.pdf"><span id="translatedtitle">46 CFR 7.55 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-10-01</p> <p>... 46 Shipping 1 2014-10-01 2014-10-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. 7.55 Section 7.55 Shipping COAST GUARD, DEPARTMENT OF HOMELAND SECURITY PROCEDURES APPLICABLE TO THE PUBLIC BOUNDARY LINES Atlantic Coast § 7.55 <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. (a) A line drawn from Rudee Inlet Jetty Light “2”...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title46-vol1/pdf/CFR-2011-title46-vol1-sec7-55.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title46-vol1/pdf/CFR-2011-title46-vol1-sec7-55.pdf"><span id="translatedtitle">46 CFR 7.55 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-10-01</p> <p>... 46 Shipping 1 2011-10-01 2011-10-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. 7.55 Section 7.55 Shipping COAST GUARD, DEPARTMENT OF HOMELAND SECURITY PROCEDURES APPLICABLE TO THE PUBLIC BOUNDARY LINES Atlantic Coast § 7.55 <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. (a) A line drawn from Rudee Inlet Jetty Light “2”...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title46-vol1/pdf/CFR-2010-title46-vol1-sec7-55.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title46-vol1/pdf/CFR-2010-title46-vol1-sec7-55.pdf"><span id="translatedtitle">46 CFR 7.55 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-10-01</p> <p>... 46 Shipping 1 2010-10-01 2010-10-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. 7.55 Section 7.55 Shipping COAST GUARD, DEPARTMENT OF HOMELAND SECURITY PROCEDURES APPLICABLE TO THE PUBLIC BOUNDARY LINES Atlantic Coast § 7.55 <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. (a) A line drawn from Rudee Inlet Jetty Light “2”...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title46-vol1/pdf/CFR-2012-title46-vol1-sec7-55.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title46-vol1/pdf/CFR-2012-title46-vol1-sec7-55.pdf"><span id="translatedtitle">46 CFR 7.55 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-10-01</p> <p>... 46 Shipping 1 2012-10-01 2012-10-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. 7.55 Section 7.55 Shipping COAST GUARD, DEPARTMENT OF HOMELAND SECURITY PROCEDURES APPLICABLE TO THE PUBLIC BOUNDARY LINES Atlantic Coast § 7.55 <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Fear, NC. (a) A line drawn from Rudee Inlet Jetty Light “2”...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19740040201&hterms=aluminium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Daluminium','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19740040201&hterms=aluminium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Daluminium"><span id="translatedtitle">Radionuclides at Descartes in the central <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wrigley, R. C.</p> <p>1973-01-01</p> <p>Throium, uranium, potassium, aluminium-26, and sodium-22 were measured by nondestructive gamma ray spectrometry in six soil and two rock samples gathered by Apollo 16 in the lunar central <span class="hlt">highlands</span>. The soil samples probably include both major geologic formations in the vicinity, the Cayley and Descartes Formations, although it is possible that the Descartes Formation is not represented. The rock samples have low concentrations of primordial radionuclides. The Al concentrations were lower than could be expected from the high abundance of alumina in the Apollo 16 soils reported earlier, but this could be due to lower concentrations of target elements in these soils, sampling depth variations, or regolithic mixing (exposure age variations).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780062755&hterms=Dunite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DDunite','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780062755&hterms=Dunite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DDunite"><span id="translatedtitle">Evolution of the lunar <span class="hlt">highland</span> crust</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Taylor, S. R.; Bence, A. E.</p> <p>1975-01-01</p> <p>The evolution of three distinct element associations in the lunar <span class="hlt">highland</span> crust is discussed in terms of the Taylor-Jakes model which involves melting of most of the moon during accretion. Sources for (1) high Ca, Al, Sr, Eu, (2) high Mg and Cr, and (3) high K, REE, Zr, Hf, Nb are suggested. Bombardment by large projectiles during the differentiation process causes melting and mixing, which produces a wide range of compositions in the crust. The formation of dunite, troctolite, high-, medium-, and low-K Fra Mauro basalts, and rocks close to the olivine-spinel-plagioclase peritectic point is considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-515.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-515.pdf"><span id="translatedtitle">33 CFR 80.515 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC. 80.515 Section 80.515 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.515 <span class="hlt">Cape</span> Henry, VA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-515.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-515.pdf"><span id="translatedtitle">33 CFR 80.515 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC. 80.515 Section 80.515 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.515 <span class="hlt">Cape</span> Henry, VA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-515.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-515.pdf"><span id="translatedtitle">33 CFR 80.515 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC. 80.515 Section 80.515 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.515 <span class="hlt">Cape</span> Henry, VA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-515.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-515.pdf"><span id="translatedtitle">33 CFR 80.515 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC. 80.515 Section 80.515 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.515 <span class="hlt">Cape</span> Henry, VA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-515.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-515.pdf"><span id="translatedtitle">33 CFR 80.515 - <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> Henry, VA to <span class="hlt">Cape</span> Hatteras, NC. 80.515 Section 80.515 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.515 <span class="hlt">Cape</span> Henry, VA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=STS036-151-225&hterms=recreation&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Drecreation','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=STS036-151-225&hterms=recreation&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Drecreation"><span id="translatedtitle"><span class="hlt">Cape</span> Cod, Buzzard's Bay, Massachusetts, USA</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1990-01-01</p> <p><span class="hlt">Cape</span> Cod, Massachusetts, USA (42.0N, 70.0W) is a national seashore recreation area with many fine resorts and summer estate homes. Geologically, the <span class="hlt">cape</span> is a deposit of earth and stone called a terminal moraine, left by the great Pleistocene glaciers of about 20,000 years ago. The through canal at the base of the <span class="hlt">cape</span> is a manmade feature for waterborne traffic and is part of the Intercoastal Canal network. The <span class="hlt">cape</span> actually begins south of the canal.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_5 --> <div id="page_6" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="101"> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/az0358.photos.180483p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/az0358.photos.180483p/"><span id="translatedtitle">27. VIEW OF <span class="hlt">CAPE</span> ROYAL ROAD FROM ANGEL'S WINDOW, FACING ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>27. VIEW OF <span class="hlt">CAPE</span> ROYAL ROAD FROM ANGEL'S WINDOW, FACING NNW. TURNOUT PICTURED IN PHOTO AZ-40-22 IS VISIBLE IN GAP OF CLIFF. - <span class="hlt">Cape</span> Royal Road, Between North Entrance Road & <span class="hlt">Cape</span> Royal, Grand Canyon, Coconino County, AZ</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/az0358.photos.180458p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/az0358.photos.180458p/"><span id="translatedtitle">2. <span class="hlt">CAPE</span> ROYAL ROAD VIEW. POST ON RIGHT SIDE OF ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>2. <span class="hlt">CAPE</span> ROYAL ROAD VIEW. POST ON RIGHT SIDE OF ROAD, CENTER OF IMAGE, MARKS CULVERT LOCATION. FACING SSW. - <span class="hlt">Cape</span> Royal Road, Between North Entrance Road & <span class="hlt">Cape</span> Royal, Grand Canyon, Coconino County, AZ</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/az0358.photos.180478p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/az0358.photos.180478p/"><span id="translatedtitle">22. ANGEL'S WINDOW TURNOUT ON <span class="hlt">CAPE</span> ROYAL ROAD, FACING NNE. ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>22. ANGEL'S WINDOW TURNOUT ON <span class="hlt">CAPE</span> ROYAL ROAD, FACING NNE. WHITE VAN IS APPROXIMATE CAMERA POSITION FOR PHOTO AZ-40-21. - <span class="hlt">Cape</span> Royal Road, Between North Entrance Road & <span class="hlt">Cape</span> Royal, Grand Canyon, Coconino County, AZ</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/350413','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/350413"><span id="translatedtitle">Mercury deposition in ombrotrophic bogs in New Brunswick, Nova Scotia and Prince Edward Island. Atlantic region surveillance report number EPS-5-AR-98-4</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Rutherford, L.A.; Matthews, S.L.</p> <p>1998-12-31</p> <p>A study was conducted to determine historical atmospheric mercury deposition patterns in the Maritime Provinces. Investigators measured mercury concentrations in peat cores from five ombrotrophic bogs in Kejimkujik, Fundy, Kouchibougouac, and <span class="hlt">Cape</span> <span class="hlt">Breton</span> <span class="hlt">Highlands</span> national parks and in East Baltic Bog, Prince Edward Island. Results presented and discussed include deposition rates calculated using lead-210 date estimates, temporal trends in mercury concentrations, and spatial patterns of mercury deposition.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=295143','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=295143"><span id="translatedtitle">Prospects for biological control of <span class="hlt">Cape</span>-ivy with the <span class="hlt">Cape</span>-ivy fly and the <span class="hlt">cape</span>-ivy moth</span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p><span class="hlt">Cape</span>-ivy (Delairea odorata, Asteraceae), native to coastal floodplains and mountain riparian zones in eastern South Africa, is an invasive vine in coastal riparian, woodland and scrub habitats in California and southern Oregon. <span class="hlt">Cape</span>-ivy smothers native vegetation and may impair water flow in coastal...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0772/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0772/"><span id="translatedtitle"><span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, Solid Rocket ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p><span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, Solid Rocket Booster Disassembly & Refurbishment Complex, Thrust Vector Control Deservicing Facility, Hangar Road, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-04-22/pdf/2011-9779.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-04-22/pdf/2011-9779.pdf"><span id="translatedtitle">76 FR 22719 - <span class="hlt">Cape</span> Wind Energy Project</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-04-22</p> <p>...: Michelle Morin, BOEMRE Office of Offshore Alternative Energy Programs, 381 Elden Street, MS 4090, Herndon... to approve the <span class="hlt">Cape</span> Wind Energy Project COP, BOEMRE considered alternatives to the Proposed Action... Bureau of Ocean Energy Management, Regulation and Enforcement <span class="hlt">Cape</span> Wind Energy Project AGENCY: Bureau...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Whaling&pg=3&id=ED161773','ERIC'); return false;" href="http://eric.ed.gov/?q=Whaling&pg=3&id=ED161773"><span id="translatedtitle"><span class="hlt">Cape</span> Verdeans in America: Our Story.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Almeida, Raymond Anthony, Ed.</p> <p></p> <p>Immigration and acculturation of <span class="hlt">Cape</span> Verdeans in the United States from the mid-19th century to the present are discussed. Emphasis is on the period prior to 1922, at which time the United States Congress enacted new laws restricting the immigration of people of color. The <span class="hlt">Cape</span> Verde islands are located in the Atlantic off the coast of West…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=165743&keyword=laptop&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68433610&CFTOKEN=33256048','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=165743&keyword=laptop&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68433610&CFTOKEN=33256048"><span id="translatedtitle"><span class="hlt">CAPE</span>-OPEN WITH .NET TRAINING COURSE</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>On March 7, 2007 in Heidelberg, Germany, the <span class="hlt">CAPE</span>-OPEN Laboratories Network (CO-LaN) is offering a one-day training seminar on implementing <span class="hlt">CAPE</span>-OPEN compliant process modeling components (PMCs) using .NET-based development tools. This seminar will be geared to component develope...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5619624','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5619624"><span id="translatedtitle">Lithology and strontium distribution of De Queen limestone at main <span class="hlt">Highland</span> Gypsum Quarry, <span class="hlt">Highland</span>, Arkansas</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Slaughter, T.A.; Ledger, E.B.; Sartin, A.A.</p> <p>1987-09-01</p> <p>The De Queen Limestone (Comanchean, Cretaceous) in the main <span class="hlt">Highland</span> Gypsum quarry at <span class="hlt">Highland</span>, Arkansas, consists of gypsum, limestone, and clastic sediments deposited along the landward margin of a broad, restricted, shallow lagoon. It grades downdip into the Ferry Lake Anhydrite. Gypsum, in the form of satin spar, selenite, and alabaster, is abundant in the lower part of the section. Limestones ranging from lime mudstones to grainstones contain fossil mollusks, ostracods, serpulid worm tubes, and foraminifera. The gypsum and limestone lithologies are interbedded with claystones and shales. Strontium concentration was determined on about 100 samples by x-ray fluorescence spectrometry (XRF) and was found to be controlled by diagenesis, not deposition. Strontium concentrations in the gypsum are likely controlled by the rate of recrystallization of secondary anhydrite. Levels of strontium in the limestones reflect the amount of celestite cement. The strontium content of the clastic beds correlates with the amount of strontium-rich microcrystals of strontianite, celestite, barite, and witherite.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17794192','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17794192"><span id="translatedtitle">Classic to postclassic in <span class="hlt">highland</span> central Mexico.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dumond, D E; Muller, F</p> <p>1972-03-17</p> <p>The data and argument we have presented converge on three points. 1) With the decline and abandonment of Teotihuacan by the end of the Metepec phase (Teotihuacan IV), the valleys of Mexico and of Puebla-Tlax-cala witnessed the development of a ceramic culture that was represented, on the one hand, by obvious Teotihuacan derivations in presumably ritual ware and possible Teotihuacan derivations in simpler pottery of red-on-buff, and, on the other hand, by elements that seem to represent a resurgence of Preclassic characteristics. Whether the development is explained through a measure of outside influence or as a local phenomenon, the direct derivation of a substantial portion of the complex from Classic Teotihuacan is unmistakable. This transitional horizon predated the arrival of plumbate tradeware in <span class="hlt">highland</span> central Mexico. 2) The transitional horizon coincided with (and no doubt was an integral part of) an alteration of Classic settlement patterns so drastic that it must bespeak political disruption. Nevertheless, there is no evidence that the Postclassic center of Tula represented a significant force in the <span class="hlt">highlands</span> at that time. There is no evidence that the center of Cholula, which may even have been substantially abandoned during the previous period, was able to exert any force at this juncture; it appears more likely that Cholula was largely reoccupied after the abandonment of Teotihuacan. There is no direct evidence of domination by Xochicalco or any other known major foreign center, although some ceramic traits suggest that relatively minor influences may have emanated from Xochicalco; unfortunately, the state of research at that center does not permit a determination at this time. Thus the most reasonable view on the basis of present evidence is that the abandonment of Teotihuacan was not the direct result of the strength of another centralized power, although some outside populations may have been involved in a minor way. Whatever the proximate cause</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19890023492&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3D%2528metamorphic%2Brock%2529','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19890023492&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3D%2528metamorphic%2Brock%2529"><span id="translatedtitle">Apennine Front revisited - Diversity of Apollo 15 <span class="hlt">highland</span> rock types</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lindstrom, Marilyn M.; Marvin, Ursula B.; Vetter, Scott K.; Shervais, John W.</p> <p>1988-01-01</p> <p>The Apollo 15 landing site is geologically the most complex of the Apollo sites, situated at a mare-<span class="hlt">highland</span> interface within the rings of two of the last major basin-forming impacts. Few of the Apollo 15 samples are ancient <span class="hlt">highland</span> rocks derived from the early differentiation of the moon, or impact melts from major basin impacts. Most of the samples are regolith breccias containing abundant clasts of younger volcanic mare and KREEP basalts. The early geologic evolution of the region can be understood only by examining the small fragments of <span class="hlt">highland</span> rocks found in regolith breccias and soils. Geochemical and petrologic studies of clasts and matrices of three impact melt breccias and four regolith breccias are presented. Twelve igneous and metamorphic rocks show extreme diversity and include a new type of ferroan norite. Twenty-five samples of <span class="hlt">highland</span> impact melt are divided into groups based on composition. These impact melts form nearly a continuum over more than an order of magnitude in REE concentrations. This continuum may result from both major basin impacts and younger local events. <span class="hlt">Highland</span> rocks from the Apennine Front include most of the <span class="hlt">highland</span> rock types found at all of the other sites. An extreme diversity of <span class="hlt">highland</span> rocks is a fundamental characteristic of the Apennine Front and is a natural result of its complex geologic evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780057774&hterms=scandium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dscandium','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780057774&hterms=scandium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3Dscandium"><span id="translatedtitle">SCCRV, a major component of <span class="hlt">highlands</span> rocks</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wasson, J. T.; Warren, P. H.; Kallemeyn, G. W.; Mcewing, C. E.; Mittlefehldt, D. W.; Boynton, W. V.</p> <p>1977-01-01</p> <p>An investigation was conducted of the composition of lunar <span class="hlt">highlands</span> samples rich in mafics. Most of the samples were Apollo 16 rocks. The compositional data for 13 lunar rocks are listed in a table. The nonpristine rocks 64815 and 77545 having essentially identical KREEP contents of about 32% have very similar, high contents of the mafic component SCCRV. The same amounts of rather similar ingredients were mixed at locations 1000 km apart. The composition of SCCRV is discussed. According to the three most plausible hypotheses for the origin of SCCRV which are proposed the SCCRV is primordial material, SCCRV consists entirely or mainly of a single type of lunar rock, or SCCRV resulted from the mixing of two or more lunar materials.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/7242698','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/7242698"><span id="translatedtitle">Seismic activity noted at Medicine Lake <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Blum, D.</p> <p>1988-12-01</p> <p>The sudden rumble of earthquakes beneath Medicine Lake <span class="hlt">Highlands</span> this fall gave geologists an early warning that one of Northern California's volcanoes may be stirring back to life. Researchers stressed that an eruption of the volcano is not expected soon. But the flurry of underground shocks in late September, combined with new evidence of a pool of molten rock beneath the big volcano, has led them to monitor Medicine Lake with new wariness. The volcano has been dormant since 1910, when it ejected a brief flurry of ash - worrying no one. A federal team plans to take measurements of Medicine Lake, testing for changes in its shape caused by underground pressures. The work is scheduled for spring because snows have made the volcano inaccessible. But the new seismic network is an effective lookout, sensitive to very small increases in activity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19840051233&hterms=nitrogen+soil&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dnitrogen%2Bsoil','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19840051233&hterms=nitrogen+soil&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dnitrogen%2Bsoil"><span id="translatedtitle">Nitrogen isotopes in lunar <span class="hlt">highlands</span> breccias</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Fourcade, S.; Clayton, R. N.</p> <p>1984-01-01</p> <p>Lunar <span class="hlt">highlands</span> breccias from Apollo 14 and 16 which may have trapped solar wind gases at a very early epoch in the history of the moon, as implied by their high content of parentless fissiogenic xenon and sometimes of parentless radiogenic Xe-129, are analyzed for nitrogen content and isotopic composition using stepwise heating techniques. The results show that the nitrogen is not particularly light and was not acquired in very ancient times. The conflicting presence of both parentless xenon and nitrogen of relatively recent isotopic signature can be explained if the hypothetical light nitrogen is diluted by more abundant, heavier nitrogen. Accordingly, the very ancient soil components implied in these breccias by the presence of excess fission xenon were reexposed at a much later epoch, or mixed with younger soil components, before the compaction event.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/7328441','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/7328441"><span id="translatedtitle">Nutritional status of Papua New Guinea <span class="hlt">highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Okuda, T; Kajiwara, N; Date, C; Sugimoto, K; Rikimaru, T; Fujita, Y; Koishi, H</p> <p>1981-01-01</p> <p>A nutritional survey was held in August, 1978, at Kalugaluvi (altitude: 1,500m) near Lufa, which is 60 km from Goroka, in the Eastern <span class="hlt">Highland</span> Province of Papua New Guinea. Anthropometric measurements were carried out on 55 males and 37 females aged from 7 to 64 years. whereas the physiques of the children looked as good as those of Japanese of a comparable age, the adult men were shorter than Japanese males, but body weight and chest girth were similar. The skinfold thickness was less than that of the Japanese. From the data collected, it was shown that the physique of the <span class="hlt">Highlanders</span> was more muscular than that of the Japanese. The food intakes and energy balances of 18 healthy men (20-40 years old) were measured over 2 or 3 consecutive days. The average consumption of sweet potatoes, the staple food, was 956 +/- 305 g per day. The average consumption of taro and yam was 93 +/- 124 g/day and 36 +/- 99 g/day, respectively. Various green leaves, sugar canes, corn, bananas and other foods. (i.e., rice and tinned fish) purchased from trade stores were sometimes eaten. The mean daily energy intake was 2.390 +/- 540 kcal, which was about the same as the daily energy expenditure. The daily protein intake was 35.2 +/- 10.7 g. These results are probably exceptionally high, because the survey was unfortunately held during the yearly festival season of the village when the people often ate fatty port. Nevertheless, it is noteworthy that the growth of children and the physique of adults are normal in spite of the extremely low intake of protein. PMID:7328441</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008DPS....40.0304W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008DPS....40.0304W"><span id="translatedtitle">Hydrated Minerals in the Martian Southern <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wray, James J.; Seelos, F. P.; Murchie, S. L.; Squyres, S. W.</p> <p>2008-09-01</p> <p>Hydrated minerals including sulfates, phyllosilicates, and hydrated silica have been observed on the surface of Mars by the orbital near-infrared spectrometers OMEGA and CRISM [1,2]. Global maps from OMEGA [3,4] show that km-scale and larger exposures of these minerals are scattered widely throughout the planet's low and mid latitudes, but are relatively rare. Yet CRISM has found hundreds to thousands of Fe/Mg-phyllosilicate exposures in the <span class="hlt">highlands</span> of Terra Tyrrhena alone [2], suggesting that smaller exposures may be much more common. To search for such exposures, we have surveyed the browse products from all PDS-released CRISM targeted observations (as of July 2008) across a large fraction of the Southern <span class="hlt">highlands</span>, including the Noachis, Cimmeria, and Sirenum regions. Sulfates are observed in Noachian-aged terrains in each of these regions, including as far South as -63º latitude, suggesting that sulfate formation may have occurred locally or regionally throughout a large fraction of Martian history. Some of our strongest phyllosilicate detections occur adjacent to inferred chloride-bearing deposits [5] in Terra Sirenum. Also in Sirenum, the D 100 km Columbus crater contains light-toned, hydrated sulfate-bearing layers overlying materials that contain both a kaolin group clay and Fe/Mg-smectite clay, in different locations. However, phyllosilicates do not appear predominantly associated with impact craters in the regions surveyed, in contrast with Terra Tyrrhena [2]. We are currently searching for additional hydrated mineral exposures using CRISM multispectral data, providing further detail on their global distribution and identifying local areas of interest for future focused studies. [1] Bibring, J.-P. et al. (2005) Science 307, 1576-1581. [2] Mustard, J. F. et al. (2008) Nature 454, 305-309. [3] Bibring, J.-P. et al. (2006) Science 312, 400-404. [4] Poulet, F. et al. (2007) Mars 7, Abs. #3170. [5] Osterloo M. M. et al. (2008) Science 319, 1651-1654.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16..145H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16..145H"><span id="translatedtitle">Sustainable Land Management in the Ethiopian <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Haile, Mitiku; Nyssen, Jan; Araya, Tesfay</p> <p>2014-05-01</p> <p>Through centuries of farming practices the farmers and pastoralists in Ethiopia were managing their land resources pertaining to the needs of prevalent populations. With an increasing population and growing demands, more land was put under cultivation. Subsequently forest areas were cleared, encroaching agriculture into steep slopes and areas that were not suitable for agricultural activities. Land degradation and particularly soil erosion by water not only reduced the productivity of the land but also aggravated the effects of drought, such as famine and migration. Obvious signs of degradation in the <span class="hlt">highlands</span> of Ethiopia are wide gullies swallowing fertile lands and rock outcrops making farming a risky business. But also less visible sheet erosion processes result in a tremendous loss of fertile topsoil, particularly on cropland. Efforts have been made by the farming communities to mitigate land degradation by developing local practices of conserving soil and water. With keen interest and openness one can observe such indigenous practices in all corners of Ethiopia. Notwithstanding these practices, there were also efforts to introduce other soil and water conservation interventions to control erosion and retain the eroded soils. Since the early 1980s numerous campaigns were carried out to build terraces in farmlands and sloping areas. Major emphasis was given to structural technologies rather than on vegetative measures. Currently the landscape of the northern <span class="hlt">highlands</span> is dotted with millions of hectares of terraced fields and in some places with planned watershed management interventions including exclosures. Apparently these interventions were introduced without prior investigating the detailed problems and conservation needs of the local population. Intensive research is undertaken on the processes of degradation, the impact of the different intervention measures and the role of communities in sustainably managing their land. This paper attempts to review the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/7328441','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/7328441"><span id="translatedtitle">Nutritional status of Papua New Guinea <span class="hlt">highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Okuda, T; Kajiwara, N; Date, C; Sugimoto, K; Rikimaru, T; Fujita, Y; Koishi, H</p> <p>1981-01-01</p> <p>A nutritional survey was held in August, 1978, at Kalugaluvi (altitude: 1,500m) near Lufa, which is 60 km from Goroka, in the Eastern <span class="hlt">Highland</span> Province of Papua New Guinea. Anthropometric measurements were carried out on 55 males and 37 females aged from 7 to 64 years. whereas the physiques of the children looked as good as those of Japanese of a comparable age, the adult men were shorter than Japanese males, but body weight and chest girth were similar. The skinfold thickness was less than that of the Japanese. From the data collected, it was shown that the physique of the <span class="hlt">Highlanders</span> was more muscular than that of the Japanese. The food intakes and energy balances of 18 healthy men (20-40 years old) were measured over 2 or 3 consecutive days. The average consumption of sweet potatoes, the staple food, was 956 +/- 305 g per day. The average consumption of taro and yam was 93 +/- 124 g/day and 36 +/- 99 g/day, respectively. Various green leaves, sugar canes, corn, bananas and other foods. (i.e., rice and tinned fish) purchased from trade stores were sometimes eaten. The mean daily energy intake was 2.390 +/- 540 kcal, which was about the same as the daily energy expenditure. The daily protein intake was 35.2 +/- 10.7 g. These results are probably exceptionally high, because the survey was unfortunately held during the yearly festival season of the village when the people often ate fatty port. Nevertheless, it is noteworthy that the growth of children and the physique of adults are normal in spite of the extremely low intake of protein.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/me0205.photos.338711p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/me0205.photos.338711p/"><span id="translatedtitle">3. View from former light tower to <span class="hlt">Cape</span> Elizabeth Light ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>3. View from former light tower to <span class="hlt">Cape</span> Elizabeth Light Tower, view northeast, southwest side of <span class="hlt">Cape</span> Elizabeth Tower - <span class="hlt">Cape</span> Elizabeth Light Station, Near Two Lights State Park at end of Two Lights Road, off State Highway 77, <span class="hlt">Cape</span> Elizabeth, Cumberland County, ME</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_6 --> <div id="page_7" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="121"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/19366475','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/19366475"><span id="translatedtitle">Host use and crop impacts of Oribius Marshall species (Coleoptera: Curculionidae) in Eastern <span class="hlt">Highlands</span> Province, Papua New Guinea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wesis, P; Niangu, B; Ero, M; Masamdu, R; Autai, M; Elmouttie, D; Clarke, A R</p> <p>2010-04-01</p> <p>Oribius species are small flightless weevils endemic to the island of New Guinea and far northern <span class="hlt">Cape</span> York, Australia. The adults feed externally on leaves, developing fruit and green bark, but their impact as pests and general host use patterns are poorly known. Working in Eastern <span class="hlt">Highlands</span> Province, Papua New Guinea, we carried out structured host use surveys, farmer surveys, shade-house growth trials and on-farm and on-station impact trials to: (i) estimate the host range of the local Oribius species; (ii) understand adult daily activity patterns; (iii) elucidate feeding habits of the soil dwelling larvae; and (iv) quantify the impacts of adult feeding damage. Oribius inimicus and O. destructor accounted for nearly all the Oribius species encountered locally, of these two O. inimicus was the most abundant. Weevils were collected from 31 of 33 plants surveyed in the Aiyura Valley, and a combination of farmer interviews and literature records provided evidence for the beetles being pestiferous on 43 crops currently or previously grown in the <span class="hlt">Highlands</span>. Adult weevils had a distinct diurnal pattern of being in the upper plant canopy early in the morning and, to a lesser extent, again late in the afternoon. For the remainder of the day, beetles resided within the canopy, or possibly off the plant. Movement of adults between plants appeared frequent. Pot trials confirmed the larvae are root feeders. Quantified impact studies showed that the weevils are damaging to a range of vegetable and orchard crops (broccoli, capsicum, celery, French bean, Irish potato, lettuce, orange and strawberry), causing average yield losses of around 30-40%, but up to 100% on citrus. Oribius weevils pose a significant and, apparently, growing problem for <span class="hlt">Highland</span>'s agriculture. PMID:19366475</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-07-06/pdf/2011-16915.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-07-06/pdf/2011-16915.pdf"><span id="translatedtitle">76 FR 39298 - Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, and Northeast <span class="hlt">Cape</span> Fear River, in Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-07-06</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, and Northeast <span class="hlt">Cape</span> Fear River, in Wilmington, NC AGENCY: Coast Guard, DHS. ACTION: Notice of temporary deviation from... regulation governing the operation of the <span class="hlt">Cape</span> Fear River Memorial Bridge across the <span class="hlt">Cape</span> Fear River, mile...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-09-09/pdf/2010-22415.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-09-09/pdf/2010-22415.pdf"><span id="translatedtitle">75 FR 54770 - Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River and Northeast <span class="hlt">Cape</span> Fear River, in Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-09-09</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River and Northeast <span class="hlt">Cape</span> Fear River, in Wilmington, NC AGENCY: Coast Guard, DHS. ACTION: Notice of temporary deviation from...: The <span class="hlt">Cape</span> Fear River Memorial Bridge, across <span class="hlt">Cape</span> Fear River, mile 26.8, and the Isabel S....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA10104&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA10104&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde"><span id="translatedtitle"><span class="hlt">Cape</span> Verde in False Color</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2007-01-01</p> <p><p/> A promontory nicknamed '<span class="hlt">Cape</span> Verde' can be seen jutting out from the walls of Victoria Crater in this false-color picture taken by the panoramic camera on NASA's Mars Exploration Rover Opportunity. The rover took this picture on martian day, or sol, 1329 (Oct. 20, 2007), more than a month after it began descending down the crater walls -- and just 9 sols shy of its second Martian birthday on sol 1338 (Oct. 29, 2007). Opportunity landed on the Red Planet on Jan. 25, 2004. That's nearly four years ago on Earth, but only two on Mars because Mars takes longer to travel around the sun than Earth. One Martian year equals 687 Earth days. <p/> This view was taken using three panoramic-camera filters, admitting light with wavelengths centered at 750 nanometers (near infrared), 530 nanometers (green) and 430 nanometers (violet).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120011125','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120011125"><span id="translatedtitle">What Lunar Meteorites Tell Us About the Lunar <span class="hlt">Highlands</span> Crust</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Korotev, R. L.; Jolliff, B. L.; Zeigler, R. A.</p> <p>2012-01-01</p> <p>The first meteorite to be found1 that was eventually (1984) recognized to have originated from the Moon is Yamato 791197. The find date, November 20, 1979, was four days after the end of the first Conference on the Lunar <span class="hlt">Highland</span> Crust. Since then, >75 other lunar meteorites have been found, and these meteorites provide information about the lunar <span class="hlt">highlands</span> that was not known from studies of the Apollo and Luna samples</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/500794','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/500794"><span id="translatedtitle">New York/New Jersey <span class="hlt">Highlands</span> -- ecological and economic sustainability</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Gray, C.</p> <p>1997-08-01</p> <p>The New York/New Jersey <span class="hlt">Highlands</span> region is one million acres of Appalachian ridges and valleys that stretch from the Hudson to the Delaware River. The spatial relationship of <span class="hlt">Highlands</span> to the New York/New Jersey metropolitan area provides a unique opportunity for regional development. The New Jersey <span class="hlt">Highlands</span> Region, stretching from the Hudson River to the Delaware River, is an area critical to the overall environmental quality of the nation`s largest metropolitan area. However, there is substantial development pressure in this region. The way in which the <span class="hlt">Highlands</span> Region is developed in the near future will have long-lasting effects. Patterns of population density, water use, pollution and resource consumption are difficult to rectify once established. All indications point to the <span class="hlt">Highlands</span> becoming the latest addition to the urban sprawl of the New York/New Jersey metropolitan areas. Great cooperation and motivation would be required to change this pattern. This paper will attempt to explore the ecological merits of a <span class="hlt">Highland</span> greenway proposal, the economic impacts and possible planning techniques which might effect a win/win situation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24575229','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24575229"><span id="translatedtitle">Diversity of fusarium species from <span class="hlt">highland</span> areas in malaysia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Manshor, Nurhazrati; Rosli, Hafizi; Ismail, Nor Azliza; Salleh, Baharuddin; Zakaria, Latiffah</p> <p>2012-12-01</p> <p>Fusarium is a cosmopolitan and highly diversified genus of saprophytic, phytopathogenic and toxigenic fungi. However, the existence and diversity of a few species of Fusarium are restricted to a certain area or climatic condition. The present study was conducted to determine the occurrence and diversity of Fusarium species in tropical <span class="hlt">highland</span> areas in Malaysia and to compare with those in temperate and subtropical regions. A series of sampling was carried out in 2005 to 2009 at several tropical <span class="hlt">highland</span> areas in Malaysia that is: Cameron <span class="hlt">Highlands</span>, Fraser Hills and Genting <span class="hlt">Highlands</span> in Pahang; Penang Hill in Penang; Gunung Jerai in Kedah; Kundasang and Kinabalu Park in Sabah; Kubah National Park and Begunan Hill in Sarawak. Sampling was done randomly from various hosts and substrates. Isolation of Fusarium isolates was done by using pentachloronitrobenzene (PCNB) agar and 1449 isolates of Fusarium were successfully recovered. Based on morphological characteristics, 20 species of Fusarium were identified. The most prevalent species occurring on the <span class="hlt">highlands</span> areas was F. solani (66.1%) followed by F. graminearum (8.5%), F. oxysporum (7.8%), F. semitectum (5.7%), F. subglutinans (3.5%) and F. proliferatum (3.4%). Other Fusarium species, namely F. avenaceum, F. camptoceras, F. chlamydosporum, F. compactum, F. crookwellense, F. culmorum, F. decemcellulare, F. equiseti, F. nygamai, F. poae, F. proliferatum, F. sacchari, F. sporotrichioides, F. sterilihyphosum and F. verticillioides accounted for 1% recoveries. The present study was the first report on the occurrences of Fusarium species on <span class="hlt">highland</span> areas in Malaysia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3799405','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3799405"><span id="translatedtitle">Diversity of Fusarium Species from <span class="hlt">Highland</span> Areas in Malaysia</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Manshor, Nurhazrati; Rosli, Hafizi; Ismail, Nor Azliza; Salleh, Baharuddin; Zakaria, Latiffah</p> <p>2012-01-01</p> <p>Fusarium is a cosmopolitan and highly diversified genus of saprophytic, phytopathogenic and toxigenic fungi. However, the existence and diversity of a few species of Fusarium are restricted to a certain area or climatic condition. The present study was conducted to determine the occurrence and diversity of Fusarium species in tropical <span class="hlt">highland</span> areas in Malaysia and to compare with those in temperate and subtropical regions. A series of sampling was carried out in 2005 to 2009 at several tropical <span class="hlt">highland</span> areas in Malaysia that is: Cameron <span class="hlt">Highlands</span>, Fraser Hills and Genting <span class="hlt">Highlands</span> in Pahang; Penang Hill in Penang; Gunung Jerai in Kedah; Kundasang and Kinabalu Park in Sabah; Kubah National Park and Begunan Hill in Sarawak. Sampling was done randomly from various hosts and substrates. Isolation of Fusarium isolates was done by using pentachloronitrobenzene (PCNB) agar and 1449 isolates of Fusarium were successfully recovered. Based on morphological characteristics, 20 species of Fusarium were identified. The most prevalent species occurring on the <span class="hlt">highlands</span> areas was F. solani (66.1%) followed by F. graminearum (8.5%), F. oxysporum (7.8%), F. semitectum (5.7%), F. subglutinans (3.5%) and F. proliferatum (3.4%). Other Fusarium species, namely F. avenaceum, F. camptoceras, F. chlamydosporum, F. compactum, F. crookwellense, F. culmorum, F. decemcellulare, F. equiseti, F. nygamai, F. poae, F. proliferatum, F. sacchari, F. sporotrichioides, F. sterilihyphosum and F. verticillioides accounted for 1% recoveries. The present study was the first report on the occurrences of Fusarium species on <span class="hlt">highland</span> areas in Malaysia. PMID:24575229</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2564045','PMC'); return false;" href="http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2564045"><span id="translatedtitle">The <span class="hlt">cape</span> triage score: a new triage system South Africa. Proposal from the <span class="hlt">cape</span> triage group</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Gottschalk, S B; Wood, D; DeVries, S; Wallis, L A; Bruijns, S</p> <p>2006-01-01</p> <p>The <span class="hlt">Cape</span> Triage Group (CTG) convened with the intention of producing a triage system for the Western <span class="hlt">Cape</span>, and eventually South Africa. The group includes in-hospital and prehospital staff from varied backgrounds. The CTG triage protocol is termed the <span class="hlt">Cape</span> Triage Score (CTG), and has been developed by a multi-disciplinary panel, through best available evidence and expert opinion. The CTS has been validated in several studies, and was launched across the Western <span class="hlt">Cape</span> on 1 January 2006. The CTG would value feedback from readers of this journal, as part of the ongoing monitoring and evaluation process. PMID:16439753</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=STS030-151-025&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3D5w','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=STS030-151-025&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3D5w"><span id="translatedtitle"><span class="hlt">Cape</span> Canaveral, Kennedy Space Center, Florida</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1989-01-01</p> <p>This overhead view of the central eastern shore of Florida shows the <span class="hlt">Cape</span> Canaveral and Kennedy Space Center (28.5N, 80.5W), where all of the NASA manned space missions originate. Sprinkled along the jutting <span class="hlt">cape</span> are a number of KSC launch pads and the nearby Space Shuttle Landing Facility. Merritt Island, just south of Kennedy Space Center is where the spacecraft liftoff tracking station is located. Orlando is on the left edge of photo.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19740060877&hterms=hugging&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dhugging','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19740060877&hterms=hugging&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dhugging"><span id="translatedtitle">Lunar basin formation and <span class="hlt">highland</span> stratigraphy</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Howard, K. A.; Wilhelms, D. E.; Scott, D. H.</p> <p>1974-01-01</p> <p>Multiring impact basins, formed after solidification of the lunar crust, account for most or all premare regional deposits and structures expressed in the lunar landscape and for major topographic and gravity variations. A fresh basin has two or more concentric mountain rings, a lineated ejecta blanket, and secondary impact craters. Crackled material on the floor may be impact melt. The ejecta blanket was emplaced at least partly as a ground-hugging flow and was probably hot. A suggested model of basin formation is that the center lifts up and the rings form by inward collapse during evisceration. The resulting basin is shallow and has a central uplift of the mantle. This results in a central gravity high and a ring low. Later flooding by mare basalt has since modified most near side basins. <span class="hlt">Highland</span> deposits of plains, furrowed and pitted terrain, and various hills, domes, and craters that were interpreted before the Apollo missions as being volcanic can now be interpreted as being basin related.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2600205','PMC'); return false;" href="http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2600205"><span id="translatedtitle">Diagnosis of Cystic Echinococcosis, Central Peruvian <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Gonzalez, Armando E.; Zhang, Wenbao; McManus, Donald P.; Lopera, Luis; Ninaquispe, Berenice; Garcia, Hector H.; Rodríguez, Silvia; Verastegui, Manuela; Calderon, Carmen; Pan, William K.Y.; Gilman, Robert H.</p> <p>2008-01-01</p> <p>We evaluated prevalence of cystic echinococcosis (CE) in a central Peruvian <span class="hlt">Highland</span> district by using 4 diagnostic methods: ultrasonography for 949 persons, radiography for 829, and 2 serologic tests for 929 (2 immunoblot formats using bovine hydatid cyst fluid [IBCF] and recombinant EpC1 glutathione S-transferase [rEpC1-GST] antigens). For the IBCF and rEpC1-GST testing, prevalence of liver and pulmonary CE was 4.7% and 1.1% and seropositivity was 8.9% and 19.7%, respectively. Frequency of seropositive results for IBCF and rEpC1-GST testing was 35.7% and 16.7% (all hepatic cysts), 47.1% and 29.4% (hepatic calcifications excluded), and 22.2% and 33.3% (lung cysts), respectively. Weak immune response against lung cysts, calcified cysts, small cysts, and cysts in sites other than lung and liver might explain the poor performance of the serodiagnostic tests. We confirm that CE is highly endemic to Peru and emphasize the limited performance of available serologic assays in the field. PMID:18258119</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70034787','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70034787"><span id="translatedtitle">'<span class="hlt">Cape</span> capture': Geologic data and modeling results suggest the holocene loss of a Carolina <span class="hlt">Cape</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Thieler, E.R.; Ashton, A.D.</p> <p>2011-01-01</p> <p>For more than a century, the origin and evolution of the set of cuspate forelands known as the Carolina <span class="hlt">Capes</span>-Hatteras, Lookout, Fear, and Romain-off the eastern coast of the United States have been discussed and debated. The consensus conceptual model is not only that these <span class="hlt">capes</span> existed through much or all of the Holocene transgression, but also that their number has not changed. Here we describe bathymetric, lithologic, seismic, and chronologic data that suggest another <span class="hlt">cape</span> may have existed between <span class="hlt">Capes</span> Hatteras and Lookout during the early to middle Holocene. This <span class="hlt">cape</span> likely formed at the distal end of the Neuse-Tar-Pamlico fiuvial system during the early Holocene transgression, when this portion of the shelf was fiooded ca. 9 cal (calibrated) kyr B.P., and was probably abandoned by ca. 4 cal kyr B.P., when the shoreline attained its present general configuration. Previously proposed mechanisms for <span class="hlt">cape</span> formation suggest that the large-scale, rhythmic pattern of the Carolina <span class="hlt">Capes</span> arose from a hydrodynamic template or the preexisting geologic framework. Numerical modeling, however, suggests that the number and spacing of <span class="hlt">capes</span> can be dynamic, and that a coast can self-organize in response to a high-angle-wave instability in shoreline shape. In shoreline evolution model simulations, smaller cuspate forelands are subsumed by larger neighbors over millennial time scales through a process of '<span class="hlt">cape</span> capture.' The suggested former <span class="hlt">cape</span> in Raleigh Bay represents the first interpreted geological evidence of dynamic abandonment suggested by the self-organization hypothesis. <span class="hlt">Cape</span> capture may be a widespread process in coastal environments with large-scale rhythmic shoreline features; its preservation in the sedimentary record will vary according to geologic setting, physical processes, and sea-level history. ?? 2011 Geological Society of America.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19950009780','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19950009780"><span id="translatedtitle">Tartarus Colles: A sampling of the Martian <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Murchie, Scott; Treiman, Allan</p> <p>1994-01-01</p> <p>Several of the most fundamental issues about the geology of Mars can be addressed using information on composition and structure of the plateau plains ('<span class="hlt">highlands</span>') that cover approximately half the planet. The units that compose the <span class="hlt">highlands</span> are interpreted as a mixture of volcanic, fluvial, lacustrine, and impact ejecta deposits. A more precise inventory of differing of igneous and sedimentary lithologies in <span class="hlt">highland</span> rock units would not only lead to a better understanding of how the plateau plains formed, but would also clarify the nature of the surface environment during the first 800 m.y. of martian history. Structural features including bedforms, joints, and small faults that are unresolved from orbit record a history of the emplacement and deformation of the <span class="hlt">highlands</span>. In addition, weathering products present in this very ancient terrain represent a mineralogic record of past climate and of the pathways by which bedrock is altered chemically. Their similarity or dissimilarity to bright soils observed spectroscopically and in situ at the Viking Lander sites will be evidence for the relative roles of regional sources and global eolian transport in producing the widespread cover of 'dust.' Unfortunately, these issues are difficult to address in the plateau plains proper, because bedrock is covered by mobile sand and weathering products, which dominate both surface composition and remotely measurable spectral properties. However, the 'Tartarus Colles' site, located at 11.41 deg N, 197.69 deg W at an elevation of -1 km, provides an excellent opportunity to address the <span class="hlt">highland</span> geology within the mission constraints of Mars Pathfinder. The site is mapped as unit HNu, and consists of knobby remnants of deeply eroded <span class="hlt">highlands</span>. It contains rolling hills, but lacks steep escarpments and massifs common in most <span class="hlt">highland</span> remnants, and is free of large channels that would have removed colluvium from eroded upper portions of the stratigraphic column. These</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09103&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09103&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DCape%2BVerde"><span id="translatedtitle">Panorama from '<span class="hlt">Cape</span> Verde' (False Color)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2007-01-01</p> <p><p/> NASA's Mars Exploration Rover Opportunity captured this vista of 'Victoria Crater' from the viewpoint of '<span class="hlt">Cape</span> Verde,' one of the promontories that are part of the scalloped rim of the crater. Opportunity drove onto <span class="hlt">Cape</span> Verde shortly after arriving at the rim of Victoria in September 2006. The view combines hundreds of exposures taken by the rover's panoramic camera (Pancam). The camera began taking the component images during Opportunity's 970th Martian day, or sol, on Mars (Oct. 16, 2006). Work on the panorama continued through the solar conjunction period, when Mars was nearly behind the sun from Earth's perspective and communications were minimized. Acquisition of images for this panorama was completed on Opportunity's 991st sol (Nov. 7, 2006). <p/> The top of <span class="hlt">Cape</span> Verde is in the immediate foreground at the center of the image. To the left and right are two of the more gradually sloped bays that alternate with the cliff-faced <span class="hlt">capes</span> or promontories around the rim of the crater. 'Duck Bay,' where Opportunity first reached the rim, is to the right. Beyond Duck Bay counterclockwise around the rim, the next promontory is 'Cabo Frio,' about 150 meters (500 feet) from the rover. On the left side of the panorama is '<span class="hlt">Cape</span> St. Mary,' the next promontory clockwise from <span class="hlt">Cape</span> Verde and about 40 meters (130 feet) from the rover. The vantage point atop <span class="hlt">Cape</span> Verde offered a good view of the rock layers in the cliff face of <span class="hlt">Cape</span> St. Mary, which is about 15 meters or 50 feet tall. By about two weeks after the Pancam finished collecting the images for this panorama, Opportunity had driven to <span class="hlt">Cape</span> St. Mary and was photographing <span class="hlt">Cape</span> Verde's rock layers. <p/> The far side of the crater lies about 800 meters (half a mile) away, toward the southeast. <p/> This view combines images taken through three of the Pancam's filters, admitting light with wavelengths centered at 750 nanometers (near infrared), 530 nanometers (green) and 430 nanometers (violet). It is presented in false</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009ECSS...83...97P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009ECSS...83...97P"><span id="translatedtitle">The effect of Hurricane Katrina on nekton communities in the tidal freshwater marshes of <span class="hlt">Breton</span> Sound, Louisiana, USA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Piazza, Bryan P.; La Peyre, Megan K.</p> <p>2009-06-01</p> <p>Hurricanes are climatically-induced resource pulses that affect community structure through the combination of physical and chemical habitat change. Estuaries are susceptible to hurricane pulses and are thought to be resilient to habitat change, because biotic communities often return quickly to pre-hurricane conditions. Although several examples provide evidence of quick recovery of estuarine nekton communities following a hurricane, few studies take place in tidal freshwater habitat where physical habitat effects can be extensive and may not be readily mitigated. We examined nekton communities (density, biomass, α and β diversity, % occurrence by residence status) in tidal freshwater marshes in <span class="hlt">Breton</span> Sound, Louisiana, before and after a direct hit by Hurricane Katrina (2005). Vegetative marsh loss in the study area was extensive, and elevated salinity persisted for almost 6 months. Post-Katrina nekton density and biomass increased significantly, and the nekton community shifted from one of tidal freshwater/resident species to one containing brackish/migrant species, many of which are characterized by pelagic and benthic life history strategies. By spring 2007, the nekton community had shifted back to tidal freshwater/resident species, despite the enduring loss of vegetated marsh habitat.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70034684','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70034684"><span id="translatedtitle">The effect of Hurricane Katrina on nekton communities in the tidal freshwater marshes of <span class="hlt">Breton</span> Sound, Louisiana, USA</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Piazza, Bryan P.; La Peyre, M.K.</p> <p>2009-01-01</p> <p>Hurricanes are climatically-induced resource pulses that affect community structure through the combination of physical and chemical habitat change. Estuaries are susceptible to hurricane pulses and are thought to be resilient to habitat change, because biotic communities often return quickly to pre-hurricane conditions. Although several examples provide evidence of quick recovery of estuarine nekton communities following a hurricane, few studies take place in tidal freshwater habitat where physical habitat effects can be extensive and may not be readily mitigated. We examined nekton communities (density, biomass, ?? and ?? diversity, % occurrence by residence status) in tidal freshwater marshes in <span class="hlt">Breton</span> Sound, Louisiana, before and after a direct hit by Hurricane Katrina (2005). Vegetative marsh loss in the study area was extensive, and elevated salinity persisted for almost 6 months. Post-Katrina nekton density and biomass increased significantly, and the nekton community shifted from one of tidal freshwater/resident species to one containing brackish/migrant species, many of which are characterized by pelagic and benthic life history strategies. By spring 2007, the nekton community had shifted back to tidal freshwater/resident species, despite the enduring loss of vegetated marsh habitat. ?? 2009 Elsevier Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930016813','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930016813"><span id="translatedtitle"><span class="hlt">Cape</span> Photographic Durchmusterung, volume 1</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1993-01-01</p> <p>The <span class="hlt">Cape</span> Photographic Durchmusterung (CPD Gill and Kapteyn 1895-1900) is a photographic survey of southern stars in the declination range -18 to -90 degrees. This volume covers the declination range -18 through -37 degrees. Positions are given for the 1875 equinox. The summary of the positional uncertainties quoted in the third volume of the published catalog gives +/- 0.28 sec (R.A.) +/- 0.044 arcmin (Dec.) for zones -18 to -57 degrees. The probable error of a photographic magnitude as determined by combining results for different magnitudes and weighting proportionately according to the numbers of stars in each class of magnitude is given as +/- 0.055 mag. From an analysis of the taint magnitude limits on the plates discussed in the third volume introduction, the catalog as a whole can be considered complete to photographic magnitude 9.2 but it is stated that it will be found practically complete in or near the Milky Way, to magnitude 9.5.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA03396&hterms=waterfall&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dwaterfall','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA03396&hterms=waterfall&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dwaterfall"><span id="translatedtitle">Guiana <span class="hlt">Highlands</span>, Shaded Relief and Colored Height</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2003-01-01</p> <p><p/> [figure removed for brevity, see original site] <p/>These two images show exactly the same area in South America, the Guiana <span class="hlt">Highlands</span> straddling the borders of Venezuela, Guyana and Brazil. The image on the left was created using the best global topographic data set previously available, the U.S. Geological Survey's GTOPO30. In contrast, the image on the right was generated with a new data set recently released by the Shuttle Radar Topography Mission (SRTM) called SRTM30, which represents a significant improvement in our knowledge of the topography of much of the world.<p/>GTOPO30, with a resolution of about 928 meters (1496 feet), was developed over a three-year period and published in 1996, and since then has been the primary source of digital elevation data for scientists and analysts involved in global studies. However, since it was compiled from a number of different map sources with varying attributes, the data for some parts of the globe were inconsistent or of low quality.<p/>The SRTM data, on the other hand, were collected within a ten-day period using the same instrument in a uniform fashion, and were processed into elevation data using consistent processing techniques. Thus SRTM30 provides a new resource of uniform quality for all parts of the Earth, and since the data, which have an intrinsic resolution of about 30 meters, were averaged and resampled to match the GTOPO30 sample spacing and format, and can be used by the same computer software without modification.<p/>The Guiana <span class="hlt">Highlands</span> are part of the Guyana Shield, which lies in northeast South America and represent one of the oldest land surfaces in the world. Chemical weathering over many millions of years has created a landscape of flat-topped table mountains with dramatic, steep cliffs with a large number of spectacular waterfalls. For example Angel Falls, at 979 meters the highest waterfall in the world, plunges from Auyan Tebuy, part of a mesa of the type that may have been the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25665685','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25665685"><span id="translatedtitle">Left ventricular adaptation to high altitude: speckle tracking echocardiography in lowlanders, healthy <span class="hlt">highlanders</span> and <span class="hlt">highlanders</span> with chronic mountain sickness.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dedobbeleer, Chantal; Hadefi, Alia; Pichon, Aurelien; Villafuerte, Francisco; Naeije, Robert; Unger, Philippe</p> <p>2015-04-01</p> <p>Hypoxic exposure depresses myocardial contractility in vitro, but has been associated with indices of increased cardiac performance in intact animals and in humans, possibly related to sympathetic nervous system activation. We explored left ventricular (LV) function using speckle tracking echocardiography and sympathetic tone by spectral analysis of heart rate variability (HRV) in recently acclimatized lowlanders versus adapted or maladapted <span class="hlt">highlanders</span> at high altitude. Twenty-six recently acclimatized lowlanders, 14 healthy <span class="hlt">highlanders</span> and 12 <span class="hlt">highlanders</span> with chronic mountain sickness (CMS) were studied. Control measurements at sea level were also obtained in the lowlanders. Altitude exposure in the lowlanders was associated with slightly increased blood pressure, decreased LV volumes and decreased longitudinal strain with a trend to increased prevalence of post-systolic shortening (p = 0.06), whereas the low frequency/high frequency (LF/HF) ratio increased (1.62 ± 0.81 vs. 5.08 ± 4.13, p < 0.05) indicating sympathetic activation. <span class="hlt">Highlanders</span> had a similarly raised LF/HF ratio, but no alteration in LV deformation. <span class="hlt">Highlanders</span> with CMS had no change in LV deformation, no significant increase in LF/HF, but decreased global HRV still suggestive of increased sympathetic tone, and lower mitral E/A ratio compared to healthy <span class="hlt">highlanders</span>. Short-term altitude exposure in lowlanders alters indices of LV systolic function and increases sympathetic nervous system tone. Life-long altitude exposure in <span class="hlt">highlanders</span> is associated with similar sympathetic hyperactivity, but preserved parameters of LV function, whereas diastolic function may be altered in those with CMS. Altered LV systolic function in recently acclimatized lowlanders may be explained by combined effects of hypoxia and changes in loading conditions.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=20080048268&hterms=Respiratory+system&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528Respiratory%2Bsystem%2529','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=20080048268&hterms=Respiratory+system&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528Respiratory%2Bsystem%2529"><span id="translatedtitle">Respiratory Toxicity of Lunar <span class="hlt">Highland</span> Dust</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>James, John T.; Lam, Chiu-wing; Wallace, William T.</p> <p>2009-01-01</p> <p>Lunar dust exposures occurred during the Apollo missions while the crew was on the lunar surface and especially when microgravity conditions were attained during rendezvous in lunar orbit. Crews reported that the dust was irritating to the eyes and in some cases respiratory symptoms were elicited. NASA s vision for lunar exploration includes stays of 6 months on the lunar surface hence the health effects of periodic exposure to lunar dust need to be assessed. NASA has performed this assessment with a series of in vitro and in vivo tests on authentic lunar dust. Our approach is to "calibrate" the intrinsic toxicity of lunar dust by comparison to a nontoxic dust (TiO2) and a highly toxic dust (quartz) using intratrachael instillation of the dusts in mice. A battery of indices of toxicity is assessed at various time points after the instillations. Cultures of selected cells are exposed to test dusts to assess the adverse effects on the cells. Finally, chemical systems are used to assess the nature of the reactivity of various dusts and to determine the persistence of reactivity under various environmental conditions that are relevant to a space habitat. Similar systems are used to assess the dissolution of the dust. From these studies we will be able to set a defensible inhalation exposure standard for aged dust and predict whether we need a separate standard for reactive dust. Presently-available data suggest that aged lunar <span class="hlt">highland</span> dust is slightly toxic, that it can adversely affect cultured cells, and that the surface reactivity induced by grinding the dust persists for a few hours after activation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/gip/7000013/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/gip/7000013/report.pdf"><span id="translatedtitle">Geologic history of <span class="hlt">Cape</span> Cod, Massachusetts</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>,</p> <p>1976-01-01</p> <p><span class="hlt">Cape</span> Cod, a sandy peninsula built mostly during the Ice Age, juts into the Atlantic Ocean like a crooked arm. Because of its exposed location, <span class="hlt">Cape</span> Cod was visited by many early explorers. Although clear-cut evidence is lacking, the Vikings may have sighted this land about 1,000 years ago. It was visited by Samuel de Champlain in 1605, and his detailed descriptions and charts have helped present-day scientists to determine the rate of growth of Nauset Beach marsh and Nauset spit. Bartholomew Gosnold, a lesser known explorer, settled for a short time on the Elizabeth Islands to the southwest and gave <span class="hlt">Cape</span> Cod its name in 1602. The Pilgrims first landed in America on the tip of Lower <span class="hlt">Cape</span> Cod after they were turned back from their more southerly destination by shoals between <span class="hlt">Cape</span> Cod and Nantucket Island. On <span class="hlt">Cape</span> Cod they found potable water and food and had their first fight with the natives. The Pilgrims, however, decided that this land was too isolated, too exposed, and too sandy to support them, and they sailed across <span class="hlt">Cape</span> Cod Bay to establish Plymouth. These features remain today. Small villages are separated by large areas of forest, dune, beach, and marsh. This unspoiled natural beauty makes <span class="hlt">Cape</span> Cod one of the most favored vacation areas for the people living in the thickly settled Northeastern States. <span class="hlt">Cape</span> Cod is of particular interest to geologists because it was formed by glaciers very recently in terms of geologic time. During the Great Ice Age, (the Pleistocene Epoch which began 2 to 3 million years ago), glaciers advanced from the north into the temperate regions of the Earth. Glacial ice covered the land at least four times. Each advance was accompanied by a worldwide lowering of sea level because the source of the ice was water from the seas. When the glaciers melted, the climate and sea level were probably much like they are today. In fact, some scientists believe that the Earth is presently between glacial episodes and that ice once again will</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/22365762','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/22365762"><span id="translatedtitle">EARTHSHINE ON A YOUNG MOON: EXPLAINING THE LUNAR FARSIDE <span class="hlt">HIGHLANDS</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Roy, Arpita; Wright, Jason T.; Sigurðsson, Steinn</p> <p>2014-06-20</p> <p>The lunar farside <span class="hlt">highlands</span> problem refers to the curious and unexplained fact that the farside lunar crust is thicker, on average, than the nearside crust. Here we recognize the crucial influence of Earthshine, and propose that it naturally explains this hemispheric dichotomy. Since the accreting Moon rapidly achieved synchronous rotation, a surface and atmospheric thermal gradient was imposed by the proximity of the hot, post-giant impact Earth. This gradient guided condensation of atmospheric and accreting material, preferentially depositing crust-forming refractories on the cooler farside, resulting in a primordial bulk chemical inhomogeneity that seeded the crustal asymmetry. Our model provides a causal solution to the lunar <span class="hlt">highlands</span> problem: the thermal gradient created by Earthshine produced the chemical gradient responsible for the crust thickness dichotomy that defines the lunar <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/6148580','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/6148580"><span id="translatedtitle">Predicting potential effects of climate change on Ozark <span class="hlt">Highlands</span> streams</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Willson, G.D.; Rabeni, C.F.; Galat, D.L. )</p> <p>1993-06-01</p> <p>The Ozark <span class="hlt">Highlands</span> biogeographic area centers on two National Park Service units: Ozark National Scenic Riverways in Missouri and Buffalo National River in Arkansas. The Ozark <span class="hlt">Highlands</span> is part of a national network of 20 research sites established to determine the potential influence of global change on ecosystems and their adaptability. The Ozark <span class="hlt">Highlands</span> program will integrate historic and proxy stream flows, fluvial geomorphology, and trophic-level responses in streams to model aquatic systems under mid-continent, climate change scenarios. Climate change in Ozarks streams will likely alter hydrologic/geomorphic patterns and disrupt community structure and ecological processes. Initially, the program has focused on defining variation inherent in stream systems and how ecological processes and biota respond to that variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930016815','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930016815"><span id="translatedtitle"><span class="hlt">Cape</span> Photographic Durchmusterung, volume 3</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1993-01-01</p> <p>The <span class="hlt">Cape</span> Photographic Durchmusterung (CPD, Gill and Kapleyn 1895-1900) is a photographic survey of southern stars in the declination range -18 to -90 degrees. This volume covers the declination range -53 through -89 degrees. Positions are given for the 1875 equinox. The summary of the positional uncertainties quoted in the third volume of the published catalog gives +/- 0.28 sec (R.A.), + 0.044 arcmin (Dec.) for zones -18 to -57 degrees, + 0.157 sec + 0.0764/cos(delta) sec (R.A.), +/- 0.056 arcmin (Dec.) for zones -58 to -85 degrees, +0.157 sec + 0.0353/cos(delta) sec (R.A.), +/- 0.0127 arcmin (Dec.) for the polar plate where, as explained in the introduction to the third volume, many positions were derived from rectangular coordinates (these are positions reported to 0.1 sec (R.A.) and 0.001 arcmin (Dec.) in the -86 to -89 degree zones in the catalog). The probable error of a photographic magnitude, as determined by combining results for different magnitudes and weighting proportionately according to the numbers of stars in each class of magnitude, is given as +0.055 mag. From an analysis of the faint magnitude limits on the plates discussed in the third volume introduction, the catalog as a whole can be considered complete to photographic magnitude 9.2, but it is stated that it will be found practically complete, in or near the Milky Way, to magnitude 9.5.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930016814','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930016814"><span id="translatedtitle"><span class="hlt">Cape</span> Photographic Durchmusterung, volume 2</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1993-01-01</p> <p>The <span class="hlt">Cape</span> Photographic Durchmusterung (CPD, Gill and Kapteyn 1895-1900) is a Photographic survey of southern stars in the declination range -18 to -90 degrees. This volume covers the declination range -53 through -89 degrees. Positions are given for 1875 equinox. The summary of the positional uncertainties quoted in the third volume of the published catalog gives +/- 0.28 sec (R.A.), +/- 0.044 arcmin (Dec.) for zones - 18 to -57 degrees, + 0.157 sec + 0.0764/cos(delta) sec (R.A.), +/- 0.056 arcmin (Dec.) for zones -58 to -85 degrees, +0.157 sec + 0.0353/cos (delta) sec (R.A.), + 0.0127 arcmin (Dec.) for the polar plate where, as explained in the introduction to the third volume, many positions were derived from rectangular coordinates (these are positions reported to 0.1 SCC (R.A.) and 0.001 arcmin (Dec.) in the -86 to -89 degree zones in the catalog). The probable error of a photographic magnitude, as determined by combining results for different magnitudes and weighting proportionately according to the numbers of stars in each class of magnitude, is given as +0.055 mag. From an analysis of the faint magnitude limits on the plates discussed in the third volume introduction, the catalog as a whole can be considered complete to photographic magnitude 9.2, but it is stated that it will be found practically complete, in or near the Milky Way, to magnitude 9.5.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0714.photos.577773p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0714.photos.577773p/"><span id="translatedtitle">BOTTOM LEVEL OF ALTITUDE CHAMBER L, FACING SOUTHWEST <span class="hlt">Cape</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>BOTTOM LEVEL OF ALTITUDE CHAMBER L, FACING SOUTHWEST - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, Altitude Chambers, First Street, between Avenue D and Avenue E, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0710.photos.577705p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0710.photos.577705p/"><span id="translatedtitle">DETAIL VIEW OF COMPUTER PANELS, ROOM 8A <span class="hlt">Cape</span> Canaveral ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>DETAIL VIEW OF COMPUTER PANELS, ROOM 8A - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, Mobile Launcher Platforms, Launcher Road, East of Kennedy Parkway North, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384607p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384607p/"><span id="translatedtitle">44. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY BUILDING ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>44. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY - BUILDING ELEVATION WITH BUILDING METAL SIDING BEING APPLIED ON "B" FACE. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0762/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0762/"><span id="translatedtitle"><span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, The Solid ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p><span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, The Solid Rocket Booster Assembly and Refurbishment Facility Manufacturing Building, Southeast corner of Schwartz Road and Contractors Road, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0709.photos.577660p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0709.photos.577660p/"><span id="translatedtitle">VIEW OF THE JACKING, ELEVATING, AND LEVELING SKID. <span class="hlt">Cape</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>VIEW OF THE JACKING, ELEVATING, AND LEVELING SKID. - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 39, Crawler Transporters, Launcher Road, East of Kennedy Parkway North, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/1015422','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/1015422"><span id="translatedtitle">Porcess-industry <span class="hlt">CAPE</span>-OPEN software standard overview</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Zitney, S.</p> <p>2009-01-01</p> <p><span class="hlt">CAPE</span>-OPEN (<span class="hlt">CAPE</span> is short for Computer Aided Process Engineering) is a standard for writing computer software interfaces. It is mainly applied in process engineering where it enables a standardized communication between process simulators (e.g. Aspen Plus) and products developed by ourselves. The advantage of <span class="hlt">CAPE</span>-OPEN is that these products are applicable to more than just one process simulator; they are aimed at all process simulators that are <span class="hlt">CAPE</span>-OPEN compliant.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=primary+AND+resource&pg=6&id=EJ918643','ERIC'); return false;" href="http://eric.ed.gov/?q=primary+AND+resource&pg=6&id=EJ918643"><span id="translatedtitle">"Free Primary Education" in Lesotho and the Disadvantages of the <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Urwick, James</p> <p>2011-01-01</p> <p>This article explores the effects of national policies associated with "Education for All" on a disadvantaged region, the <span class="hlt">highlands</span> of Lesotho. Since 2000 a programme of "Free Primary Education" has improved the position of the <span class="hlt">highlands</span> in access to primary schooling; nevertheless, <span class="hlt">highland</span> primary schools compare poorly with those in the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577411p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577411p/"><span id="translatedtitle">Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air Force Station, Florida. Drawing 86K01547, Maurice H. Connell & Associates, February, 1961. OPERATIONS SUPPORT BUILDING SITE PLAN. Sheet 2 of 34 - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 34, Operations Support Building, Freedom Road, Southwest of Launch Stand CX-34, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577413p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577413p/"><span id="translatedtitle">Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air Force Station, Florida. Drawing 86K01547, Maurice H. Connell & Associates, February, 1961. OPERATIONS SUPPORT BUILDING ELEVATIONS AND SECTION. Sheet 5 of 34 - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 34, Operations Support Building, Freedom Road, Southwest of Launch Stand CX-34, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577414p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577414p/"><span id="translatedtitle">Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air Force Station, Florida. Drawing 86K01547, Maurice H. Connell & Associates, February, 1961. OPERATIONS SUPPORT BUILDING ROOF PLAN, REFLECTED CEILING PLAN, AND DETAILS. Sheet 7 of 34 - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 34, Operations Support Building, Freedom Road, Southwest of Launch Stand CX-34, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577412p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/fl0680.photos.577412p/"><span id="translatedtitle">Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>Photocopy of drawing. OPERATIONS SUPPORT BUILDING. NASA, <span class="hlt">Cape</span> Canaveral Air Force Station, Florida. Drawing 86K01547, Maurice H. Connell & Associates, February, 1961. OPERATIONS SUPPORT BUILDING FLOOR PLAN AND SCHEDULES. Sheet 4 of 34 - <span class="hlt">Cape</span> Canaveral Air Force Station, Launch Complex 34, Operations Support Building, Freedom Road, Southwest of Launch Stand CX-34, <span class="hlt">Cape</span> Canaveral, Brevard County, FL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec117-823.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec117-823.pdf"><span id="translatedtitle">33 CFR 117.823 - <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false <span class="hlt">Cape</span> Fear River. 117.823 Section... DRAWBRIDGE OPERATION REGULATIONS Specific Requirements North Carolina § 117.823 <span class="hlt">Cape</span> Fear River. The draw of the <span class="hlt">Cape</span> Fear Memorial Bridge, mile 26.8, at Wilmington need not open for the passage of vessels...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec117-822.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec117-822.pdf"><span id="translatedtitle">33 CFR 117.822 - <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false <span class="hlt">Cape</span> Fear River. 117.822 Section... DRAWBRIDGE OPERATION REGULATIONS Specific Requirements North Carolina § 117.822 <span class="hlt">Cape</span> Fear River. The draw of the <span class="hlt">Cape</span> Fear Memorial Bridge, mile 26.8, at Wilmington need not open for the passage of vessels...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec117-822.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec117-822.pdf"><span id="translatedtitle">33 CFR 117.822 - <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false <span class="hlt">Cape</span> Fear River. 117.822 Section... DRAWBRIDGE OPERATION REGULATIONS Specific Requirements North Carolina § 117.822 <span class="hlt">Cape</span> Fear River. The draw of the <span class="hlt">Cape</span> Fear Memorial Bridge, mile 26.8, at Wilmington need not open for the passage of vessels...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-823.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-823.pdf"><span id="translatedtitle">33 CFR 117.823 - <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> Fear River. 117.823 Section... DRAWBRIDGE OPERATION REGULATIONS Specific Requirements North Carolina § 117.823 <span class="hlt">Cape</span> Fear River. The draw of the <span class="hlt">Cape</span> Fear Memorial Bridge, mile 26.8, at Wilmington need not open for the passage of vessel from...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec117-822.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec117-822.pdf"><span id="translatedtitle">33 CFR 117.822 - <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false <span class="hlt">Cape</span> Fear River. 117.822 Section... DRAWBRIDGE OPERATION REGULATIONS Specific Requirements North Carolina § 117.822 <span class="hlt">Cape</span> Fear River. The draw of the <span class="hlt">Cape</span> Fear Memorial Bridge, mile 26.8, at Wilmington need not open for the passage of vessels...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=STS030-76-042&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3D5w','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=STS030-76-042&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3D5w"><span id="translatedtitle"><span class="hlt">Cape</span> Canaveral and Kennedy Space Center, Florida</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1989-01-01</p> <p>This single view of <span class="hlt">Cape</span> Canaveral and the Kennedy Space Center, Florida (28.5N, 80.5W), shows the layout of the entire Kennedy Space Center in minute detail. All of the early Mercury and Gemini series launch facilities can be seen at the hook of the <span class="hlt">Cape</span>. At the north end of the space center where the newer Apollo, Skylab and Space Shuttle series facilities are located, the vehicle assembly building, two launch pads and landing strip are easily seen.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.water.usgs.gov/sir2004-5294/','USGSPUBS'); return false;" href="http://pubs.water.usgs.gov/sir2004-5294/"><span id="translatedtitle">Hydrogeology of the Mogollon <span class="hlt">Highlands</span>, central Arizona</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Parker, John T.C.; Steinkampf, William C.; Flynn, Marilyn E.</p> <p>2005-01-01</p> <p>The Mogollon <span class="hlt">Highlands</span>, 4,855 square miles of rugged, mountainous terrain at the southern edge of the Colorado Plateau in central Arizona, is characterized by a bedrock-dominated hydrologic system that results in an incompletely integrated regional ground-water system, flashy streamflow, and various local water-bearing zones that are sensitive to drought. Increased demand on the water resources of the area as a result of recreational activities and population growth have made necessary an increased understanding of the hydrogeology of the region. The U.S. Geological Survey conducted a study of the geology and hydrology of the region in cooperation with the Arizona Department of Water Resources under the auspices of the Arizona Rural Watershed Initiative, a program launched in 1998 to assist rural areas in dealing with water-resources issues. The study involved the analysis of geologic maps, surface-water and ground-water flow, and water and rock chemical data and spatial relationships to characterize the hydrogeologic framework. The study area includes the southwestern corner of the Colorado Plateau and the Mogollon Rim, which is the eroded edge of the plateau. A 3,000- to 4,000-foot sequence of early to late Paleozoic sedimentary rocks forms the generally south-facing scarp of the Mogollon Rim. The area adjacent to the edge of the Mogollon Rim is an erosional landscape of rolling, step-like terrain exposing Proterozoic metamorphic and granitic rocks. Farther south, the Sierra Ancha and Mazatzal Mountain ranges, which are composed of various Proterozoic rocks, flank an alluvial basin filled with late Cenozoic sediments and volcanic flows. Eight streams with perennial to intermittent to ephemeral flow drain upland regions of the Mogollon Rim and flow into the Salt River on the southern boundary or the Verde River on the western boundary. Ground-water flow paths generally are controlled by large-scale fracture systems or by karst features in carbonate rocks. Stream</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005ECSS...65..319R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005ECSS...65..319R"><span id="translatedtitle">Macrofaunal distributions and habitat change following winter spring releases of freshwater into the <span class="hlt">Breton</span> Sound estuary, Louisiana (USA)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rozas, Lawrence P.; Minello, Thomas J.; Munuera-Fernández, Itzíar; Fry, Brian; Wissel, Björn</p> <p>2005-10-01</p> <p>We examined the effect of freshwater inflows on the aquatic environment and macrofauna in the intermediate and brackish zones of the <span class="hlt">Breton</span> Sound estuary. Following water releases from the Caernarvon Freshwater Diversion Structure in winter 2000 and spring 2001, we compared environmental conditions and the abundance and distribution of nekton in May 2001 between the inflow area, which receives freshwater directly from the structure, and a nearby reference area. We used these data and stable isotope analyses for C, N, and S in brown shrimp Farfantepenaeus aztecus and two species of grass shrimp ( Palaemonetes paludosus and Palaemonetes intermedius) to test four null hypotheses: (1) water quality and SAV (submerged aquatic vegetation) coverage were similar between the inflow and reference areas, (2) macrofaunal abundance and biomass were similar between the two areas, (3) stable isotopic values of brown shrimp and grass shrimp were similar between areas, habitat types, and species, and (4) brown shrimp distributions were unaffected by river inputs. Freshwater from the structure clearly influenced the estuarine environment within the inflow area. Releases from the Caernarvon structure freshened the inflow area as intended and increased SAV and daytime dissolved oxygen concentrations. The response by macrofauna to these increased freshwater flows and habitat changes involved mostly changes in density and biomass rather than shifts in species composition. Although we detected no strong effect of the freshwater diversion on brown shrimp abundance or size in the inflow area, results of the sulfur stable isotope analysis indicated that brown shrimp collected in the inflow area had been growing in higher salinity waters, possibly following downstream displacement by the diversion. Species that would benefit most from continued freshwater diversions are likely to be those species that both use SAV as nursery habitat and thrive in a low-salinity environment. Nutrients carried</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED112475.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED112475.pdf"><span id="translatedtitle">Educational Leadership by Objectives. <span class="hlt">Highland</span>, Indiana Superintendency Team Assessment Plan.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Highland Public Schools, IN.</p> <p></p> <p>This publication describes the <span class="hlt">Highland</span> Superintendency Team Assessment Program, an effort to apply the principles of management by objectives to the evaluation of school district administrative personnel. Section 1 presents the basic rationale and goals of the assessment program and explains the concept of "educational leadership by objectives"…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ739889.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ739889.pdf"><span id="translatedtitle">An Exploration of Myles Horton's Democratic Praxis: <span class="hlt">Highlander</span> Folk School</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Thayer-Bacon, Barbara J.</p> <p>2004-01-01</p> <p><span class="hlt">Highlander</span> Folk School is an adult education center located in eastern Tennessee that was formed in 1932 by Myles Horton and continues today. Myles Horton (1905-1990) hoped to create an independent adult learning center where people could come together and address their problems. He wanted to create a public space where people could learn from…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19730013041&hterms=orientale+basin&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dorientale%2Bbasin','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19730013041&hterms=orientale+basin&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dorientale%2Bbasin"><span id="translatedtitle">Descartes <span class="hlt">highlands</span>: Possible analogs around the Orientale Basin, part D</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Carroll, A. H.</p> <p>1972-01-01</p> <p>Two possible analogs, although not entirely satisfactory, offer reasonable alternatives to the volcanic interpretation of the Descartes <span class="hlt">highlands</span>. Reconsideration of this complex terrain, prompted by the preliminary results of the Apollo 16 mission, will lead to the revision of some theories on lunar volcanism and also to a better understanding of the landforms caused by the formation of multi-ring basins.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=326643','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=326643"><span id="translatedtitle">Virulence diversity of Uromyces Appendiculatus in the <span class="hlt">Highlands</span> of Guatemala</span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p>The common bean is planted throughout Guatemala, especially in the <span class="hlt">highlands</span> of the South East, North East, and South West regions. In these regions, temperatures fluctuate between 16 y 20 °C and the average rain precipitation is about 1000 mm. These conditions are optimum for the rust disease and b...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780032326&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528metamorphic%2Brock%2529','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780032326&hterms=metamorphic+rock&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3D%2528metamorphic%2Brock%2529"><span id="translatedtitle">On the age of KREEP. [in lunar <span class="hlt">highland</span> rocks</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Palme, H.</p> <p>1977-01-01</p> <p>It is noted that the variable Rb-Sr model ages of lunar <span class="hlt">highland</span> rocks containing a significant amount of KREEP basalt may be best explained by some fractionation of Rb from Sr during metamorphism 3.9 billion years ago, but the uniformity of the KREEP-type trace-element pattern in different <span class="hlt">highland</span> samples indicates that elements such as the rare earth were hardly fractionated at all during the metamorphic event. Data are presented which show that the Rb/Sr fractionation 3.9 billion years ago was due to Rb mobilization alone in most cases and that this fractionation can be accounted for by coupling of Rb to other, less volatile incompatible elements. Variations of Rb in lunar <span class="hlt">highland</span> rocks are analyzed, a correction method is applied for the Rb/Sr fractionation, and results are evaluated separately for Apollo 16 VHA and KREEP basalts, Apollo 17 noritic breccias, Apollo 14 KREEP breccias, Apollo 15 KREEP basalts, and Apollo 15-KREEP-enriched breccias. Evidence for volatilization of alkalis from glasses of impact origin is summarized, and an apparent correlation is discussed between meteoritic component (as given by the Ir/Au ratio) and rock type (as given by the U or Rb content) for many lunar <span class="hlt">highland</span> samples.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76694&keyword=logistic+AND+management&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=66596780&CFTOKEN=89888993','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76694&keyword=logistic+AND+management&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=66596780&CFTOKEN=89888993"><span id="translatedtitle">INTERACTIVE HABITAT MODELS FOR MID-ATLANTIC <span class="hlt">HIGHLAND</span> STREAM FISHES</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>In most wadeable streams of the Mid-Atlantic <span class="hlt">Highland</span> region of the eastern United States, habitat alteration resulting from development in the watershed is the primary stressor for fish. Models that predict the presence of stream fish species based on habitat characteristics ca...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title27-vol1/pdf/CFR-2010-title27-vol1-sec9-139.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title27-vol1/pdf/CFR-2010-title27-vol1-sec9-139.pdf"><span id="translatedtitle">27 CFR 9.139 - Santa Lucia <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... 1984) (7) Paraiso Springs, Calif., 1956 (photorevised 1984) (c) Boundaries. The Santa Lucia <span class="hlt">Highlands</span>... boundary follows Limekiln Creek for approximately 1.25 miles northeast to the 100 foot elevation. (2) Then... the junction of Foothill and Paraiso Roads on the Soledad, California U.S.G.S. map. (8) Then...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2305628','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2305628"><span id="translatedtitle">Malaria in the African <span class="hlt">highlands</span>: past, present and future.</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lindsay, S. W.; Martens, W. J.</p> <p>1998-01-01</p> <p>Many of the first European settlers in Africa sought refuge from the heat and diseases of the plains by moving to the cool and salubrious <span class="hlt">highlands</span>. Although many of the <span class="hlt">highlands</span> were originally malaria free, there has been a progressive rise in the incidence of the disease over the last 50 years, largely as a consequence of agroforestry development, and it has been exacerbated by scarce health resources. In these areas of fringe transmission where the malaria pattern is unstable, epidemics may be precipitated by relatively subtle climatic changes. Since there is little immunity against the disease in these communities, outbreaks can be devastating, resulting in a substantial increase in morbidity and death among both children and adults. We present here the results obtained using a mathematical model designed to identify these epidemic-prone regions in the African <span class="hlt">highlands</span> and the differences expected to occur as a result of projected global climate change. These <span class="hlt">highlands</span> should be recognized as an area of special concern. We further recommend that a regional modelling approach should be adopted to assess the extent and severity of this problem and help improve disease surveillance and the quality of health care delivered in this unstable ecosystem. Images Fig. 1 Fig. 4 Fig. 5 Fig. 6 PMID:9615495</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title27-vol1/pdf/CFR-2010-title27-vol1-sec9-122.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title27-vol1/pdf/CFR-2010-title27-vol1-sec9-122.pdf"><span id="translatedtitle">27 CFR 9.122 - Western Connecticut <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... <span class="hlt">Highlands</span>. 9.122 Section 9.122 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE... (Litchfield-Hartford-New Haven County line); (6) The boundary then travels approximately 7 miles west along the Litchfield-New Haven County line to Connecticut Route #8 at Waterville in the Town of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=AS07-05-1617&hterms=Studded&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3DStudded','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=AS07-05-1617&hterms=Studded&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3DStudded"><span id="translatedtitle"><span class="hlt">Highlands</span> of Tibet as seen from the Apollo 7 spacecraft</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1968-01-01</p> <p>The great lake-studded <span class="hlt">highlands</span> of Tibet, as seen from the Apollo 7 spacecraft during its 24th revolution of the earth. Photographed from an altitude of 124 nautical miles. The snow line in the picture is at 18,000 feet; and the lakes are at 15,000 feet above sea level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/27035346','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/27035346"><span id="translatedtitle">Neurological Impact of World War I on the Artistic Avant-Garde: The Examples of André <span class="hlt">Breton</span>, Guillaume Apollinaire and Blaise Cendrars.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bogousslavsky, Julien; Tatu, Laurent</p> <p>2016-01-01</p> <p>World War I erupted at a time when artistic avant-gardes were particularly thriving across Europe. Young poets, writers, painters and sculptors were called to arms or voluntary enrolled to fight, and several of them died during the conflict. Among others, it dramatically changed their creative output, either through specific wounds or through personal encounters and experiences. These individual events then significantly modified the course of the literary and artistic avant-garde movements. Three particularly illustrative examples of avant-garde French poets are presented here: André <span class="hlt">Breton</span> (1896-1966), Guillaume Apollinaire (1880-1918) and Blaise Cendrars (1887-1961). The deep source of the surrealist movement can indeed be found in André <span class="hlt">Breton</span>'s involvement as an auxiliary physician with critical interest in neuropsychiatry, which caused him to discover automatic writing. Guillaume Apollinaire's right temporal subdural hematoma strongly modified his emotional state and subsequent artistic activities. Alternatively, after losing his right, writing hand, Blaise Cendrars not only substituted it with a phantom but also rapidly switched from poetry to novels after he learnt to write with his left hand. PMID:27035346</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/ds/542/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/ds/542/"><span id="translatedtitle">Archive of Sediment Data Collected around the Chandeleur Islands and <span class="hlt">Breton</span> Island in 2007 and 1987 (Vibracore Surveys: 07SCC04, 07SCC05, and 87039)</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dreher, C.A.; Flocks, J.G.; Kulp, M.A.; Ferina, N.F.</p> <p>2010-01-01</p> <p>In 2006 and 2007, the U.S. Geological Survey (USGS) and collaborators at the University of New Orleans (UNO) collected high-resolution seismic profiles and subsurface cores around the Chandeleur and <span class="hlt">Breton</span> Islands, Louisiana (Study Area Map). To ground-truth the acoustic seismic surveys conducted in 2006, 124 vibracores were acquired during the 07SCC04 and 07SCC05 cruises in 2007. These cores were collected within the back-barrier, nearshore, and offshore environments. The surveys were conducted as part of a post-hurricane assessment and sediment resource inventory for the Barrier Island Coastal Monitoring (BICM) project. Vibracores were collected offshore using the USGS R/V G.K. Gilbert, while the terrestrial, back-barrier, and nearshore vibracores were collected from the UNO R/V Greenhead. This report serves as an archive of sediment data from two concurrent vibracore surveys (cruises 07SCC04 and 07SCC05) from around the <span class="hlt">Breton</span> and Chandeleur Islands in 2007 and also documents sediment data from vibracores collected offshore of the Chandeleur Islands in 1987 (cruise 87039). The 1987 vibracores were collected through the collaborated efforts of the USGS, Louisiana Geological Survey (LGS), and Alpine Ocean Seismic. Each vibracore can be identified by cruise and core number.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27035346','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27035346"><span id="translatedtitle">Neurological Impact of World War I on the Artistic Avant-Garde: The Examples of André <span class="hlt">Breton</span>, Guillaume Apollinaire and Blaise Cendrars.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bogousslavsky, Julien; Tatu, Laurent</p> <p>2016-01-01</p> <p>World War I erupted at a time when artistic avant-gardes were particularly thriving across Europe. Young poets, writers, painters and sculptors were called to arms or voluntary enrolled to fight, and several of them died during the conflict. Among others, it dramatically changed their creative output, either through specific wounds or through personal encounters and experiences. These individual events then significantly modified the course of the literary and artistic avant-garde movements. Three particularly illustrative examples of avant-garde French poets are presented here: André <span class="hlt">Breton</span> (1896-1966), Guillaume Apollinaire (1880-1918) and Blaise Cendrars (1887-1961). The deep source of the surrealist movement can indeed be found in André <span class="hlt">Breton</span>'s involvement as an auxiliary physician with critical interest in neuropsychiatry, which caused him to discover automatic writing. Guillaume Apollinaire's right temporal subdural hematoma strongly modified his emotional state and subsequent artistic activities. Alternatively, after losing his right, writing hand, Blaise Cendrars not only substituted it with a phantom but also rapidly switched from poetry to novels after he learnt to write with his left hand.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002PhDT........23R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002PhDT........23R"><span id="translatedtitle">A 'private adventure'? John Herschel's <span class="hlt">Cape</span> voyage and the production of the '<span class="hlt">Cape</span> Results'</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ruskin, Steven William</p> <p>2002-07-01</p> <p>This dissertation considers the life of John Herschel (1792 1871) from the years 1833 to 1847. In 1833 Herschel sailed from London to <span class="hlt">Cape</span> Town, southern Africa, to undertake (at his own expense) an astronomical exploration of the southern heavens, as well as a terrestrial exploration of the area around <span class="hlt">Cape</span> Town. After his return to England in 1838, he was highly esteemed and became Britain's most recognized scientist. In 1847 his southern hemisphere astronomical observations were published as the <span class="hlt">Cape</span> Results. The main argument of this dissertation is that Herschel's voyage, and the publication of the <span class="hlt">Cape</span> Results, in addition to their contemporary scientific importance, were also significant for nineteenth-century politics and culture. This dissertation is a two-part dissertation. The first part is entitled “John Herschel's <span class="hlt">Cape</span> Voyage: Private Science, Public Imagination, and the Ambitions of Empire”; and the second part, “The Production of the <span class="hlt">Cape</span> Results.” In the first part it is demonstrated that the reason for Herschel's cultural renown was the popular notion that his voyage to the <span class="hlt">Cape</span> was a project aligned with the imperial ambitions of the British government. By leaving England for one of its colonies, and pursuing there a significant scientific project, Herschel was seen in the same light as other British men of science who had also undertaken voyages of exploration and discovery. It is then demonstrated, in the second part of this work, that the production of the <span class="hlt">Cape</span> Results, in part because of Herschel's status as Britain's scientific figurehead, was a significant political and cultural event. In addition to the narrow area of Herschel scholarship, this dissertation touches on other areas of research in the history of science as well: science and culture, science and empire, science and politics, and what has been called the “new” history of scientific books.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140010695','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140010695"><span id="translatedtitle">GEO-<span class="hlt">CAPE</span> Aerosol Working Group Report</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Chin, Mian; Jethva, Hiren; Joiner, Joanna; Lyapustin, Alexei; Mattoo, Shana; Torres, Omar; Vasilkov, Alexander; Kondragunta, Shobha; Ciren, Pubu; Remer, Lorraine; Wang, Jun</p> <p>2013-01-01</p> <p>GEO-<span class="hlt">CAPE</span> will measure a suite of short-lived species that are relevant to both air quality and climate. The document was presented at the 2013 AEROCENTER Annual Meeting held at the GSFC Visitors Center, May 31, 2013. The Organizers of the meeting are posting the talks to the public Aerocentr website, after the meeting.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_9 --> <div id="page_10" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="181"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED167870.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED167870.pdf"><span id="translatedtitle">Red <span class="hlt">Capes</span>, Red Herrings, and Red Flags.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Fiske, Donald W.</p> <p></p> <p>The argument that the personality structures obtained from retrospective ratings reflect semantic similarity structures has been as provocative as a red <span class="hlt">cape</span> in the bull ring. High congruence between those two kinds of structures seems well established. What is less clear is how and why those structures differ from that for immediate judgments of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/wri/1980/0048/WRIR80-48.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/wri/1980/0048/WRIR80-48.pdf"><span id="translatedtitle">Distribution of nitrate in the unsaturated zone, <span class="hlt">Highland</span>-East <span class="hlt">Highlands</span> area, San Bernardino County, California</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Klein, John M.; Bradford, Wesley L.</p> <p>1980-01-01</p> <p>Nitrogen in the unsaturated soil zone in the <span class="hlt">Highland</span>-East <span class="hlt">Highlands</span> area of San Bernardino County, Calif., has been suspected as the source of nitrate in water from wells. Plans to recharge the local aquifers with imported surface water would raise the water table and intercept that nitrogen. This study was made to describe the distribution of inorganic nitrogen and other chemical constituents and nitrogen-using bacteria in the unsaturated zone, to relate nitrogen occurrences, in a general way, to present and historical land use, and to attempt to predict nitrogen concentrations in ground water after recharge. Some generalized correlations between nitrogen occurrence and land use were observed. In 11 of 13 test holes, the maximum nitrate-nitrogen (NO3--N) concentrations occurred within 10 feet of the surface, suggesting that the major source of nitrogen is from the surface at these sites. Test holes were ranked according to maximum NO3--N in the top 10 feet, total NO3--N in the top 10 feet, and total NO3--N in the top 40 feet. In all three rankings, the top seven test holes were the same--five in or near present or historical agricultural areas (primarily citrus groves), one in a feedlot, and one adjacent to an abandoned sewage-treatment plant. Two test holes in historically uninhabited areas ranked lowest. The control test hole in an uninhabited area ranked high in geometric mean of ammonium-nitrogen concentration (NH4+-N), suggesting that present in freshly weathered granite. The geometric means of NH4+-N concentrations in six of eight citrus-related test holes were significantly lower than in the control hole, suggesting that irrigation in citrus groves may have created conditions favoring nitrification of the primary NH4+-N. Rank correlation analyses between various measurements in test holes showed that high NO3--N concentrations tend to occur with high specific conductance and chloride concentrations in soil extracts. If recharge is carried out as planned</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.6831M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.6831M"><span id="translatedtitle">Late-Quaternary niche glaciation in the Lesotho <span class="hlt">highlands</span>, southern Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mills, Stephanie; Carr, Simon; Grab, Stefan; Rea, Brice</p> <p>2010-05-01</p> <p>Records of past climate data for southern Africa are predominantly restricted to arid, coastal or semi-arid environments (Karoo, Kalahari & Namib deserts, Western <span class="hlt">Cape</span>). There is currently no reliable temperature or rainfall proxy data for climate change prior to the present interglacial for Lesotho. Consequently, there has been continued debate over the issue of whether this region in southern Africa experienced increased or reduced precipitation at and around the global Last Glacial Maximum (LGM). Recent published work has applied a geomorphological, micromorphological and glaciological approach to demonstrate a glacial origin for various ‘moraine like' deposits in south-eastern Lesotho. This geomorphic evidence, dated to the LGM, implies that specific climatic conditions would have been required to sustain active glaciers. This paper presents results from two sites in the Lesotho <span class="hlt">highlands</span>, which host linear ridges interpreted as glacial moraines. The application of a glacier reconstruction technique to determine whether these sites could have supported glaciers permits the calculation of palaeoglacier mass balance, total velocity and basal slip, which in turn may be compared to modern analogues. Reconstructed equilibrium line altitudes (ELAs) range from 3071 to 3074 m a.s.l. and palaeotemperatures during the summer months would have been around 2.7°C, whilst palaeoprecipitation would have approximated 1500 mm per annum. The results indicate that the mass balance characteristics for the palaeoglaciers are comparable with modern analogues, reflecting viable, if marginal glaciation. The importance of topographic shading on determining the location of the glaciers is reflected through insolation mapping and the potential of this shading on glacier mass balance is quantified from energy balance model calculations. The occurrence of small-scale glaciation in the Drakensberg during the LGM implies that precipitation was greater than at present, despite the general</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014E%26ES...19a2009A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014E%26ES...19a2009A"><span id="translatedtitle">Willingness to pay for <span class="hlt">highlands</span>' agro-tourism recreational facility: A case of Boh Tea plantation, Cameron <span class="hlt">Highlands</span>, Malaysia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>A, Syamsul Herman M.; M, Nur A'in C.; S, Ahmad; S, Ramachandran</p> <p>2014-03-01</p> <p>The increase in tourist demand for <span class="hlt">highland</span> experience is inevitable. Cameron <span class="hlt">Highlands</span>, established as a Tea Plantation Estate during the British Colonial era in 1929, has evolved into a major <span class="hlt">highland</span> tourism destination providing a cool climatic experience coupled with scenic beauty in the midst of Tudor concept architecture which enhances the destinations historical value. Realising such tourism potential, the Boh Plantation management has provided a visitor centre as recreational facility for tourist utilisation. However, the absence in imposing an entrance fee has left a vacuum in determining the recreational economic value of this facility as the benefit of this agro-tourism product to tourists remains unknown. It would be important for the management to identify the benefit since the development and maintenance of the facility is costly. Hence, the purpose of this paper is to estimate the benefit of such establishment in <span class="hlt">highlands</span> area by assessing visitor's Willingness to pay (WTP). The study examines, explores and debates the issues in a critical yet supportive environment especially <span class="hlt">highlands</span>. The study obtained 179 usable questionnaires from visitors during weekends, weekdays and public holidays. The result showed that 59% of the visitors were willing to pay for the agro-tourism product. The WTP was estimated at RM 7.21 (1.81). Three factors were found to be influencing WTP which were monthly income, years of education and perception on scenery. Although the study was conducted post development, the finding indicated the WTP for current management practise. Should the management change its style, it would also affect WTP and also the total economic value. Since WTP is established concept, the finding of the study reflects on the opportunities, barriers and challenges inherent in embracing post-disciplinary approaches to research and suggest ways to further enhance the approach.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/ds/0860/ds860_title.html','USGSPUBS'); return false;" href="https://pubs.usgs.gov/ds/0860/ds860_title.html"><span id="translatedtitle">Baseline coastal oblique aerial photographs collected from Dauphin Island, Alabama, to <span class="hlt">Breton</span> Island, Louisiana, August 8, 2012</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Morgan, Karen L.M.; Westphal, Karen A.</p> <p>2014-01-01</p> <p>The U.S. Geological Survey (USGS) conducts baseline and storm response photography missions to document and understand the changes in vulnerability of the Nation's coasts to extreme storms. On August 8, 2012, the USGS conducted an oblique aerial photographic survey from Dauphin Island, Alabama, to <span class="hlt">Breton</span> Island, Louisiana, aboard a Cessna 172 at an altitude of 500 feet (ft) and approximately 1,000 ft offshore. This mission was flown to collect baseline data for assessing incremental changes since the last survey, and the data can be used in the assessment of future coastal change. The images provided here are Joint Photographic Experts Group (JPEG) images. Exiftool was used to add the following to the header of each photo: time of collection, Global Positioning System (GPS) latitude, GPS longitude, keywords, credit, artist (photographer), caption, copyright, and contact information. The photograph locations are an estimate of the position of the aircraft and do not indicate the location of any feature in the images (see the Navigation Data page). These photographs document the configuration of the barrier islands and other coastal features at the time of the survey. Pages containing thumbnail images of the photographs, referred to as contact sheets, were created in 5-minute segments of flight time. These segements can be found on the Photos and Maps page. Photographs can be opened directly with any JPEG-compatible image viewer by clicking on a thumbnail on the contact sheet. Table 1 provides detailed information about the GPS location, name, date, and time each of the 1241 photographs taken along with links to each photograph. The photography is organized into segments, also referred to as contact sheets, and represent approximately 5 minutes of flight time. (Also see the Photos and Maps page). In addition to the photographs, a Google Earth Keyhole Markup Language (KML) file is provided and can be used to view the images by clicking on the marker and then clicking</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/ds/0857/ds857_title.html','USGSPUBS'); return false;" href="https://pubs.usgs.gov/ds/0857/ds857_title.html"><span id="translatedtitle">Baseline coastal oblique aerial photographs collected from <span class="hlt">Breton</span> Island, Louisiana, to the Alabama-Florida border, July 13, 2013</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Morgan, Karen L.M.; Westphal, Karen A.</p> <p>2014-01-01</p> <p>The U.S. Geological Survey (USGS) conducts baseline and storm response photography missions to document and understand the changes in vulnerability of the Nation's coasts to extreme storms. On July 13, 2013, the USGS conducted an oblique aerial photographic survey from <span class="hlt">Breton</span> Island, Louisiana, to the Alabama-Florida border, aboard a Cessna 172 flying at an altitude of 500 feet (ft) and approximately 1,000 ft offshore. This mission was flown to collect baseline data for assessing incremental changes since the last survey, and the data can be used in the assessment of future coastal change. The images provided here are Joint Photographic Experts Group (JPEG) images. ExifTtool was used to add the following to the header of each photo: time of collection, Global Positioning System (GPS) latitude, GPS longitude, keywords, credit, artist (photographer), caption, copyright, and contact information. The photograph locations are an estimate of the position of the aircraft and do not indicate the location of any feature in the images (see the Navigation Data page). These photographs document the configuration of the barrier islands and other coastal features at the time of the survey. Pages containing thumbnail images of the photographs, referred to as contact sheets, were created in 5-minute segments of flight time. These segements can be found on the Photos and Maps page. Photographs can be opened directly with any JPEG-compatible image viewer by clicking on a thumbnail on the contact sheet. Table 1 provides detailed information about the GPS location, name, date, and time each of the 1242 photographs taken along with links to each photograph. The photography is organized into segments, also referred to as contact sheets, and represent approximately 5 minutes of flight time. (Also see the Photos and Maps page). In addition to the photographs, a Google Earth Keyhole Markup Language (KML) file is provided and can be used to view the images by clicking on the marker and then</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-07-30/pdf/2010-18718.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-07-30/pdf/2010-18718.pdf"><span id="translatedtitle">75 FR 44916 - Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-07-30</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC... of the <span class="hlt">Cape</span> Fear River Memorial Bridge, across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC. The... <span class="hlt">Cape</span> Fear River Memorial Bridge across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC has...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EOSTr..94R..21K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EOSTr..94R..21K"><span id="translatedtitle">The Evolution of the Lunar <span class="hlt">Highlands</span> Crust: A Complicated History</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Klima, Rachel</p> <p>2013-01-01</p> <p>More than 30 years after the first Lunar <span class="hlt">Highlands</span> Crust conference, lunar petrology and remote sensing experts from around the world gathered to discuss and debate the formation and evolution of the lunar <span class="hlt">highlands</span> crust. Huge strides in orbital remote sensing have enabled researchers to put the samples gathered during the Apollo missions into a larger, global context, yet many of the original, key questions remain. What was the extent and fate of the lunar magma ocean (LMO)? What is the nature of the lower lunar crust? Do lunar sample ages still suggest that the inner solar system was subject to an increase in impact flux around 3.9 billion years ago? At the heart of these questions is the desire to understand not only the formation and evolution of the Moon but of Earth, the terrestrial planets, and the inner solar system as a whole.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/21071665','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/21071665"><span id="translatedtitle">Structure and formation of the lunar farside <span class="hlt">highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Garrick-Bethell, Ian; Nimmo, Francis; Wieczorek, Mark A</p> <p>2010-11-12</p> <p>The formation of the lunar farside <span class="hlt">highlands</span> has long been an open problem in lunar science. We show that much of the topography and crustal thickness in this terrain can be described by a degree-2 harmonic. No other portion of the Moon exhibits comparable degree-2 structure. The quantified structure of the farside <span class="hlt">highlands</span> unites them with the nearside and suggests a relation between lunar crustal structure, nearside volcanism, and heat-producing elements. The farside topography cannot be explained by a frozen-in tidal bulge. However, the farside crustal thickness and the topography it produces may have been caused by spatial variations in tidal heating when the ancient crust was decoupled from the mantle by a liquid magma ocean, similar to Europa's present ice shell. PMID:21071665</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19750006613','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19750006613"><span id="translatedtitle">Lunar <span class="hlt">highland</span> rock types: Their implications for impact induced fractionation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Phinney, W. C.; Warner, J. L.; Simonds, C. H.</p> <p>1974-01-01</p> <p>The first step in a petrologic study must be a classification based on observed textures and mineralogy. Lunar rocks, may be classified into three major groups: (1) coarse-grained igneous rocks, (2) fine-grained igneous rocks and (3) breccias. Group 1 is interpreted as primitive lunar crustal rocks that display various degrees of crushing and/or annealing. Group 2 is interpreted as volcanic rocks. Group 3 is interpreted as resulting from impacts on the lunar surface and is subdivided on the basis of matrix textures into fragmental breccias, crystalline breccias that have been annealed, and crystalline breccias with igneous matrices. A synthesis of the relevant data concerning lunar <span class="hlt">highlands</span> polymict breccias from the fields of petrography, chemistry, photogeology, and impact studies compels the prediction that the breccias should have homogeneous matrices from rock to rock within regions of the <span class="hlt">highlands</span> of limited size where impact mixing has been efficient and extensive.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130011614','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130011614"><span id="translatedtitle">Mission Applications of a HIAD for the Mars Southern <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Winski, Richard; Bose, Dave; Komar, David R.; Samareh, Jamshid</p> <p>2013-01-01</p> <p>Recent discoveries of evidence of a flowing liquid in craters throughout the Mars Southern <span class="hlt">Highlands</span>, like Terra Sirenum, have spurred interest in sending science missions to those locations; however, these locations are at elevations that are much higher (0 to +4 km MOLA) than any previous landing site (-1 to -4 km MOLA). New technologies may be needed to achieve a landing at these sites with significant payload mass to the surface. A promising technology is the hypersonic inflatable aerodynamic decelerator (HIAD); a number of designs have been advanced but the stacked torus has been recently successfully flight tested in the IRVE-2 and IRVE-3 projects through the NASA Langley Research Center. This paper will focus on a variety of mission applications of the stacked torus type attached HIAD to the Mars southern <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992Metic..27R.295T&link_type=ABSTRACT','NASAADS'); return false;" href="http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992Metic..27R.295T&link_type=ABSTRACT"><span id="translatedtitle">The Lunar <span class="hlt">Highland</span> Crust: Complex or Simple Petrogenesis?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Taylor, S. R.; Koeberl, C.</p> <p>1992-07-01</p> <p>Following the general acceptance of the magma ocean hypothesis, models for the evolution of the <span class="hlt">highland</span> crust of the Moon have become increasingly complicated, just as religious and philosophical systems have always diverged from the teachings of their founder. Three components make up the <span class="hlt">highland</span> crust: the ferroan anorthosite, which crystallizes early from the magma ocean, depletes the deep interior in Eu, and adds a large Eu enrichment to the crust. KREEP, choked with incompatible trace elements from the residual 2% melt resulting from the crystallization of the magma ocean is pervasively mixed into the crust by cratering. KREEP adds a deep Eu depletion, with high abundances of the other REE parallel to those of the ferroan anorthosites. The third well-recognized component is the Mg Suite, commonly about 100-200 Ma younger, with intermediate REE patterns parallel to the ferroan anorthosites and KREEP (Fig. 1). If the <span class="hlt">highland</span> crust were formed from many igneous events, in which the Mg suite comes from several separate plutons, crystallization and separation of mineral phases would surely result in REE patterns with diverse slopes, as is observed on Earth. This does not seem to have occurred. For example, the deep-seated troctolite 76535 has a well-established age of 4236 +- 15 Ma (Premo and Tatsumoto, 1992), much younger than the 4440 +- 20 Ma crystallization age of the lunar crust (Carlson and Lugmair, 1988), and the 4400-Ma closure ages for the source regions of the lunar mare basalts. If 76535 formed as a separate intrusion by partial melting during "serial magmatism" 200 Ma after the ferroan anorthosites crystallized, why is its REE pattern parallel to those of all the other <span class="hlt">highland</span> rocks (Fig. 1)? Two explanations seem viable. The first possibility is that a diverse crust may have been homogenized by cratering. Alternatively, only one major igneous event produced the lunar <span class="hlt">highland</span> crust. All subsequent complexity in ages and production of "igneous</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2010/5097/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2010/5097/"><span id="translatedtitle">Hydrogeology and groundwater quality of <span class="hlt">Highlands</span> County, Florida</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Spechler, Rick M.</p> <p>2010-01-01</p> <p>Groundwater is the main source of water supply in <span class="hlt">Highlands</span> County, Florida. As the demand for water in the county increases, additional information about local groundwater resources is needed to manage and develop the water supply effectively. To address the need for additional data, a study was conducted to evaluate the hydrogeology and groundwater quality of <span class="hlt">Highlands</span> County. Total groundwater use in <span class="hlt">Highlands</span> County has increased steadily since 1965. Total groundwater withdrawals increased from about 37 million gallons per day in 1965 to about 107 million gallons per day in 2005. Much of this increase in water use is related to agricultural activities, especially citrus cultivation, which increased more than 300 percent from 1965 to 2005. <span class="hlt">Highlands</span> County is underlain by three principal hydrogeologic units. The uppermost water-bearing unit is the surficial aquifer, which is underlain by the intermediate aquifer system/intermediate confining unit. The lowermost hydrogeologic unit is the Floridan aquifer system, which consists of the Upper Floridan aquifer, as many as three middle confining units, and the Lower Floridan aquifer. The surficial aquifer consists primarily of fine-to-medium grained quartz sand with varying amounts of clay and silt. The aquifer system is unconfined and underlies the entire county. The thickness of the surficial aquifer is highly variable, ranging from less than 50 to more than 300 feet. Groundwater in the surficial aquifer is recharged primarily by precipitation, but also by septic tanks, irrigation from wells, seepage from lakes and streams, and the lateral groundwater inflow from adjacent areas. The intermediate aquifer system/intermediate confining unit acts as a confining layer (except where breached by sinkholes) that restricts the vertical movement of water between the surficial aquifer and the underlying Upper Floridan aquifer. The sediments have varying degrees of permeability and consist of permeable limestone, dolostone, or</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140007403','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140007403"><span id="translatedtitle">Cubesat Application for Planetary Entry Missions (<span class="hlt">CAPE</span>)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Esper, Jaime; Baumann, Jean-Pierre; Herdrich, Georg</p> <p>2013-01-01</p> <p>The Cubesat Application for Planetary Entry Missions (<span class="hlt">CAPE</span>) concept describes a high-performing Cubesat system which includes a propulsion module and miniaturized technologies capable of surviving atmospheric entry heating, while reliably transmitting scientific and engineering data. The Micro Return Capsule 2 (MIRKA2) is CAPE’s first planetary entry probe flight prototype. Within this context, this paper summarizes CAPE’s configuration and typical operational scenario. It also summarizes MIRKA2’s design and basic aerodynamic characteristics, and discusses potential challenges drawn from the experience of missions such as Stardust and MUSES-C. <span class="hlt">CAPE</span> not only opens the door to new planetary mission capabilities, it also offers relatively low-cost opportunities especially suitable to university participation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMPP51E1179S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMPP51E1179S"><span id="translatedtitle">The Effect of Local Topographic Unevenness on Contourite Paleo-Deposition Around Marine <span class="hlt">Capes</span>: A Novel "Geostrophic Cascade" in <span class="hlt">Cape</span> Suvero and <span class="hlt">Cape</span> Cilento (Tyrrhenian Sea)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Salusti, E.; Chiocci, F. L.; Martorelli, E.; Falcini, F.</p> <p>2014-12-01</p> <p>Despite the fact that two neighboring headlands in the Italian Southern Tyrrhenian Sea, <span class="hlt">Cape</span> Cilento and <span class="hlt">Cape</span> Suvero, have rather similar morphology and contouring flows, their contourite drifts were recognized, respectively, upstream the <span class="hlt">Cape</span> Cilento tip and downstream <span class="hlt">Cape</span> Suvero tip. Such an intriguing difference is discussed in terms of paleo-sedimentary processes induced by the interaction between large scale marine current turbulence and seafloor morphology around a <span class="hlt">cape</span> (Martorelli et al., 2010). However Martorelli's et al. model for contourite location - which allows only an upstream contourite location for this kind of <span class="hlt">capes</span> - fails in trying to explain such a difference. We thus focus on the local effect of a topographic depression, viz. a landslide scar off <span class="hlt">Cape</span> Suvero, on flows contouring a <span class="hlt">cape</span>. By applying the classical conservation of marine water potential vorticity we find a steady cyclonic circulation over the scar, that generates a "geostrophic cascade" that affects contourite deposition and stability. All this intuitively reminds the current dynamics around the Galileo's Red Spot in Jupiter's atmosphere. We thus show that the application of the potential vorticity conservation can provide a novel theoretical tool for investigating sedimentary structures and their evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1029973','PMC'); return false;" href="http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1029973"><span id="translatedtitle">Prevalence of asthma and wheeze in the <span class="hlt">Highlands</span> of Scotland.</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Austin, J B; Russell, G; Adam, M G; Mackintosh, D; Kelsey, S; Peck, D F</p> <p>1994-01-01</p> <p>To establish the prevalence of asthma and wheeze in 12 year old children in a region with low background pollution levels, a population of children resident in the <span class="hlt">Highland</span> Region of Scotland was studied by questionnaire supported by objective data. A respiratory questionnaire was distributed to the parents of 1919 children aged from 12-13 years and attending secondary schools in the educational divisions of Lochaber, Ross and Cromarty, and Inverness including Skye in <span class="hlt">Highland</span> Region to ascertain history of wheeze and parental awareness of a diagnosis of asthma. Peak expiratory flow (PEF) measurements were carried out before and after a standardised exercise test. Ozone levels were noted. Questionnaires were completed by 1825 parents (95% of those invited) and 1702 (93%) of those returning questionnaires took part in the exercise test. The overall prevalence of reported asthma was 14% and wheeze 25%. Defined as a fall in PEF of more than 15% with exercise, the overall prevalence of exercise induced bronchospasm was 9%. In Skye the prevalence of reported asthma was 17%, wheeze 28%, and exercise induced bronchospasm 30%. There were no significant differences between areas for reported asthma or wheeze. There was, however, a highly significant difference between areas for exercise induced bronchospasm, most of which was accounted for by the very high incidence in Skye, which is one of the most rural of the areas studied. The results of this study do not support the hypothesis that asthma is commoner in urban than rural areas, whether we compare the <span class="hlt">Highlands</span> with the rest of the UK or areas within the <span class="hlt">Highlands</span>, or whether we examine reported symptoms or exercise induced bronchospasm. The results do not support an association between atmospheric pollution and the prevalence of asthma. PMID:7979493</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19810041815&hterms=Ants&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3DAnts','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19810041815&hterms=Ants&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D90%26Ntt%3DAnts"><span id="translatedtitle">Genesis of <span class="hlt">highland</span> basalt breccias - A view from 66095</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Garrison, J. R., Jr.; Taylor, L. A.</p> <p>1980-01-01</p> <p>Electron microprobe and defocused beam analyses of the lunar <span class="hlt">highland</span> breccia sample 66095 show it consists of a fine-grained subophitic matrix containing a variety of mineral and lithic clasts, such as intergranular and cataclastic ANT, shocked and unshocked plagioclase, and basalts. Consideration of the chemistries of both matrix and clasts provides a basis for a qualitative three-component mixing model consisting of an ANT plutonic complex, a Fra Mauro basalt, and minor meteoric material.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/1275431','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/1275431"><span id="translatedtitle">Biological correlates of modernization in a Guatemalan <span class="hlt">highland</span> municipio.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Scholl, T O; Odell, M E</p> <p>1976-01-01</p> <p>The demographic correlates of modernization were studied in a municipio of the Guatemalan <span class="hlt">highlands</span> using, as indicators of modernization, the introduction of chemical fertilizers and of a religous revitalization movement. Accion Catolica. Records, taken from interviews, of 340 women divided into declines (decennial groups) within ten-year birth cohorts extending from before 1925 to 1954, were checked for representativeness against the birth registries for the entire municipio for the years 1965-69.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5707833','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5707833"><span id="translatedtitle">Mafic rocks of the Adirondack <span class="hlt">Highlands</span>: One suite or many</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Whitney, P.R. . New York State Museum)</p> <p>1993-03-01</p> <p>Mafic rocks in the granulite facies terrane of the Adirondack <span class="hlt">Highlands</span> form at least 3 and possibly as many as 6 groups, based on field, petrographic, and geochemical criteria. Most abundant is the olivine metagabbro-amphibolite group (OMA), equivalent to the mafic suite'' of Olson (J. Petrol. 33:471, 1992). OMA occurs in irregular to tabular bodies, locally with intrusive relations, in all major rock types in the E and central <span class="hlt">Highlands</span>. OMA is strongly olivine normative and forms a continuous differentiation series (Olson, 1992). Plagioclase-two pyroxene-garnet granulites (PGG) form dikes up to several m wide, in anorthositic host rocks. PGG are ferrogabbroic or ferrodioritic and approximately silica saturated. Two subgroups differ sharply in Mg, P, and trace elements. Ferrodiorite and monzodiorite gneisses (FMG), quartz normative and commonly migmatitic, occur in several large bodies in the NE <span class="hlt">Highlands</span> and as extensive thin sheets in the W and SE <span class="hlt">Highlands</span>, in association with anorthositic rocks. Three subgroups are distinguishable using Mg/Fe ratios and trace elements. Major element least-squares modeling suggests that both PGG and FMG could be derived by fractionation of gabbroic anorthosite liquids. A differentiation series is not evident, however, and both trace element (Ba, Rb, Sr, Zr and REE) data and normative plagioclase (An [>=] plag. in anorthosite) indicate a more complex origin. One subgroup of FMG may be early cumulates of the mangerite-charnockite suite. The chemistry of OMA, PGG, and FMG reflects their evolved nature and cannot be readily interpreted in terms of magma sources.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/1275431','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/1275431"><span id="translatedtitle">Biological correlates of modernization in a Guatemalan <span class="hlt">highland</span> municipio.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Scholl, T O; Odell, M E</p> <p>1976-01-01</p> <p>The demographic correlates of modernization were studied in a municipio of the Guatemalan <span class="hlt">highlands</span> using, as indicators of modernization, the introduction of chemical fertilizers and of a religous revitalization movement. Accion Catolica. Records, taken from interviews, of 340 women divided into declines (decennial groups) within ten-year birth cohorts extending from before 1925 to 1954, were checked for representativeness against the birth registries for the entire municipio for the years 1965-69. PMID:1275431</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/17255031','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/17255031"><span id="translatedtitle">Prehistoric human impact on rainforest biodiversity in <span class="hlt">highland</span> New Guinea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Haberle, Simon G</p> <p>2007-02-28</p> <p>In the <span class="hlt">highlands</span> of New Guinea, the development of agriculture as an indigenous innovation during the Early Holocene is considered to have resulted in rapid loss of forest cover, a decrease in forest biodiversity and increased land degradation over thousands of years. But how important is human activity in shaping the diversity of vegetation communities over millennial time-scales? An evaluation of the change in biodiversity of forest habitats through the Late Glacial transition to the present in five palaeoecological sites from <span class="hlt">highland</span> valleys, where intensive agriculture is practised today, is presented. A detailed analysis of the longest and most continuous record from Papua New Guinea is also presented using available biodiversity indices (palynological richness and biodiversity indicator taxa) as a means of identifying changes in diversity. The analysis shows that the collapse of key forest habitats in the <span class="hlt">highland</span> valleys is evident during the Mid - Late Holocene. These changes are best explained by the adoption of new land management practices and altered disturbance regimes associated with agricultural activity, though climate change may also play a role. The implications of these findings for ecosystem conservation and sustainability of agriculture in New Guinea are discussed. PMID:17255031</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26078279','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26078279"><span id="translatedtitle">Independent Molecular Basis of Convergent <span class="hlt">Highland</span> Adaptation in Maize.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Takuno, Shohei; Ralph, Peter; Swarts, Kelly; Elshire, Rob J; Glaubitz, Jeffrey C; Buckler, Edward S; Hufford, Matthew B; Ross-Ibarra, Jeffrey</p> <p>2015-08-01</p> <p>Convergent evolution is the independent evolution of similar traits in different species or lineages of the same species; this often is a result of adaptation to similar environments, a process referred to as convergent adaptation. We investigate here the molecular basis of convergent adaptation in maize to <span class="hlt">highland</span> climates in Mesoamerica and South America, using genome-wide SNP data. Taking advantage of archaeological data on the arrival of maize to the <span class="hlt">highlands</span>, we infer demographic models for both populations, identifying evidence of a strong bottleneck and rapid expansion in South America. We use these models to then identify loci showing an excess of differentiation as a means of identifying putative targets of natural selection and compare our results to expectations from recently developed theory on convergent adaptation. Consistent with predictions across a wide parameter space, we see limited evidence for convergent evolution at the nucleotide level in spite of strong similarities in overall phenotypes. Instead, we show that selection appears to have predominantly acted on standing genetic variation and that introgression from wild teosinte populations appears to have played a role in <span class="hlt">highland</span> adaptation in Mexican maize.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4571994','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4571994"><span id="translatedtitle">Independent Molecular Basis of Convergent <span class="hlt">Highland</span> Adaptation in Maize</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Takuno, Shohei; Ralph, Peter; Swarts, Kelly; Elshire, Rob J.; Glaubitz, Jeffrey C.; Buckler, Edward S.; Hufford, Matthew B.; Ross-Ibarra, Jeffrey</p> <p>2015-01-01</p> <p>Convergent evolution is the independent evolution of similar traits in different species or lineages of the same species; this often is a result of adaptation to similar environments, a process referred to as convergent adaptation. We investigate here the molecular basis of convergent adaptation in maize to <span class="hlt">highland</span> climates in Mesoamerica and South America, using genome-wide SNP data. Taking advantage of archaeological data on the arrival of maize to the <span class="hlt">highlands</span>, we infer demographic models for both populations, identifying evidence of a strong bottleneck and rapid expansion in South America. We use these models to then identify loci showing an excess of differentiation as a means of identifying putative targets of natural selection and compare our results to expectations from recently developed theory on convergent adaptation. Consistent with predictions across a wide parameter space, we see limited evidence for convergent evolution at the nucleotide level in spite of strong similarities in overall phenotypes. Instead, we show that selection appears to have predominantly acted on standing genetic variation and that introgression from wild teosinte populations appears to have played a role in <span class="hlt">highland</span> adaptation in Mexican maize. PMID:26078279</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920001563','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920001563"><span id="translatedtitle">Ancient fluvial processes in the equatorial <span class="hlt">highlands</span> of Mars</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Craddock, Robert A.; Maxwell, Ted A.</p> <p>1991-01-01</p> <p>Martian <span class="hlt">highland</span> craters typically lack ejecta deposits, have no noticeable rim, and are flat floored. In addition, crater size frequency distribution curves show that <span class="hlt">highland</span> craters have depleted populations less than 20 km in diameter. A variety of processes have been suggested to explain these observations including deposition of aeolian or volcanic materials up to the crater rim crests, thermal creep, terrain softening, and mass wasting. However, none of these processes adequately explains both the crater morphology and population distribution. In order to explain both the Martian <span class="hlt">highland</span> crater morphology and population distribution, a fluvial process is proposed which is capable of removing the loose crater rim material. The resulting effect is to decrease the crater diameter, thereby causing the population curves to bendover. The eroded material is redistributed, burying or partially burying smaller diameter craters before complete erosion. This material may also be deposited into local topographic lows, creating the depositional basins observed. A fluvial process explains both sets of observations: crater morphology and crater population distribution curves.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012icha.book...50G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012icha.book...50G"><span id="translatedtitle">The <span class="hlt">Cape</span> Observatory: all Categories of Heritage</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Glass, Ian S.</p> <p>2012-09-01</p> <p>In this presentation I will give an outline of the various types of heritage related to the Royal Observatory, <span class="hlt">Cape</span> of Good Hope, established in 1820 and now the headquarters campus of the South African Astronomical Observatory, located quite close to downtown <span class="hlt">Cape</span> Town. In terms of tangible, fixed heritage, the campus itself, the domes and the various other buildings are obviously relevant. This category includes the Classical Revival Main Building of 1828 and the McClean dome of 1895 by the leading colonial architect Herbert Baker as well as many other buildings and even the graves of two directors. Tangible movable items include, in principle, the telescopes, the accessory instruments and many pieces of apparatus that have been preserved. In addition, extensive collections of antique paintings, drawings, furniture and books add to the site's cultural significance. Many of the Observatory's archives are still kept locally. The intangible heritage of the Observatory consists for example of its history, its major discoveries, its interaction with the City, its central role in the history of science in South Africa and its appeal as a living cultural institution. Especially notable were the observations by Henderson (ca 1831) leading to the distance of a Cen and the early sky survey known as the <span class="hlt">Cape</span> Photographic Durchmusterung.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/7033824','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/7033824"><span id="translatedtitle">Seismic stratigraphy or <span class="hlt">Cape</span> Sorell Basin, Tasmania</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Bellow, T.L.</p> <p>1990-05-01</p> <p>Because large new exploration areas have become scarce, the <span class="hlt">Cape</span> Sorell basin has become an increasingly attractive frontier area. <span class="hlt">Cape</span> Sorell basin, located along the western passive continental margin of Tasmania formed as a result of the breakup of eastern Gondwanaland 95{plus minus}5 Ma. An extensional fault system trending west-northwest with dip-slip movement down to the south-southwest forms the northern boundary and a second fault system trending north-northwest with oblique slip down to the south-southwest creates the basin. Second order extensional faults within the basin have created wrench-type flower structures, which are potential migration pathways for hydrocarbons. Nine distinct depositional sequences identified within the <span class="hlt">Cape</span> Sorell basin record the evolution of this passive continental margin. Late Cretaceous-early Paleocene sequences were deposited as the rifting ceased and clastic progradation over the rift terrain began. Relative lowering of sea level occurred during the Paleocene, resulting in extensive channeling of the Late Cretaceous-early Paleocene sequences. A subsequent rise in relative sea level resulted in canyon-fill deposition during the early Paleocene to early Eocene. During the Eocene, sedimentation sufficiently increased to produce a downlapping sediment progradation characterized by deltaic depositional environment. Although interrupted several times by changes in relative sea level and shifting sediment sources, deltaic deposition continued until the late Oligocene. As the rate of clastic sedimentation slowed, carbonate shelf deposition began and has typified the basin since late the Oligocene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/wri7814','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/wri7814"><span id="translatedtitle">Distribution of dissolved nitrate and fluoride in ground water, <span class="hlt">Highland</span>-East <span class="hlt">Highlands</span>, San Bernardino County, California</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Eccles, Lawrence A.; Klein, John M.</p> <p>1978-01-01</p> <p>In the <span class="hlt">Highland</span>-East <span class="hlt">Highlands</span> area of southern California, concentrations of nitrate in water from many wells exceed the U.S. Environmental Protection Agency 's and the California Department of Health 's recommended limit for public water supplies. The nitrate standards for public water supplies in the study area are commonly met by blending the high-nitrate water with low-nitrate water before distribution; however, some of the low-nitrate water sources have fluoride concentrations that exceed the optimum level, or in a few cases exceed the maximum level recommended by the California Department of Health. Nitrate-nitrogen concentrations in the study area are generally between 1 and 20 milligrams per liter. In general, nitrate-nitrogen concentrations exceeding 10 milligrams per liter are found in water from wells perforated at depths of less than 500 feet. (Woodard-USGS)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.water.usgs.gov/wri824054','USGSPUBS'); return false;" href="http://pubs.water.usgs.gov/wri824054"><span id="translatedtitle">Preliminary delineation and description of the regional aquifers of Tennessee : the <span class="hlt">Highland</span> Rim aquifer system</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Brahana, J.V.; Bradley, M.W.</p> <p>1986-01-01</p> <p>The <span class="hlt">Highland</span> Rim aquifer system in Tennessee is primarily composed of Mississippian carbonates and occurs west of the Valley and Ridge Province. It crops out in the <span class="hlt">Highland</span> Rim and the Sequatchie Valley. It has been removed by erosion from the Central Basin. Groundwater in the <span class="hlt">Highland</span> Rim aquifer system occurs primarily in secondary openings including solution openings, joints, and faults. The Chattanooga Shale is the lower confining layer for the <span class="hlt">Highland</span> Rim aquifer system. Under the Cumberland plateau, this aquifer system is separated from the overlying Pennsylvanian formations by the Pennington Shale. The <span class="hlt">Highland</span> Rim aquifer system is an important source of drinking water. It supplies most of the rural, domestic, and many public supplies of drinking water in the <span class="hlt">Highland</span> Rim. Where there is a dynamic flow system, dissolved solids concentrations are less than 500 mg/L. However, isolated cells may exist where the groundwater has dissolved solids concentrations of more than 1 ,000 mg/L. (USGS)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2009/5252/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2009/5252/"><span id="translatedtitle">Sand Resources, Regional Geology, and Coastal Processes of the Chandeleur Islands Coastal System: an Evaluation of the <span class="hlt">Breton</span> National Wildlife Refuge</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lavoie, Dawn</p> <p>2009-01-01</p> <p><span class="hlt">Breton</span> National Wildlife Refuge, the Chandeleur Islands chain in Louisiana, provides habitat and nesting areas for wildlife and is an initial barrier protecting New Orleans from storms. The U.S. Geological Survey (USGS) in partnership with the University of New Orleans Pontchartrain Institute for Environmental Sciences undertook an intensive study that included (1) an analysis of island change based on historical maps and remotely sensed shoreline and topographic data; (2) a series of lidar surveys at 3- to 4-month intervals after Hurricane Katrina to determine barrier island recovery potential; (3) a discussion of sea level rise and effects on the islands; (4) an analysis of sea floor evolution and sediment dynamics in the refuge over the past 150 years; (5) an assessment of the local sediment transport and sediment resource availability based on the bathymetric and subbottom data; (6) a carefully selected core collection effort to groundtruth the geophysical data and more fully characterize the sediments composing the islands and surrounds; (7) an additional survey of the St. Bernard Shoals to assess their potential as a sand resource; and (8) a modeling study to numerically simulate the potential response of the islands to the low-intensity, intermediate, and extreme events likely to affect the refuge over the next 50 years. Results indicate that the islands have become fragmented and greatly diminished in subaerial extent over time: the southern islands retreating landward as they reorganize into subaerial features, the northern islands remaining in place. <span class="hlt">Breton</span> Island, because maintenance of the Mississippi River-Gulf Outlet (MRGO) outer bar channel requires dredging, is deprived of sand sufficient to sustain itself. Regional sediment transport trends indicate that large storms are extremely effective in transporting sand and controlling the shoreline development and barrier island geometry. Sand is transported north and south from a divergent zone near</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=lighthouse&pg=3&id=ED214792','ERIC'); return false;" href="http://eric.ed.gov/?q=lighthouse&pg=3&id=ED214792"><span id="translatedtitle"><span class="hlt">Cape</span> Hatteras Lighthouse, Project <span class="hlt">CAPE</span> Teaching Module, Publication 3-4a.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Temple, Bonnie K.</p> <p></p> <p>Twelve interdisciplinary lessons with supplementary materials for grades three and four comprise this teaching guide about the <span class="hlt">Cape</span> Hatteras Lighthouse. An introduction explains how the lighthouse is threatened by erosion, alternatives for saving it, the need for the lighthouse, and its history. Each lesson includes subject area, skills, lesson…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=MEG&pg=3&id=EJ685197','ERIC'); return false;" href="http://eric.ed.gov/?q=MEG&pg=3&id=EJ685197"><span id="translatedtitle"><span class="hlt">Cape</span> of Storms or <span class="hlt">Cape</span> of Good Hope? Educational Technology in a Changing Environment</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Czerniewicz, Laura</p> <p>2004-01-01</p> <p>This article locates and describes the work of the Multimedia Education Group (MEG) at the University of <span class="hlt">Cape</span> Town (UCT). This work is contextualised by three national and international challenges, these being (1) the need to increase access to new technologies and overcome the digital divide, (2) the need to respond to a new communication order,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1981STIN...8310640L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1981STIN...8310640L"><span id="translatedtitle">Geothermal community heating for <span class="hlt">Cape</span> Charles, Virginia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Leffel, C. S., Jr.</p> <p>1981-10-01</p> <p>An economic feasibility study for a geothermal community heating system was made for the residential heat load of <span class="hlt">Cape</span> Charles, Virginia using a computer program. The effects of inflation, interest rates, wellhead temperatures, and the addition of reinjection wells are investigated. It is concluded that the utilization of geothermal energy would be feasible if well flows of 500 gal/minute could be obtained and if reinjection of the geothermal fluids were not required. A comparison of the geothermal assisted community system with a coal fired system shows that the coal fired system may be the most attractive alternative to the heating of homes with individual oil fired furnaces.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-589.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-589.pdf"><span id="translatedtitle">33 CFR 117.589 - <span class="hlt">Cape</span> Cod Canal.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> Cod Canal. 117.589 Section 117.589 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY BRIDGES DRAWBRIDGE OPERATION REGULATIONS Specific Requirements Massachusetts § 117.589 <span class="hlt">Cape</span> Cod Canal. The draw...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384610p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384610p/"><span id="translatedtitle">47. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY AERIAL VIEW ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>47. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY AERIAL VIEW OF "A" FACE (LEFT) WITH CLEANING SYSTEM INSTALLED (NOW REMOVED) AND "B" FACE (RIGHT) WITH CONSTRUCTION CRANE IN USE. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384609p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384609p/"><span id="translatedtitle">46. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY BUILDING ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>46. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY - BUILDING ELEVATION VIEW WITH ALL METAL SIDING INSTALLED AND WITH EMITTER/ANTENNA ARRAY SYSTEM NEARING OCMPLETION ON "B" FACE (RIGHT). VIEW ALSO SHOWS TRAVELING "CLEANING" SYSTEM ON "B" FACE - NOW REMOVED. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title36-vol1/pdf/CFR-2010-title36-vol1-sec7-67.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title36-vol1/pdf/CFR-2010-title36-vol1-sec7-67.pdf"><span id="translatedtitle">36 CFR 7.67 - <span class="hlt">Cape</span> Cod National Seashore.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... SPECIAL REGULATIONS, AREAS OF THE NATIONAL PARK SYSTEM § 7.67 <span class="hlt">Cape</span> Cod National Seashore. (a) Off-road operation of motor vehicles. (1) What do I need to do to operate a vehicle off road? To operate a vehicle off road at <span class="hlt">Cape</span> Cod National Seashore, you must meet the requirements in paragraphs (b) through...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1633.photos.384563p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1633.photos.384563p/"><span id="translatedtitle">17. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY AERIAL VIEW ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>17. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY AERIAL VIEW WITH PROJECT NEARING COMPLETION. VIEW SHOWS "A" FACE (LEFT) AND "B" FACE OF RADAR ARRAY SYSTEM. NOTE THAT NORTH IS GENERALLY TO RIGHT OF VIEW. - <span class="hlt">Cape</span> Cod Air Station, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384608p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384608p/"><span id="translatedtitle">45. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY BUILDING ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>45. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY - BUILDING ELEVATION VIEW WITH BUILDING METAL SIDING BEING APPLIED ON "A" FACE (LEFT) AND "B" FACE (RIGHT). NOTE THAT NORTH IS GENERALLY TO RIGHT OF VIEW. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384605p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384605p/"><span id="translatedtitle">42. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY SHOWING ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>42. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY - SHOWING BUILDING "RED IRON" STEEL STRUCTURE AT 46T DAY OF STEEL CONSTRUCTION. "BUILDING TOPPED OFF, 7 JULY, 1974. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384606p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/ma1634.photos.384606p/"><span id="translatedtitle">43. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY WITH ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>43. <span class="hlt">CAPE</span> COD AIR STATION PAVE PAWS FACILITY - WITH BUILDING METAL SIDING BEING APPLIED ON "C" FACE (RIGHT) AND "B" FACE BEING PREPARED FOR INSTALLATION. - <span class="hlt">Cape</span> Cod Air Station, Technical Facility-Scanner Building & Power Plant, Massachusetts Military Reservation, Sandwich, Barnstable County, MA</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=garbage&pg=5&id=EJ563289','ERIC'); return false;" href="http://eric.ed.gov/?q=garbage&pg=5&id=EJ563289"><span id="translatedtitle"><span class="hlt">Cape</span> of Good Hope: Teacher Description and Project Plan.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Moyo, Kimya</p> <p>1998-01-01</p> <p>Presents detailed information about the <span class="hlt">Cape</span> of Good Hope project in which pairs of students designed <span class="hlt">capes</span> and cloaks out of the garbage bags for a fashion show. Also describes student objectives, unit goals, group activities, products required, and the final show and presentation. (ASK)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-829.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec117-829.pdf"><span id="translatedtitle">33 CFR 117.829 - Northeast <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Northeast <span class="hlt">Cape</span> Fear River. 117... Fear River. (a) The draw of the Isabel S. Holmes Bridge, at mile 1.0, at Wilmington, North Carolina... across the <span class="hlt">Cape</span> Fear River. (2) The draw shall be left in the open position to vessels and will only...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec117-829.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec117-829.pdf"><span id="translatedtitle">33 CFR 117.829 - Northeast <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Northeast <span class="hlt">Cape</span> Fear River. 117... Fear River. (a) The draw of the Isabel S. Holmes Bridge, at mile 1.0, at Wilmington, North Carolina... at the Navassa Railroad Bridge mile 34.0 across the <span class="hlt">Cape</span> Fear River. (2) The draw shall be left...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec117-829.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec117-829.pdf"><span id="translatedtitle">33 CFR 117.829 - Northeast <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false Northeast <span class="hlt">Cape</span> Fear River. 117... Fear River. (a) The draw of the Isabel S. Holmes Bridge, at mile 1.0, at Wilmington, North Carolina... at the Navassa Railroad Bridge mile 34.0 across the <span class="hlt">Cape</span> Fear River. (2) The draw shall be left...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5170603','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5170603"><span id="translatedtitle">Bedrock geology of the <span class="hlt">Cape</span> Ann Area, Massachusetts. Technical report</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Not Available</p> <p>1981-09-01</p> <p><span class="hlt">Cape</span> Ann on the Massachusetts eastern shore is dominated by igneous rocks, intruded into an igneous and metamorphic complex all cut by numerous faults. Geophysical investigations include total intensity aeromagnetic and gravity and magnetic studies. This report addresses structural features, stratigraphy, economic and environmental geology at the bedrock geology of the <span class="hlt">Cape</span> Ann area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED164408','ERIC'); return false;" href="http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED164408"><span id="translatedtitle"><span class="hlt">Cape</span> Verdeans in America: Our Story. A Teachers Manual.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Almeida, Raymond A.; And Others</p> <p></p> <p>Teaching strategies are suggested to help high school social studies teachers develop and implement a study of <span class="hlt">Cape</span> Verdean American history. Intended as a guide to accompany "<span class="hlt">Cape</span> Verdeans in America," (SO 011 060), the teacher's manual offers three categories of teaching methods: (1) ideas to help students read and understand the book, (2)…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15..171K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15..171K"><span id="translatedtitle">Soil erosion and land degradation in the <span class="hlt">Highlands</span> of Jordan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khresat, Saeb</p> <p>2013-04-01</p> <p>The <span class="hlt">Highlands</span> of Jordan has a Mediterranean type of climate characterized by hot dry summers and cold wet winters. Unsustainable land use practices, recurrent droughts and climate change are the main causes of land degradation in the <span class="hlt">Highlands</span> area of Jordan. Unsustainable land use practices include improper plowing, inappropriate rotations, inadequate or inexistent management of plant residues, overgrazing of natural vegetation, forest cutting, land fragmentation and over-pumping of groundwater. In addition, Jordan's rapid population growth (2.8% per year) is exerting considerable pressure upon its limited arable land through uncontrolled and random urbanization activities. Water erosion is the most widespread Land degradation type in the country. It greatly increases on slopes where the vegetation cover is (seasonally) reduced. It is further aggravated by a loss of soil structure and reduced infiltration rates. Wind erosion occurs most frequently in the arid and semi-arid portions of the southern <span class="hlt">Highlands</span>, especially in areas with sandy or loamy soils. Rangeland degradation is the second most widespread land degradation type that is driven by overgrazing. The impact of overgrazing on the vegetation is evident from the excessive uprooting of the green matter (grass and bushes), leading to reduced seeding, reduced regeneration, and the consequent loss of plant cover which make the soil more susceptible to water and wind erosion. It is estimated that about 41 percent of Jordan's total land area is characterized as degraded of which 22 percent of the total land mass is classified as moderately degraded and agricultural productivity is greatly reduced. Observed aspects of land degradation include the recession of forest areas, high rate of erosion by water (formation of rills and gullies), expansion of urbanized area, reduction in soil organic matter and soil structure deterioration. Implementation of soil erosion control measures such as contour cultivation</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27569548','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27569548"><span id="translatedtitle">Ancestral Origins and Genetic History of Tibetan <span class="hlt">Highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lu, Dongsheng; Lou, Haiyi; Yuan, Kai; Wang, Xiaoji; Wang, Yuchen; Zhang, Chao; Lu, Yan; Yang, Xiong; Deng, Lian; Zhou, Ying; Feng, Qidi; Hu, Ya; Ding, Qiliang; Yang, Yajun; Li, Shilin; Jin, Li; Guan, Yaqun; Su, Bing; Kang, Longli; Xu, Shuhua</p> <p>2016-09-01</p> <p>The origin of Tibetans remains one of the most contentious puzzles in history, anthropology, and genetics. Analyses of deeply sequenced (30×-60×) genomes of 38 Tibetan <span class="hlt">highlanders</span> and 39 Han Chinese lowlanders, together with available data on archaic and modern humans, allow us to comprehensively characterize the ancestral makeup of Tibetans and uncover their origins. Non-modern human sequences compose ∼6% of the Tibetan gene pool and form unique haplotypes in some genomic regions, where Denisovan-like, Neanderthal-like, ancient-Siberian-like, and unknown ancestries are entangled and elevated. The shared ancestry of Tibetan-enriched sequences dates back to ∼62,000-38,000 years ago, predating the Last Glacial Maximum (LGM) and representing early colonization of the plateau. Nonetheless, most of the Tibetan gene pool is of modern human origin and diverged from that of Han Chinese ∼15,000 to ∼9,000 years ago, which can be largely attributed to post-LGM arrivals. Analysis of ∼200 contemporary populations showed that Tibetans share ancestry with populations from East Asia (∼82%), Central Asia and Siberia (∼11%), South Asia (∼6%), and western Eurasia and Oceania (∼1%). Our results support that Tibetans arose from a mixture of multiple ancestral gene pools but that their origins are much more complicated and ancient than previously suspected. We provide compelling evidence of the co-existence of Paleolithic and Neolithic ancestries in the Tibetan gene pool, indicating a genetic continuity between pre-historical <span class="hlt">highland</span>-foragers and present-day Tibetans. In particular, highly differentiated sequences harbored in <span class="hlt">highlanders</span>' genomes were most likely inherited from pre-LGM settlers of multiple ancestral origins (SUNDer) and maintained in high frequency by natural selection.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/27569548','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/27569548"><span id="translatedtitle">Ancestral Origins and Genetic History of Tibetan <span class="hlt">Highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lu, Dongsheng; Lou, Haiyi; Yuan, Kai; Wang, Xiaoji; Wang, Yuchen; Zhang, Chao; Lu, Yan; Yang, Xiong; Deng, Lian; Zhou, Ying; Feng, Qidi; Hu, Ya; Ding, Qiliang; Yang, Yajun; Li, Shilin; Jin, Li; Guan, Yaqun; Su, Bing; Kang, Longli; Xu, Shuhua</p> <p>2016-09-01</p> <p>The origin of Tibetans remains one of the most contentious puzzles in history, anthropology, and genetics. Analyses of deeply sequenced (30×-60×) genomes of 38 Tibetan <span class="hlt">highlanders</span> and 39 Han Chinese lowlanders, together with available data on archaic and modern humans, allow us to comprehensively characterize the ancestral makeup of Tibetans and uncover their origins. Non-modern human sequences compose ∼6% of the Tibetan gene pool and form unique haplotypes in some genomic regions, where Denisovan-like, Neanderthal-like, ancient-Siberian-like, and unknown ancestries are entangled and elevated. The shared ancestry of Tibetan-enriched sequences dates back to ∼62,000-38,000 years ago, predating the Last Glacial Maximum (LGM) and representing early colonization of the plateau. Nonetheless, most of the Tibetan gene pool is of modern human origin and diverged from that of Han Chinese ∼15,000 to ∼9,000 years ago, which can be largely attributed to post-LGM arrivals. Analysis of ∼200 contemporary populations showed that Tibetans share ancestry with populations from East Asia (∼82%), Central Asia and Siberia (∼11%), South Asia (∼6%), and western Eurasia and Oceania (∼1%). Our results support that Tibetans arose from a mixture of multiple ancestral gene pools but that their origins are much more complicated and ancient than previously suspected. We provide compelling evidence of the co-existence of Paleolithic and Neolithic ancestries in the Tibetan gene pool, indicating a genetic continuity between pre-historical <span class="hlt">highland</span>-foragers and present-day Tibetans. In particular, highly differentiated sequences harbored in <span class="hlt">highlanders</span>' genomes were most likely inherited from pre-LGM settlers of multiple ancestral origins (SUNDer) and maintained in high frequency by natural selection. PMID:27569548</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/4067671','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/4067671"><span id="translatedtitle">Utilization of urea nitrogen in Papua New Guinea <span class="hlt">highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rikimaru, T; Fujita, Y; Okuda, T; Kajiwara, N; Date, C; Heywood, P F; Alpers, M P; Koishi, H</p> <p>1985-06-01</p> <p>The utilization of urea nitrogen was examined in 10 healthy adult men from a village near Lufa, in the Eastern <span class="hlt">Highlands</span> Province of Papua New Guinea. The staple diet of these men was sweet potatoes. [15N]urea was used as tracer for urea released into their intestinal tracts and the utilization of the urea-N was estimated from the trend of 15N. The men were orally given [15N]urea at the beginning of the study and then their daily protein intake, serum protein levels, 15N excretion in the feces and urine, 15N retention in the whole body and 15N incorporation into serum protein were examined. Their daily protein intake (32.2 +/- 8.6 g/day) was low, but their serum protein level (8.05 +/- 0.41 g/100 ml) was within the normal range. 15N retention in the whole body on day 3 was estimated to be 35.4 +/- 20.2% of the total amount administered, calculated from the recoveries in the feces (1.64 +/- 0.85%) and urine (63.0 +/- 20.5%) on days 1-3. The utilization of urea nitrogen in Papua New Guinea <span class="hlt">highlanders</span> was confirmed from the finding of 15N incorporation into serum proteins on day 3 (0.008 +/- 0.005 atom% excess). This incorporation was negatively correlated with the urinary nitrogen excretion and serum protein level. This correlation suggests that Papua New Guinea <span class="hlt">highlanders</span> with low urinary nitrogen excretion or a low level in serum protein, who are in a poor state of protein nutrition, tend to utilize more urea nitrogen for the synthesis of serum protein.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19950034777&hterms=emissivity&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Demissivity','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19950034777&hterms=emissivity&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Demissivity"><span id="translatedtitle">A ferroelectric model for the low emissivity <span class="hlt">highlands</span> on Venus</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Shepard, Michael K.; Arvidson, Raymond E.; Brackett, Robert A.; Fegley, Bruce, Jr.</p> <p>1994-01-01</p> <p>A model to explain the low emissivity venusian <span class="hlt">highlands</span> is proposed utilizing the temperature-dependent dielectric constant of ferroelectric minerals. Ferroelectric minerals are known to occur in alkaline and carbonite rocks, both of which are plausible for Venus. Ferroelectric minerals possess extremely high dielectric constants (10(exp 5)) over small temperature intervals and are only required in minor (much less than 1%) abundances to explain the observed emissivities. The ferroelectric model can account for: (1) the observed reduction in emissivity with increased altitude, (2) the abrupt return to normal emissivities at highest elevations, and (3) the variations in the critical elevation observed from region to region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/26624312','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/26624312"><span id="translatedtitle">A new species of Parakari (Ephemeroptera: Baetidae) from Guiana <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Derka, Tomáš; Nieto, Carolina; Svitok, Marek</p> <p>2015-01-01</p> <p>The genus Parakari was described from Guiana <span class="hlt">Highlands</span> in southeastern Venezuela by Nieto & Derka in 2011 for two species inhabiting streams draining isolated, flat-topped table mountains called tepuis. A description of a third representative, Parakari roraimensis sp. n., is given here based on material collected from a coldwater stream at the foothills of Roraima-tepui (SE Venezuela). Detailed morphological descriptions of mature nymph and female adult are given. A differential diagnosis and a key to nymphs of the three Parakari species are provided. PMID:26624312</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26624312','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26624312"><span id="translatedtitle">A new species of Parakari (Ephemeroptera: Baetidae) from Guiana <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Derka, Tomáš; Nieto, Carolina; Svitok, Marek</p> <p>2015-10-08</p> <p>The genus Parakari was described from Guiana <span class="hlt">Highlands</span> in southeastern Venezuela by Nieto & Derka in 2011 for two species inhabiting streams draining isolated, flat-topped table mountains called tepuis. A description of a third representative, Parakari roraimensis sp. n., is given here based on material collected from a coldwater stream at the foothills of Roraima-tepui (SE Venezuela). Detailed morphological descriptions of mature nymph and female adult are given. A differential diagnosis and a key to nymphs of the three Parakari species are provided.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=151624&keyword=activities+AND+libraries&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=64948460&CFTOKEN=53050965','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=151624&keyword=activities+AND+libraries&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=64948460&CFTOKEN=53050965"><span id="translatedtitle">WATERSHED RESTORATION AND FISHERIES MANAGEMENT IN THE MID-ATLANTIC <span class="hlt">HIGHLANDS</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>This presentation is about watershed restoration and fisheries management in the Mid-Atlantic <span class="hlt">Highlands</span>. The goal of the Canaan Valley Institue is to develop and implement solutions to restore damaged areas and protect aquatic systems in the Mid-Atlantic <span class="hlt">Highlands</span>. A decision ana...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED362910.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED362910.pdf"><span id="translatedtitle">Ethos in Action: Public Relations at the <span class="hlt">Highlander</span> Folk School, 1955-1956.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Durham, Frank</p> <p></p> <p>An examination of Rosa Parks' relationship with the <span class="hlt">Highlander</span> Folk School from the first encounter in 1955 through Labor Day of 1956 provides a new understanding of the school's public relations program that sought to end segregation in the Jim Crow South. Myles Horton founded <span class="hlt">Highlander</span> in 1932 to provide an adult residential center in the South…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-03/pdf/2010-10093.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-03/pdf/2010-10093.pdf"><span id="translatedtitle">75 FR 23221 - <span class="hlt">Highlands</span> Regional Study: Connecticut and Pennsylvania 2010 Update</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-03</p> <p>..., USDA. ACTION: Notice of public meetings; request for comment. SUMMARY: As required by the <span class="hlt">Highlands</span> Conservation Act, Public Law 108- 421, the Forest Service has drafted the <span class="hlt">Highlands</span> Regional Study: Connecticut... conservation value areas, the impacts of land use change on the natural resources, and conservation...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED560029.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED560029.pdf"><span id="translatedtitle">A New Turnaround Model: Michigan's <span class="hlt">Highland</span> Park Goes Charter. Policy Brief</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Spalding, Audrey</p> <p>2013-01-01</p> <p>This brief examines the series of events that led to the <span class="hlt">Highland</span> Park school district being converted to a system of charter public schools in 2012. Used as a strategy to help the district eliminate its large fiscal debt while still providing resident students with a local public school option, <span class="hlt">Highland</span> Park's charter conversion is one of the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol3/pdf/CFR-2010-title33-vol3-sec334-595.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol3/pdf/CFR-2010-title33-vol3-sec334-595.pdf"><span id="translatedtitle">33 CFR 334.595 - Atlantic Ocean off <span class="hlt">Cape</span> Canaveral; 45th Space Wing, <span class="hlt">Cape</span> Canaveral Air Force Station, FL...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... navigable waters of the United States, as defined at 33 CFR part 329, contiguous to the area offshore of... 33 Navigation and Navigable Waters 3 2010-07-01 2010-07-01 false Atlantic Ocean off <span class="hlt">Cape</span> Canaveral... AND RESTRICTED AREA REGULATIONS § 334.595 Atlantic Ocean off <span class="hlt">Cape</span> Canaveral; 45th Space Wing,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol3/pdf/CFR-2014-title33-vol3-sec334-595.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol3/pdf/CFR-2014-title33-vol3-sec334-595.pdf"><span id="translatedtitle">33 CFR 334.595 - Atlantic Ocean off <span class="hlt">Cape</span> Canaveral; 45th Space Wing, <span class="hlt">Cape</span> Canaveral Air Force Station, FL...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... navigable waters of the United States, as defined at 33 CFR part 329, contiguous to the area offshore of... 33 Navigation and Navigable Waters 3 2014-07-01 2014-07-01 false Atlantic Ocean off <span class="hlt">Cape</span> Canaveral... AND RESTRICTED AREA REGULATIONS § 334.595 Atlantic Ocean off <span class="hlt">Cape</span> Canaveral; 45th Space Wing,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1813089T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1813089T"><span id="translatedtitle"><span class="hlt">Cape</span> Fear: an outdoor hillslope laboratory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tauro, Flavia; Petroselli, Andrea; Fiori, Aldo; Romano, Nunzio; Rulli, Maria Cristina; Porfiri, Maurizio; Palladino, Mario; Grimaldi, Salvatore</p> <p>2016-04-01</p> <p>Hydrological processes occurring at the hillslope scale highly influence the response of natural catchments. However, modelling hillslope dynamics is often extremely challenging, and conceptualizations may be inadequate to simulate such complex processes. Towards this aim, field experiments on natural and artificial catchments have proved highly beneficial. In this work, we present <span class="hlt">Cape</span> Fear, an ad hoc designed experimental plot whereby traditional and new measurement systems are integrated for improved comprehension of hillslope processes. This outdoor hillslope laboratory hosts diverse sensing apparatuses, spanning from a system of rainfall simulators, a v-notch weir for input and output fluxes analysis, sophisticated instrumentation for continuous measurements of surface and subsurface water and soil transport, to innovative image-based setups to remotely sense surface waters. We demonstrate the potential of such a versatile and thoroughly instrumented outdoor laboratory through a proof-of-concept experiment conducted during a natural rainfall event. The response of the plot to the storm is reconstructed based on continuous monitoring of input and output fluxes. Further, an innovative tracer-based approach involving the use of fluorescent particles is utilized to remotely investigate the onset of overland flow from captured images. Insight from experimental observations is utilized to identify the physical phenomena governing the response of the hillslope to the precipitation event. <span class="hlt">Cape</span> Fear is a powerful resource for the hydrological community and this small scale experimental observatory is expected to provide diverse and innovative observations to advance current knowledge on hydrological processes at the hillslope scale.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006QuRes..66..454D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006QuRes..66..454D"><span id="translatedtitle">Holocene paleoclimates of southern Arabia from lacustrine deposits of the Dhamar <span class="hlt">highlands</span>, Yemen</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Davies, Caroline Pickens</p> <p>2006-11-01</p> <p>This paper presents new evidence from the Dhamar <span class="hlt">highlands</span>, Yemen, of paleohydrologic response to fluctuations in Holocene climate. Stratigraphic, geochemical, and chronological analyses of <span class="hlt">highland</span> peat and lacustrine deposits contribute to knowledge of the timing of early Holocene moisture changes on the Arabian Peninsula, providing a backdrop to understanding early cultural development in the Arabian <span class="hlt">highlands</span>. The location of the Dhamar <span class="hlt">highlands</span>, characterized by intermontane valleys surrounded by the highest mountains on the Arabian Peninsula and adjacent to the Indian Ocean is ideal for examining the influence of the Indian Ocean Monsoon (IOM) on the moisture history of this region. Fluctuations in the lacustrine and paleosol records of the Dhamar <span class="hlt">highlands</span> reflect both local changes in paleohydrology and regional influences on the Holocene paleoclimatic conditions in southwest Arabia. In addition, a peat deposit with a radiocarbon age of 10,253 - 10,560 cal yr BP documents some of the earliest Holocene high moisture conditions on the Arabian Peninsula.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/journal/1974/vol2issue1/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/journal/1974/vol2issue1/report.pdf"><span id="translatedtitle">Lunar <span class="hlt">highlands</span> volcanism implications from Luna 20 and Apollo 16</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wilshire, H.G.; Wilhelms, D.E.; Howard, K.A.</p> <p>1974-01-01</p> <p><span class="hlt">Highlands</span> materials sampled at the Apollo 16 and Luna 20 sites represent units of distinctive morphology that are widespread on the lunar nearside. Samples from the Apollo 16 site represent hilly and furrowed materials of the Descartes <span class="hlt">highlands</span> and Cayley Formation. Materials were collected by Luna 20 from terrain resembling the Descartes terrain. Most photogeologic interpretations of these units favored volcanic origins, but the samples fail to support this interpretation. Luna 20 soil fragments are mainly glassy microbreccia with lithic inclusions of fine-grained hornfels; less than 3 percent of the fragments have textures of volcanic rocks, and most of these are likely crystalline products of impact melting. Apollo 16 soils formed on ejecta derived from a plutonic anorthosite-norite-troctolite suite. The similarity of Luna 20 soils indicates that these too formed as regolith on ejecta of anorthosite-norite-troctolitc composition. Interpretation of the samples from the two locations now suggests that hilly and furrowed terrains, previously thought to be of volcanic origin, are impact ejecta; in view of the plutonic nature of the source rocks and their extensive fusion and metamorphism, it is likely that the ejecta were derived from multiring basins. At one point, the Apollo 16 site, the Cayley Formation is composed of basin ejecta.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19810041811&hterms=Gabbro&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DGabbro','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19810041811&hterms=Gabbro&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3DGabbro"><span id="translatedtitle">Lunar <span class="hlt">highland</span> melt rocks - Chemistry, petrology and silicate mineralogy</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Vaniman, D. T.; Papike, J. J.</p> <p>1980-01-01</p> <p>A selected suite containing several of the largest samples of lunar <span class="hlt">highland</span> melt rocks includes impact melt specimens (anorthositic gabbro, low-K Fra Mauro) and volcanic specimens (intermediate-K Fra Mauro). Although previous assumptions of LKFM volcanism have fallen into disfavor, no fatal arguments against this hypothesis have been presented, and the evidence of a possibly 'inherited igneous' olivine-plagioclase cosaturation provides cause for keeping a volcanic LKFM hypothesis viable. Comparisons of silicate mineralogy with melt rock compositions provide information on the specimen's composition and cooling history. Plagioclase-rock compositions can be matched to the experimentally determined equilibria for appropriate samples to identify melt rocks with refractory anorthitic clasts. Olivine-rock compositions indicate that melt rock vitrophyres precipitate anomalously Fe-rich olivine; the cause of this anomaly is not immediately evident. The Al-Ti and Ca-Fe-Mg zonation in pyroxene provide information on relative cooling rates of <span class="hlt">highland</span> melt rocks, but Cr- and Al-content (where Al-rich low-Ca pyroxene cores are preserved in rapidly cooled samples) can be correlated with composition of the host rock.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70176658','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70176658"><span id="translatedtitle">‘<span class="hlt">Cape</span> capture’: Geologic data and modeling results suggest the Holocene loss of a Carolina <span class="hlt">Cape</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Thieler, E. Robert; Ashton, Andrew D.</p> <p>2011-01-01</p> <p>For more than a century, the origin and evolution of the set of cuspate forelands known as the Carolina Capes—Hatteras, Lookout, Fear, and Romain—off the eastern coast of the United States have been discussed and debated. The consensus conceptual model is not only that these <span class="hlt">capes</span> existed through much or all of the Holocene transgression, but also that their number has not changed. Here we describe bathymetric, lithologic, seismic, and chronologic data that suggest another <span class="hlt">cape</span> may have existed between <span class="hlt">Capes</span> Hatteras and Lookout during the early to middle Holocene. This <span class="hlt">cape</span> likely formed at the distal end of the Neuse-Tar-Pamlico fluvial system during the early Holocene transgression, when this portion of the shelf was flooded ca. 9 cal (calibrated) kyr B.P., and was probably abandoned by ca. 4 cal kyr B.P., when the shoreline attained its present general configuration. Previously proposed mechanisms for <span class="hlt">cape</span> formation suggest that the large-scale, rhythmic pattern of the Carolina <span class="hlt">Capes</span> arose from a hydrodynamic template or the preexisting geologic framework. Numerical modeling, however, suggests that the number and spacing of <span class="hlt">capes</span> can be dynamic, and that a coast can self-organize in response to a high-angle-wave instability in shoreline shape. In shoreline evolution model simulations, smaller cuspate forelands are subsumed by larger neighbors over millennial time scales through a process of ‘<span class="hlt">cape</span> capture.’ The suggested former <span class="hlt">cape</span> in Raleigh Bay represents the first interpreted geological evidence of dynamic abandonment suggested by the self-organization hypothesis. <span class="hlt">Cape</span> capture may be a widespread process in coastal environments with large-scale rhythmic shoreline features; its preservation in the sedimentary record will vary according to geologic setting, physical processes, and sea-level history.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26844017','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26844017"><span id="translatedtitle">Non-native species in the vascular flora of <span class="hlt">highlands</span> and mountains of Iceland.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wasowicz, Pawel</p> <p>2016-01-01</p> <p>The <span class="hlt">highlands</span> and mountains of Iceland are one of the largest remaining wilderness areas in Europe. This study aimed to provide comprehensive and up-to-date data on non-native plant species in these areas and to answer the following questions: (1) How many non-native vascular plant species inhabit <span class="hlt">highland</span> and mountainous environments in Iceland? (2) Do temporal trends in the immigration of alien species to Iceland differ between <span class="hlt">highland</span> and lowland areas? (3) Does the incidence of alien species in the disturbed and undisturbed areas within Icelandic <span class="hlt">highlands</span> differ? (4) Does the spread of non-native species in Iceland proceed from lowlands to <span class="hlt">highlands</span>? and (5) Can we detect hot-spots in the distribution of non-native taxa within the <span class="hlt">highlands</span>? Overall, 16 non-native vascular plant species were detected, including 11 casuals and 5 naturalized taxa (1 invasive). Results showed that temporal trends in alien species immigration to <span class="hlt">highland</span> and lowland areas are similar, but it is clear that the process of colonization of <span class="hlt">highland</span> areas is still in its initial phase. Non-native plants tended to occur close to man-made infrastructure and buildings including huts, shelters, roads etc. Analysis of spatio-temporal patterns showed that the spread within <span class="hlt">highland</span> areas is a second step in non-native plant colonization in Iceland. Several statically significant hot spots of alien plant occurrences were identified using the Getis-Ord Gi* statistic and these were linked to human disturbance. This research suggests that human-mediated dispersal is the main driving force increasing the risk of invasion in Iceland's <span class="hlt">highlands</span> and mountain areas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/26844017','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/26844017"><span id="translatedtitle">Non-native species in the vascular flora of <span class="hlt">highlands</span> and mountains of Iceland.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wasowicz, Pawel</p> <p>2016-01-01</p> <p>The <span class="hlt">highlands</span> and mountains of Iceland are one of the largest remaining wilderness areas in Europe. This study aimed to provide comprehensive and up-to-date data on non-native plant species in these areas and to answer the following questions: (1) How many non-native vascular plant species inhabit <span class="hlt">highland</span> and mountainous environments in Iceland? (2) Do temporal trends in the immigration of alien species to Iceland differ between <span class="hlt">highland</span> and lowland areas? (3) Does the incidence of alien species in the disturbed and undisturbed areas within Icelandic <span class="hlt">highlands</span> differ? (4) Does the spread of non-native species in Iceland proceed from lowlands to <span class="hlt">highlands</span>? and (5) Can we detect hot-spots in the distribution of non-native taxa within the <span class="hlt">highlands</span>? Overall, 16 non-native vascular plant species were detected, including 11 casuals and 5 naturalized taxa (1 invasive). Results showed that temporal trends in alien species immigration to <span class="hlt">highland</span> and lowland areas are similar, but it is clear that the process of colonization of <span class="hlt">highland</span> areas is still in its initial phase. Non-native plants tended to occur close to man-made infrastructure and buildings including huts, shelters, roads etc. Analysis of spatio-temporal patterns showed that the spread within <span class="hlt">highland</span> areas is a second step in non-native plant colonization in Iceland. Several statically significant hot spots of alien plant occurrences were identified using the Getis-Ord Gi* statistic and these were linked to human disturbance. This research suggests that human-mediated dispersal is the main driving force increasing the risk of invasion in Iceland's <span class="hlt">highlands</span> and mountain areas. PMID:26844017</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4736984','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4736984"><span id="translatedtitle">Non-native species in the vascular flora of <span class="hlt">highlands</span> and mountains of Iceland</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2016-01-01</p> <p>The <span class="hlt">highlands</span> and mountains of Iceland are one of the largest remaining wilderness areas in Europe. This study aimed to provide comprehensive and up-to-date data on non-native plant species in these areas and to answer the following questions: (1) How many non-native vascular plant species inhabit <span class="hlt">highland</span> and mountainous environments in Iceland? (2) Do temporal trends in the immigration of alien species to Iceland differ between <span class="hlt">highland</span> and lowland areas? (3) Does the incidence of alien species in the disturbed and undisturbed areas within Icelandic <span class="hlt">highlands</span> differ? (4) Does the spread of non-native species in Iceland proceed from lowlands to <span class="hlt">highlands</span>? and (5) Can we detect hot-spots in the distribution of non-native taxa within the <span class="hlt">highlands</span>? Overall, 16 non-native vascular plant species were detected, including 11 casuals and 5 naturalized taxa (1 invasive). Results showed that temporal trends in alien species immigration to <span class="hlt">highland</span> and lowland areas are similar, but it is clear that the process of colonization of <span class="hlt">highland</span> areas is still in its initial phase. Non-native plants tended to occur close to man-made infrastructure and buildings including huts, shelters, roads etc. Analysis of spatio-temporal patterns showed that the spread within <span class="hlt">highland</span> areas is a second step in non-native plant colonization in Iceland. Several statically significant hot spots of alien plant occurrences were identified using the Getis-Ord Gi* statistic and these were linked to human disturbance. This research suggests that human-mediated dispersal is the main driving force increasing the risk of invasion in Iceland’s <span class="hlt">highlands</span> and mountain areas. PMID:26844017</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/9410249','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/9410249"><span id="translatedtitle">[The reconquest of the Madagascar <span class="hlt">highlands</span> by malaria].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mouchet, J; Laventure, S; Blanchy, S; Fioramonti, R; Rakotonjanabelo, A; Rabarison, P; Sircoulon, J; Roux, J</p> <p>1997-01-01</p> <p>A strong malaria epidemic with a high mortality rate occurred on the Madagascar <span class="hlt">Highlands</span> in 1986-88. Vector control and free access to antimalaria drugs controlled the disease. The authors have searched for the causes of the epidemic to propose a strategy avoiding such events. The <span class="hlt">Highlands</span> on Madagascar were known as malaria free. In 1878 a very severe epidemic flooded all the country. Development of irrigated ricefields which house both An. arabiensis and An. funestus had created a new anthropic environment. Moreover manpower imported from malarious coastal areas for rice cultivation and also for building large temples, could have brought P. falciparum. After several outbreaks the disease became endemic up to 1949. In 1949 a malaria eradication programme based on DDT spraying and drug chemoprophylaxis and chemotherapy was launched. By 1960 malaria was eliminated and DDT spraying cancelled. Only 3 foci were kept under surveillance with irregular spraying until 1975. The prophylaxis and treatment centres ("centres de nivaquinisation") were kept open up to 1979. The catholic dispensary of Analaroa, 100 km N.E. of Tananarive, opened in 1971 and worked without interruption up to now. The malaria diagnosis has always been controlled by microscopy. Its registers are probably the more reliable source of information on malaria in the area. They show that malaria was already present on the <span class="hlt">Highlands</span> in 1971 but at a low prevalence; in 1980 when the "centres de nivaquinisation" were closed the number of cases increased by three times the progressive increase of the number of cases became exponential from 1986 to 1988 which was the peak of the epidemic; malaria remained at a high level until the end of 1993; yearly DDT spraying since 1993 have decreased the number of malaria cases among the dispensary attendants by 90%. The epidemic peak of 1988 was well documented by the Pasteur Institute of Madagascar around Tananarive. Before the epidemic started it was observed a come</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-08-27/pdf/2012-20977.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-08-27/pdf/2012-20977.pdf"><span id="translatedtitle">77 FR 51699 - Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-08-27</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC... operation of the <span class="hlt">Cape</span> Fear River Memorial Bridge, at mile 26.8, over <span class="hlt">Cape</span> Fear River, at Wilmington, NC. The... a.m. on the first or second Sunday of November every year. The <span class="hlt">Cape</span> Fear River Memorial Bridge,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-03-01/pdf/2012-4918.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-03-01/pdf/2012-4918.pdf"><span id="translatedtitle">77 FR 12475 - Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-03-01</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River, Wilmington, NC... operation of the <span class="hlt">Cape</span> Fear Memorial Bridge, across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC. The..., the bridge opens on signal as required by 33 CFR 117.5. The <span class="hlt">Cape</span> Fear Memorial Bridge across the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-02-11/pdf/2013-02962.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-02-11/pdf/2013-02962.pdf"><span id="translatedtitle">78 FR 9587 - Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-02-11</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC... <span class="hlt">Cape</span> Fear River Memorial Bridge, across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC. The... second Sunday of November every year. The <span class="hlt">Cape</span> Fear River Memorial Bridge, at mile 26.8, at...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-08-26/pdf/2011-21869.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-08-26/pdf/2011-21869.pdf"><span id="translatedtitle">76 FR 53342 - Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-08-26</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulations; <span class="hlt">Cape</span> Fear River, Wilmington, NC... operation of the <span class="hlt">Cape</span> Fear Memorial Bridge, at mile 26.8, over <span class="hlt">Cape</span> Fear River, at Wilmington, NC. The... structure. The <span class="hlt">Cape</span> Fear Memorial Bridge, at mile 26.8, at Wilmington NC has vertical clearances in the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-03-04/pdf/2011-4854.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-03-04/pdf/2011-4854.pdf"><span id="translatedtitle">76 FR 11960 - Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-03-04</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulation; <span class="hlt">Cape</span> Fear River, Wilmington, NC... of the <span class="hlt">Cape</span> Fear River Memorial Bridge, across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC. The... Fear River Memorial Bridge across the <span class="hlt">Cape</span> Fear River, mile 26.8, at Wilmington, NC has...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17340187','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17340187"><span id="translatedtitle">HIV/AIDS and immigrant <span class="hlt">Cape</span> Verdean women: contextualized perspectives of <span class="hlt">Cape</span> Verdean community advocates.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>De Jesus, Maria</p> <p>2007-03-01</p> <p>This research explored <span class="hlt">Cape</span> Verdean community advocates' understandings of the structural and social realities that contribute to the increased HIV/AIDS risk of Northeastern U.S.-based immigrant <span class="hlt">Cape</span> Verdean women. A community perspective informed the analysis of the multi-layered contextual barriers that these advocates identified as limiting the effectiveness of individual-level HIV/AIDS prevention and intervention models. Qualitative content analysis of interviews with nine community advocates revealed several thematic clusters including challenges to (1) perceived institutional and community realities; (2) traditional gender relations; and, (3) traditional ways of thinking. These findings challenge universalist cognitive-behavioral change models of HIV/AIDS prevention and intervention and are critically discussed to better understand the complex realities faced by <span class="hlt">Cape</span> Verdean immigrant women. A liberatory community psychology perspective framed the research process and contributed to reconceptualizing HIV/AIDS risk as a community problem that requires interventions not simply at the individual and relational levels, but also at the structural level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09079&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09079&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> Verde' from '<span class="hlt">Cape</span> St. Mary' in Mid-Afternoon (False Color)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> Verde' from the vantage point of '<span class="hlt">Cape</span> St. Mary,' the next promontory clockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> Verde combines several exposures taken by the rover's panoramic camera into an approximately false-color mosaic. The exposures were taken during mid-afternoon lighting conditions. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. <p/> The images combined into this mosaic were taken during the 1,006th Martian day, or sol, of Opportunity's Mars-surface mission (Nov. 22, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters. The false color enhances subtle color differences among materials in the rocks and soils of the scene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09086&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09086&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> Verde' from '<span class="hlt">Cape</span> St. Mary' in Late Morning (False Color)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> Verde' from the vantage point of '<span class="hlt">Cape</span> St. Mary,' the next promontory clockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> Verde combines several exposures taken by the rover's panoramic camera into a false-color mosaic. The exposures were taken during late-morning lighting conditions. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. <p/> The images combined into this mosaic were taken during the 1,006th Martian day, or sol, of Opportunity's Mars-surface mission (Nov. 22, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters. The false color enhances subtle color differences among materials in the rocks and soils of the scene.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09078&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09078&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> Verde' from '<span class="hlt">Cape</span> St. Mary' in Mid-Afternoon</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> Verde' from the vantage point of '<span class="hlt">Cape</span> St. Mary,' the next promontory clockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> Verde combines several exposures taken by the rover's panoramic camera into an approximately true-color mosaic. The exposures were taken during mid-afternoon lighting conditions. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. <p/> The images combined into this mosaic were taken during the 1,006th Martian day, or sol, of Opportunity's Mars-surface mission (Nov. 22, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA09080&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA09080&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde"><span id="translatedtitle">View of '<span class="hlt">Cape</span> Verde' from '<span class="hlt">Cape</span> St. Mary' in Late Morning</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> As part of its investigation of 'Victoria Crater,' NASA's Mars Exploration Rover Opportunity examined a promontory called '<span class="hlt">Cape</span> Verde' from the vantage point of '<span class="hlt">Cape</span> St. Mary,' the next promontory clockwise around the crater's deeply scalloped rim. This view of <span class="hlt">Cape</span> Verde combines several exposures taken by the rover's panoramic camera into an approximately true-color mosaic. The exposures were taken during late-morning lighting conditions. <p/> The upper portion of the crater wall contains a jumble of material tossed outward by the impact that excavated the crater. This vertical cross-section through the blanket of ejected material surrounding the crater was exposed by erosion that expanded the crater outward from its original diameter, according to scientists' interpretation of the observations. Below the jumbled material in the upper part of the wall are layers that survive relatively intact from before the crater-causing impact. <p/> The images combined into this mosaic were taken during the 1,006th Martian day, or sol, of Opportunity's Mars-surface mission (Nov. 22, 2006). The panoramic camera took them through the camera's 750-nanometer, 530-nanometer and 430-nanometer filters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA08809&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA08809&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3DCape%2BVerde"><span id="translatedtitle">Layers of '<span class="hlt">Cape</span> Verde' in 'Victoria Crater'</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2006-01-01</p> <p><p/> This view of Victoria crater is looking north from 'Duck Bay' towards the dramatic promontory called '<span class="hlt">Cape</span> Verde.' The dramatic cliff of layered rocks is about 50 meters (about 165 feet) away from the rover and is about 6 meters (about 20 feet) tall. The taller promontory beyond that is about 100 meters (about 325 feet) away, and the vista beyond that extends away for more than 400 meters (about 1300 feet) into the distance. This is an approximately true color rendering of images taken by the panoramic camera (Pancam) on NASA's Mars Exploration Rover Opportunity during the rover's 952nd sol, or Martian day, (Sept. 28, 2006) using the camera's 750-nanometer, 530-nanometer and 430-nanometer filters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/servlets/purl/974792','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/servlets/purl/974792"><span id="translatedtitle">2006 Toyota <span class="hlt">Highlander</span>-6395 Hyrid Electric Vehicle Battery Test Results</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Tyler Gray; Chester Motloch; James Francfort</p> <p>2010-01-01</p> <p>The U.S. Department of Energy's Advanced Vehicle Testing Activity conducts several different types of tests on hybrid electric vehicles, including testing hybrid electric vehicles batteries when both the vehicles and batteries are new, and at the conclusion of 160,000 miles of accelerated testing. This report documents the battery testing performed and battery testing results for the 2007 Toyota <span class="hlt">Highlander</span> hybrid electric vehicle (Vin Number JTEDW21A160006395). Testing was performed by the Electric Transportation Engineering Corporation. The Advanced Vehicle Testing Activity is part of the U.S. Department of Energy's Vehicle Technologies Program. The Idaho National Laboratory and the Electric Transportation Engineering Corporation conduct Advanced Vehicle Testing Activity for the U.S. Department of Energy.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5415069','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5415069"><span id="translatedtitle">Electronic control system for air fuel ratio compensation in <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Kimura, J.; Noji, A.</p> <p>1981-12-29</p> <p>An electronic control system which electronically controls the air fuel ratio of a mixture being supplied to a gasoline engine in <span class="hlt">highlands</span> is described. An orifice device is provided in a passage through which secondary air is supplied to the venturi section of the engine carburetor. An electronic control unit carries out programmed control of the orifice opening of the orifice device in response to the atmospheric pressure and the engine temperature to create a reference pressure. A further electronic control unit drives a second air control valve provided in the secondary air supply passage along a predetermined operating characteristic pattern in response to the difference between the reference pressure and an actual pressure present in the venturi section of the carburetor. A mixture having an optimum air fuel ratio corresponding to the atmospheric pressure can thus be supplied to the engine from the carburetor.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/servlets/purl/974752','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/servlets/purl/974752"><span id="translatedtitle">2006 Toyota <span class="hlt">Highlander</span>-5681 Hybrid Electric Vehicle Battery Test Results</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Tyler Gray; Chester Motloch; James Francfort</p> <p>2010-01-01</p> <p>The U.S. Department of Energy's Advanced Vehicle Testing Activity conducts several different types of tests on hybrid electric vehicles, including testing hybrid electric vehicles batteries when both the vehicles and batteries are new, and at the conclusion of 160,000 miles of accelerated testing. This report documents the battery testing performed and battery testing results for the 2007 Toyota <span class="hlt">Highlander</span> hybrid electric vehicle (Vin Number JTEDW21A860005681). Testing was performed by the Electric Transportation Engineering Corporation. The Advanced Vehicle Testing Activity is part of the U.S. Department of Energy's Vehicle Technologies Program. The Idaho National Laboratory and the Electric Transportation Engineering Corporation conduct Advanced Vehicle Testing Activity for the U.S. Department of Energy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17201301','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17201301"><span id="translatedtitle">[Malaria in the central <span class="hlt">highlands</span> of Madagascar: control strategies].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rabarijaona, L P; Rabe, T; Ranaivo, L H; Raharimalala, L A; Rakotomanana, F; Rakotondraibe, E M; Ramarosandratana, B; Rakotoson, J D; Rakotonjanabelo, L A; Tafangy, P B</p> <p>2006-10-01</p> <p>The purpose of this article is to present data on malaria in the central <span class="hlt">highland</span> plateaux of Madagascar and strategies to improve the national malaria control program. Use of rapid diagnosis strips, early home-based fever management with pre-packaged chloroquine treatment kits and proposed new therapeutic combination based on artemisinine are discussed for management of patients with high suspicion of malaria attack. Preventive measures including alternated targeted and full-house indoor spraying for vector control, use of insecticide-impregnated bednets, implementation of intermittent preventive treatment in risk groups, optimization of the epidemic early detection and warning system using the Lot Quality Assurance Sampling method for epidemiological investigation if the alert threshold is exceeded, and provision of rapid diagnosis strips are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/17963098','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/17963098"><span id="translatedtitle">Rebel girls? Unplanned pregnancy and colonialism in <span class="hlt">highlands</span> Papua, Indonesia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Butt, Leslie; Munro, Jenny</p> <p>2007-01-01</p> <p>In <span class="hlt">highlands</span> Papua, Indonesia, rapid social change under a colonial system of governance has created novel sexual opportunities for young indigenous women. Recent scholarship has viewed similar youthful sexual practices that challenge the status quo as expressions of personal agency. By looking at how young women and their families cope with unplanned pregnancies, we suggest that a more viable analytic approach would be to view sexuality, pregnancy and childbirth as a single unit of analysis. From this perspective, young women's experiences are primarily ones of constraint. Case studies offer insights into the ways a political context of colonial domination limits options and choices for young women who have children born out of wedlock. In particular, this paper describes how the 'settler gaze' - omnipresent colonial norms and judgments - creates regulatory effects in the realm of reproduction. PMID:17963098</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19901901','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19901901"><span id="translatedtitle">Cytotoxicity screening of endemic plants from Guayana <span class="hlt">highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guil-Guerrero, José Luis; Campra, Pablo</p> <p>2009-08-01</p> <p>A chemical-ecology approach has been used to screen plants growing in Guyana <span class="hlt">Highlands</span> as an indicator of production of biologically active secondary metabolites. Extracts of leaves from 19 species, most of them endemic in this area, and collected at the top of Roraima Tepui (2,723 m) were screened in vitro at different concentrations for their potential cytotoxic activity against three tumour cell lines: HT29 (colon), A549 (lung) and MDA-MB-231 (breast). MTT (tetrazolium blue) colorimetric assay was employed as cytotoxicity test. Extracts of nine species caused less than 30% growth in at least one cell line. From these species, high cytotoxic activity was detected in Casearia sylvestris var. lingua and Ledotamnus sessiliflorus extracts; medium activity was found in Cyathea sp. Two other species, Cyrilla racemiflora and Heliamphora minor showed lower but significant cytotoxicity. Further cytotoxicity-directed fractionation of these extracts would be advisable to isolate and identify the active principles of these plants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19920040774&hterms=ADC&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DADC','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19920040774&hterms=ADC&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DADC"><span id="translatedtitle">Venusian <span class="hlt">highlands</span> - Geoid to topography ratios and their implications</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Smrekar, Suzanne E.; Phillips, Roger J.</p> <p>1991-01-01</p> <p>Geoid-to-topography ratios (GTRs) are estimated for 12 Venusian <span class="hlt">highland</span> features to allow comparison with convection calculations and with terrestrial data of oceanic hot spots, swells, and plateaus. The geoid is estimated in the wavenumber domain from the isostatic formula, using the topography and the apparent depths isostatic compensation (ADC) for each region. In the space domain, the GTR is equal to the least squares slope of the linear fit of the geoid to the topograpy. The resulting GTR range is 7-31 m/km, which is much higher than terrestrial oceanic values (-1 to 5 m/km). The features fall into two distinct groups, one with a GTR range of 7-13 m/km, and one with a range of 19-25 m/km. A model for thermal thinning of a 100-km-thick lithosphere fits all values in the lower GTR group to within one standard deviation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19824309','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19824309"><span id="translatedtitle">[The pure being of writing. Ecriture automatique in 19th century psychiatry and early surrealism (<span class="hlt">Breton</span>/Soupault: Les champs magnétiques)].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bergengruen, Maximilian</p> <p>2009-03-01</p> <p>Ecriture automatique and psychoanalysis are often lumped together in literary studies, almost as a knee-jerk reaction. However, on closer inspection it can be seen that the discoverers of automatic writing--the surrealists--were more interested in the hysteria research that prevailed around the year 1900 (Pierre Janet, Alfred Binet) and in parapsychology (Frederic Myers). In these two branches of medicine, the theory and practice of automatic writing are based on an experimental constellation in which the relationship between the psychiatrist/experiment organiser and the patient/participant takes centre stage. Here, the latter writes in response to an order or question from the former, mostly while overcoming a physical or memory block. André <span class="hlt">Breton</span> and Philippe Soupault set up a very similar constellation in the Champs magnétiques, though with some key alterations. Indeed, surrealism liberates the patient engaging in automatic writing from the dictates of the psychiatrist--but only to submit him to a yet more overwhelming force, a pure violence of writing, so to speak: the automatism of a 'higher reality'.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/19824309','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/19824309"><span id="translatedtitle">[The pure being of writing. Ecriture automatique in 19th century psychiatry and early surrealism (<span class="hlt">Breton</span>/Soupault: Les champs magnétiques)].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bergengruen, Maximilian</p> <p>2009-03-01</p> <p>Ecriture automatique and psychoanalysis are often lumped together in literary studies, almost as a knee-jerk reaction. However, on closer inspection it can be seen that the discoverers of automatic writing--the surrealists--were more interested in the hysteria research that prevailed around the year 1900 (Pierre Janet, Alfred Binet) and in parapsychology (Frederic Myers). In these two branches of medicine, the theory and practice of automatic writing are based on an experimental constellation in which the relationship between the psychiatrist/experiment organiser and the patient/participant takes centre stage. Here, the latter writes in response to an order or question from the former, mostly while overcoming a physical or memory block. André <span class="hlt">Breton</span> and Philippe Soupault set up a very similar constellation in the Champs magnétiques, though with some key alterations. Indeed, surrealism liberates the patient engaging in automatic writing from the dictates of the psychiatrist--but only to submit him to a yet more overwhelming force, a pure violence of writing, so to speak: the automatism of a 'higher reality'. PMID:19824309</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70173632','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70173632"><span id="translatedtitle">Analysis of environmental factors influencing salinity patterns, oyster growth, and mortality in lower <span class="hlt">Breton</span> Sound Estuary, Louisiana using 20 years of data</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>LaPeyre, Megan K.; Geaghan, James; Decossas, Gary A.; La Peyre, Jerome F.</p> <p>2016-01-01</p> <p>Freshwater inflow characteristics define estuarine functioning by delivering nutrients, sediments, and freshwater, which affect biological resources and ultimately system production. Using 20 years of water quality, weather, and oyster growth and mortality data from <span class="hlt">Breton</span> Sound Estuary (BSE), Louisiana, we examined the relationship of riverine, weather, and tidal influence on estuarine salinity, and the relationship of salinity to oyster growth and mortality. Mississippi River discharge was found to be the most important factor determining salinity patterns over oyster grounds within lower portions of BSE, with increased river flow associated with lowered salinities, while easterly winds associated with increased salinity were less influential. These patterns were consistent throughout the year. Salinity and temperature (season) were found to critically control oyster growth and mortality, suggesting that seasonal changes to river discharge affecting water quality over the oyster grounds have profound impacts on oyster populations. The management of oyster reefs in estuaries (such as BSE) requires an understanding of how estuarine hydrodynamics and salinity are influenced by forcing factors such as winds, river flow, and by the volume, timing, and location of controlled releases of riverine water.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2642781','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2642781"><span id="translatedtitle">The use of magical plants by curanderos in the Ecuador <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Cavender, Anthony P; Albán, Manuel</p> <p>2009-01-01</p> <p>Although the use of plants for treating supernaturally caused illnesses (e.g., soul loss, evil wind, witchcraft) has been documented in the Ecuador <span class="hlt">highlands</span>, so-called magical plants have received much less focused attention than plants used for treating naturalistic disorders. Drawing on interviews done in 2002 and 2003 with 116 curanderos residing in the Ecuador <span class="hlt">highlands</span>, this paper examines the characteristics of plants identified as magical, how they are used, and how the study of magical plants provides insights into the mindscape of residents of the <span class="hlt">highlands</span>. PMID:19161618</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150018100','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150018100"><span id="translatedtitle">Strategies Geo<span class="hlt">Cape</span> Intelligent Observation Studies @ GSFC</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Cappelaere, Pat; Frye, Stu; Moe, Karen; Mandl, Dan; LeMoigne, Jacqueline; Flatley, Tom; Geist, Alessandro</p> <p>2015-01-01</p> <p>This presentation provides information a summary of the tradeoff studies conducted for Geo<span class="hlt">Cape</span> by the GSFC team in terms of how to optimize Geo<span class="hlt">Cape</span> observation efficiency. Tradeoffs include total ground scheduling with simple priorities, ground scheduling with cloud forecast, ground scheduling with sub-area forecast, onboard scheduling with onboard cloud detection and smart onboard scheduling and onboard image processing. The tradeoffs considered optimzing cost, downlink bandwidth and total number of images acquired.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994DSRII..41..809H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994DSRII..41..809H"><span id="translatedtitle">Unusual megafaunal assemblages on the continental slope off <span class="hlt">Cape</span> Hatteras</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hecker, Barbara</p> <p></p> <p>Megafaunal assemblages were studied in August-September 1992 using a towed camera sled along seven cross-isobath transects on the continental slope off <span class="hlt">Cape</span> Hatteras. A total of 20,722 megafaunal organisms were observed on 10,918 m 2 of the sea floor between the depths of 157 and 1 924 m. These data were compared with data previously collected off <span class="hlt">Cape</span> Hatteras in 1985 and at other locations along the eastern U.S. coast between 1981 and 1987. Megafaunal populations on the upper and lower slopes off <span class="hlt">Cape</span> Hatteras were fouond to be similar, in terms of density and species composition, to those observed at the other locations. In contrast, megafaunal abundances were found to be elevated (0.88 and 2.65 individuals per m 2 during 1985 and 1992, respectively) on the middle slope off <span class="hlt">Cape</span> Hatteras when compared to most other slope locations (<0.5individuals per m 2). These elevated abundances mainly reflect dense populations of three demersal fish, two eel pouts ( Lysenchelys verrilli and Lycodes atlanticus) and the witch flounder Glyptocephalus cynoglossus, and a large anemone ( Actinauge verrilli). These four species dominated the megafauna off <span class="hlt">Cape</span> Hatteras, whereas they represented only a minor component of megafaunal populations found at other slope locations. Additionally, numerous tubes of the foraminiferan Bathysiphon filiformis were observed off <span class="hlt">Cape</span> Hatteras, but not elsewhere. The high density of demersal fish found off <span class="hlt">Cape</span> Hatteras appears to be related to the high densities of infaunal prey reported from this area. The high densities of A. verrilli and B. fuliformis may be related to the same factors responsible for the high infaunal densities, namely enhanced nutrient inputs in the form of fine particles. Extreme patchiness also was observed in the distributions of the middle slope taxa off <span class="hlt">Cape</span> Hatteras. This patchiness may reflect the habitat heterogeneity of this exceptionally rugged slope and the sedentary nature of the organisms inhabiting it.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19820002800','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19820002800"><span id="translatedtitle">Lagrangian circulation study near <span class="hlt">Cape</span> Henry, Virginia. [Chesapeake Bay</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Johnson, R. E.</p> <p>1981-01-01</p> <p>A study of the circulation near <span class="hlt">Cape</span> Henry, Virginia, was made using surface and seabed drifters and radar tracked surface buoys coupled to subsurface drag plates. Drifter releases were conducted on a line normal to the beach just south of <span class="hlt">Cape</span> Henry. Surface drifter recoveries were few; wind effects were strongly noted. Seabed drifter recoveries all exhibited onshore motion into Chesapeake Bay. Strong winds also affected seabed recoveries, tending to move them farther before recovery. Buoy trajectories in the vicinity of <span class="hlt">Cape</span> Henry appeared to be of an irrotational nature, showing a clockwise rotary tide motion. Nearest the <span class="hlt">cape</span>, the buoy motion elongated to almost parallel depth contours around the <span class="hlt">cape</span>. Buoy motion under the action of strong winds showed that currents to at least the depth of the drag plates substantially are altered from those of low wind conditions near the Bay mouth. Only partial evidence could be found to support the presence of a clockwise nontidal eddy at Virginia Beach, south of <span class="hlt">Cape</span> Henry.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5050521','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5050521"><span id="translatedtitle">A Cretaceous origin for fire adaptations in the <span class="hlt">Cape</span> flora</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>He, Tianhua; Lamont, Byron B.; Manning, John</p> <p>2016-01-01</p> <p>Fire has had a profound effect on the evolution of worldwide biotas. The <span class="hlt">Cape</span> Floristic Region is one of the world’s most species-rich regions, yet it is highly prone to recurrent fires and fire-adapted species contribute strongly to the overall flora. It is hypothesized that the current fire regimes in the <span class="hlt">Cape</span> could be as old as 6–8 million years (My), while indirect evidence indicates that the onset of fire could have reached 18 million years ago (Ma). Here, we trace the origin of fire-dependent traits in two monocot families that are significant elements in the fire-prone <span class="hlt">Cape</span> flora. Our analysis shows that fire-stimulated flowering originated in the <span class="hlt">Cape</span> Haemodoraceae 81 Ma, while fire-stimulated germination arose in the African Restionaceae at least 70 Ma, implying that wildfires have been a significant force in the evolution of the <span class="hlt">Cape</span> flora at least 60 My earlier than previous estimates. Our results provide strong evidence for the presence of fire adaptations in the <span class="hlt">Cape</span> from the Cretaceous, leading to the extraordinary persistence of a fire-adapted flora in this biodiversity hotspot, and giving support to the hypothesis that Cretaceous fire was a global phenomenon that shaped the evolution of terrestrial floras. PMID:27703273</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26952840','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26952840"><span id="translatedtitle">SENP1, but not fetal hemoglobin, differentiates Andean <span class="hlt">highlanders</span> with chronic mountain sickness from healthy individuals among Andean <span class="hlt">highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hsieh, Matthew M; Callacondo, David; Rojas-Camayo, Jose; Quesada-Olarte, Jose; Wang, Xunde; Uchida, Naoya; Maric, Irina; Remaley, Alan T; Leon-Velarde, Fabiola; Villafuerte, Francisco C; Tisdale, John F</p> <p>2016-06-01</p> <p>Chronic mountain sickness (CMS) results from chronic hypoxia. It is unclear why certain <span class="hlt">highlanders</span> develop CMS. We hypothesized that modest increases in fetal hemoglobin (HbF) are associated with lower CMS severity. In this cross-sectional study, we found that HbF levels were normal (median = 0.4%) in all 153 adult Andean natives in Cerro de Pasco, Peru. Compared with healthy adults, the borderline elevated hemoglobin group frequently had symptoms (headaches, tinnitus, cyanosis, dilatation of veins) of CMS. Although the mean hemoglobin level differed between the healthy (17.1 g/dL) and CMS (22.3 g/dL) groups, mean plasma erythropoietin (EPO) levels were similar (healthy, 17.7 mIU/mL; CMS, 12.02 mIU/mL). Sanger sequencing determined that single-nucleotide polymorphisms in endothelial PAS domain 1 (EPAS1) and egl nine homolog 1 (EGLN1), associated with lower hemoglobin in Tibetans, were not identified in Andeans. Sanger sequencing of sentrin-specific protease 1 (SENP1) and acidic nuclear phosphoprotein 32 family, member D (ANP32D), in healthy and CMS individuals revealed that non-G/G genotypes were associated with higher CMS scores. No JAK2 V617F mutation was detected in CMS individuals. Thus, HbF and other classic erythropoietic parameters did not differ between healthy and CMS individuals. However, the non-G/G genotypes of SENP1 appeared to differentiate individuals with CMS from healthy Andean <span class="hlt">highlanders</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70010094','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70010094"><span id="translatedtitle">Differentiation and volcanism in the lunar <span class="hlt">highlands</span>: photogeologic evidence and Apollo 16 implications</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Trask, N.J.; McCauley, J.F.</p> <p>1972-01-01</p> <p>Materials of possible volcanic origin in the lunar <span class="hlt">highlands</span> include (1) <span class="hlt">highland</span> plains materials, (2) materials forming closely spaced hills in which summit furrows and chains of craters are common and (3) materials forming closely spaced hills (some of which parallel the lunar grid) on which summit furrows and chain craters are rare. The <span class="hlt">highland</span> plains materials probably are basaltic lavas with less Fe and Ti than the mare plains materials. The two hilly units appear to consist of materials that, if volcanic, were more viscous in the molten state than any of the lunar plains units; thus these materials may be significantly enriched in felsic components. Most of the <span class="hlt">highland</span> materials of possible volcanic origin formed after the Imbrium multi-ring basin but before mare material completed flooding parts of the moon; they therefore postdate accretion of the moon and may represent several episodes of premare volcanism. ?? 1972.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=75535&keyword=Deforestation&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68456007&CFTOKEN=73405563','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=75535&keyword=Deforestation&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68456007&CFTOKEN=73405563"><span id="translatedtitle">IDENTIFICATION AND LOCATION OF FUNDAMENTAL FISH ASSEMBLAGES IN THE MID-ATLANTIC <span class="hlt">HIGHLANDS</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>To predict fish community response to environmental restoration in the <span class="hlt">Highlands</span> Region one must first have information on fish abundance and diversity. We used data collected by the US Environmental Protection Agency's EMAP (Environmental Monitoring and Assessment Program) to i...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016LPICo1911.6038O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016LPICo1911.6038O"><span id="translatedtitle">Composition of the Lunar <span class="hlt">Highland</span> Crust and Mantle and Its Implications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ohtake, M.; Yamamoto, S.; Uemoto, K.</p> <p>2016-05-01</p> <p>Recent remote sensing data suggest that extremely pure anorthosite (PAN) layer is a main component of the lunar <span class="hlt">highland</span> crust and presence of crustal material with higher Mg# on the farside than the nearside.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19940007707&hterms=echo+sounder&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3D%2528echo%2Bsounder%2529','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19940007707&hterms=echo+sounder&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3D%2528echo%2Bsounder%2529"><span id="translatedtitle">Using lunar sounder imagery to distinguish surface from subsurface reflectors in lunar <span class="hlt">highlands</span> areas</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Cooper, Bonnie L.; Carter, James L.</p> <p>1993-01-01</p> <p>We have developed a method using the Apollo 17 Lunar Sounder imagery data which appears capable of filtering out off-nadir surface noise from <span class="hlt">highland</span> area profiles, so that subsurface features may now be detected in <span class="hlt">highland</span> areas as well as mare areas. Previously, this had been impossible because the rough topography in the <span class="hlt">highland</span> areas created noise in the profiles which could not be distinguished from subsurface echoes. The new method is an image processing procedure involving the computerized selection of pixels which represent intermediate echo intensity values, then manually removing those pixels from the profile. Using this technique, a subsurface feature with a horizontal extent of about 150 km, at a calculated depth of approximately 3 km, has been detected beneath the crater Riccioli in the <span class="hlt">highlands</span> near Oceanus Procellarum. This result shows that the ALSE data contain much useful information that remains to be extracted and used.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.usgs.gov/of/2010/1187/','USGSPUBS'); return false;" href="http://pubs.usgs.gov/of/2010/1187/"><span id="translatedtitle">Connecticut <span class="hlt">Highlands</span> Technical Report - Documentation of the Regional Rainfall-Runoff Model</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Ahearn, Elizabeth A.; Bjerklie, David M.</p> <p>2010-01-01</p> <p>This report provides the supporting data and describes the data sources, methodologies, and assumptions used in the assessment of existing and potential water resources of the <span class="hlt">Highlands</span> of Connecticut and Pennsylvania (referred to herein as the “Highlands”). Included in this report are <span class="hlt">Highlands</span> groundwater and surface-water use data and the methods of data compilation. Annual mean streamflow and annual mean base-flow estimates from selected U.S. Geological Survey (USGS) gaging stations were computed using data for the period of record through water year 2005. The methods of watershed modeling are discussed and regional and sub-regional water budgets are provided. Information on <span class="hlt">Highlands</span> surface-water-quality trends is presented. USGS web sites are provided as sources for additional information on groundwater levels, streamflow records, and ground- and surface-water-quality data. Interpretation of these data and the findings are summarized in the <span class="hlt">Highlands</span> study report.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4830403','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4830403"><span id="translatedtitle">Emergence or improved detection of Japanese encephalitis virus in the Himalayan <span class="hlt">highlands</span>?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Baylis, Matthew; Barker, Christopher M.; Caminade, Cyril; Joshi, Bhoj R.; Pant, Ganesh R.; Rayamajhi, Ajit; Reisen, William K.; Impoinvil, Daniel E.</p> <p>2016-01-01</p> <p>The emergence of Japanese encephalitis virus (JEV) in the Himalayan <span class="hlt">highlands</span> is of significant veterinary and public health concern and may be related to climate warming and anthropogenic landscape change, or simply improved surveillance. To investigate this phenomenon, a One Health approach focusing on the phylogeography of JEV, the distribution and abundance of the mosquito vectors, and seroprevalence in humans and animal reservoirs would be useful to understand the epidemiology of Japanese encephalitis in <span class="hlt">highland</span> areas. PMID:26956778</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19820038740&hterms=contaminated&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcontaminated','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19820038740&hterms=contaminated&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dcontaminated"><span id="translatedtitle">The distinction of pristine from meteorite-contaminated <span class="hlt">highlands</span> rocks using metal compositions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ryder, G.; Norman, M. D.; Score, R. A.</p> <p>1980-01-01</p> <p>Pristine <span class="hlt">highlands</span> rocks, i.e., those which have retained the chemical characteristics they acquired from igneous processes, contain metal grains whose Ni and Co contents are distinct from those in most polymict, meteorite-contaminated rocks. The difference is mainly a result of the bulk Ni/Co ratios of pristine rocks being much lower than those of chondritic meteorites. The compositions of metal grains thus provide a rapid and effective criterion for the recognition of pristine <span class="hlt">highlands</span> samples.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/26956778','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/26956778"><span id="translatedtitle">Emergence or improved detection of Japanese encephalitis virus in the Himalayan <span class="hlt">highlands</span>?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Baylis, Matthew; Barker, Christopher M; Caminade, Cyril; Joshi, Bhoj R; Pant, Ganesh R; Rayamajhi, Ajit; Reisen, William K; Impoinvil, Daniel E</p> <p>2016-04-01</p> <p>The emergence of Japanese encephalitis virus (JEV) in the Himalayan <span class="hlt">highlands</span> is of significant veterinary and public health concern and may be related to climate warming and anthropogenic landscape change, or simply improved surveillance. To investigate this phenomenon, a One Health approach focusing on the phylogeography of JEV, the distribution and abundance of the mosquito vectors, and seroprevalence in humans and animal reservoirs would be useful to understand the epidemiology of Japanese encephalitis in <span class="hlt">highland</span> areas. PMID:26956778</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19820038752&hterms=density+iron&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Ddensity%2Biron','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19820038752&hterms=density+iron&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Ddensity%2Biron"><span id="translatedtitle">Lunar <span class="hlt">highland</span> crustal models based on iron concentrations - Isostasy and center-of-mass displacement</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Haines, E. L.; Metzger, A. E.</p> <p>1980-01-01</p> <p>Data is introduced on the iron concentrations of the lunar surface which have been refined by means of convolution corrections to restore the spatial resolution and contrast lost by the omnidirectional spectrometer. This refined iron data is synthesized with other orbital seismic, and lunar sample data to derive <span class="hlt">highland</span> crustal density and thickness, and isostasy and lunar centers of mass models are examined in light of this new information. A model is developed by which <span class="hlt">highland</span> crustal density is calculated for each <span class="hlt">highland</span> region from orbital observations of Fe, Mg and Ti concentrations. The results of this model are presented numerically and graphically for 35 <span class="hlt">highland</span> and two non-<span class="hlt">highland</span> regions. Density and thickness results are then applied to two long-standing lunar problems: (1) the nature of <span class="hlt">highland</span> isostasy, which is shown to be controlled by crustal thickness rather than density, and (2) the separation of the moon's mass and figure centers, which is shown to be due to the crustal thickness difference between the lunar near and far sides.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23783403','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23783403"><span id="translatedtitle">Conopeptides from <span class="hlt">Cape</span> Verde Conus crotchii.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Neves, Jorge; Campos, Alexandre; Osório, Hugo; Antunes, Agostinho; Vasconcelos, Vitor</p> <p>2013-06-01</p> <p>Marine Cone snails of the genus Conus contain complex peptide toxins in their venom. Living in tropical habitats, they usually use the powerful venom for self-defense and prey capture. Here, we study Conus crotchii venom duct using a peptide mass-matching approach. The C. crotchii was collected on the <span class="hlt">Cape</span> Verde archipelago in the Boa Vista Island. The venom was analyzed using matrix-assisted laser desorption/ionization time-of-flight mass spectrometry (MALDI-TOF MS). About 488 molecular masses between 700 Da and 3000 Da were searched bymatching with known peptide sequences from UniProtKB protein sequence database. Through this method we were able to identify 12 conopeptides. For validation we considered the error between the experimental molecular mass (monoisotopic) and the calculated mass of less than 0.5 Da. All conopeptides detected belong to the A-, O1-, O2-, O3-, T- and D-superfamilies, which can block Ca²⁺ channels, inhibit K⁺ channels and act on nicotinic acetylcholine receptors (nAChRs). Only a few of the detected peptides have a 100% UniProtKB database similarity, suggesting that several of them could be newly discovered marine drugs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2007/1375/start.html','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2007/1375/start.html"><span id="translatedtitle">EAARL topography: <span class="hlt">Cape</span> Cod National Seashore</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Brock, John C.; Wright, C. Wayne; Patterson, Matt; Nayegandhi, Amar; Travers, Laurinda J.</p> <p>2007-01-01</p> <p>This Web site contains 90 Lidar-derived bare earth topography maps and GIS files for the <span class="hlt">Cape</span> Cod National Seashore. These Lidar-derived topography maps were produced as a collaborative effort between the U.S. Geological Survey (USGS) Florida Integrated Science Center (FISC) St. Petersburg, Florida, the National Park Service (NPS), Northeast Coastal and Barrier Network, Inventory and Monitoring Program, and the National Aeronautics and Space Administration (NASA) Wallops Flight Facility. One objective of this research is to create techniques to survey coral reefs and barrier islands for the purposes of geomorphic change studies, habitat mapping, ecological monitoring, change detection, and event assessment. As part of this project, data from an innovative instrument under development at the NASA Wallops Flight Facility, the NASA Experimental Airborne Advanced Research Lidar (EAARL) are being used. This sensor has the potential to make significant contributions in this realm for measuring subaerial and submarine topography wthin cross-environment surveys. High spectral resolution, water-column correction, and low costs were found to be key factors in providing accurate and affordable imagery to coastal resource managers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA10105&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA10105&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde"><span id="translatedtitle">Opportunity's Second Martian Birthday at <span class="hlt">Cape</span> Verde</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2007-01-01</p> <p><p/> A promontory nicknamed '<span class="hlt">Cape</span> Verde' can be seen jutting out from the walls of Victoria Crater in this approximate true-color picture taken by the panoramic camera on NASA's Mars Exploration Rover Opportunity. The rover took this picture on martian day, or sol, 1329 (Oct. 20, 2007), more than a month after it began descending down the crater walls -- and just 9 sols shy of its second Martian birthday on sol 1338 (Oct. 29, 2007). Opportunity landed on the Red Planet on Jan. 25, 2004. That's nearly four years ago on Earth, but only two on Mars because Mars takes longer to travel around the sun than Earth. One Martian year equals 687 Earth days. <p/> The overall soft quality of the image, and the 'haze' seen in the lower right portion, are the result of scattered light from dust on the front sapphire window of the rover's camera. <p/> This view was taken using three panoramic-camera filters, admitting light with wavelengths centered at 750 nanometers (near infrared), 530 nanometers (green) and 430 nanometers (violet).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70148691','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70148691"><span id="translatedtitle">Differences in extreme low salinity timing and duration differentially affect eastern oyster (Crassostrea virginica) size class growth and mortality in <span class="hlt">Breton</span> Sound, LA</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>LaPeyre, Megan K.; Eberline, Benjamin S.; Soniat, Thomas M.; La Peyre, Jerome F.</p> <p>2013-01-01</p> <p>Understanding how different life history stages are impacted by extreme or stochastic environmental variation is critical for predicting and modeling organism population dynamics. This project examined recruitment, growth, and mortality of seed (25–75 mm) and market (>75 mm) sized oysters along a salinity gradient over two years in <span class="hlt">Breton</span> Sound, LA. In April 2010, management responses to the Deepwater Horizon oil spill resulted in extreme low salinity (<5) at all sites through August 2010; in 2011, a 100-year Mississippi River flood event resulted in low salinity in late spring. Extended low salinity (<5) during hot summer months (>25 °C) significantly and negatively impacted oyster recruitment, survival and growth in 2010, while low salinity (<5) for a shorter period that did not extend into July (<25 °C) in 2011 had minimal impacts on oyster growth and mortality. In 2011, recruitment was limited, which may be due to a combination of low spring time salinities, high 2010 oyster mortality, minimal 2010 recruitment, cumulative effects from 10 years of declining oyster stock in the area, and poor cultch quality. In both 2010 and 2011, Perkinsus marinusinfection prevalence remained low throughout the year at all sites and almost all infection intensities were light. Oyster plasma osmolality failed to match surrounding low salinity waters in 2010, while oysters appeared to osmoconform throughout 2011 indicating that the high mortality in 2010 may be due to extended valve closing and resulting starvation or asphyxiation in response to the combination of low salinity during high temperatures (>25 °C). With increasing management of our freshwater inputs to estuaries combined with predicted climate changes, how extreme events affect different life history stages is key to understanding variation in population demographics of commercially important species and predicting future populations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/ds/0838/ds838title.html','USGSPUBS'); return false;" href="https://pubs.usgs.gov/ds/0838/ds838title.html"><span id="translatedtitle">Topographic lidar survey of Dauphin Island, Alabama and Chandeleur, Stake, Grand Gosier and <span class="hlt">Breton</span> Islands, Louisiana, July 12-14, 2013</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Guy, Kristy K.; Plant, Nathaniel G.</p> <p>2014-01-01</p> <p>This Data Series Report contains lidar elevation data collected on July 12 and 14, 2013, for Dauphin Island, Alabama, and Chandeleur, Stake, Grand Gosier and <span class="hlt">Breton</span> Islands, Louisiana. Classified point cloud data—data points described in three dimensions—in lidar data exchange format (LAS) and bare earth digital elevation models (DEMs) in ERDAS Imagine raster format (IMG) are available as downloadable files. Photo Science, Inc., was contracted by the U.S. Geological Survey (USGS) to collect and process these data. The lidar data were acquired at a horizontal spacing (or nominal pulse spacing) of 1 meter (m) or less. The USGS surveyed points within the project area from July 14–23, 2013, for use in ground control and accuracy assessment. Photo Science, Inc., calculated a vertical root mean square error (RMSEz) of 0.012 m by comparing 10 surveyed points to an interpolated elevation surface of unclassified lidar data. The USGS also checked the data using 80 surveyed points and unclassified lidar point elevation data and found an RMSEz of 0.073 m. The project specified an RMSEz of 0.0925 m or less. The lidar survey was acquired to document the short- and long-term changes of several different barrier island systems. Specifically, this survey supports detailed studies of Chandeleur and Dauphin Islands that resolve annual changes in beaches, berms and dunes associated with processes driven by storms, sea-level rise, and even human restoration activities. These lidar data are available to Federal, State and local governments, emergency-response officials, resource managers, and the general public.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMOS21D1786R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMOS21D1786R"><span id="translatedtitle">Marsh loss from 1984 - 2011 in the <span class="hlt">Breton</span> Sound, Barataria and Terrebonne Basins, Louisiana, U.S.A.: Impacts of hurricanes and excess nutrients</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Riter, J. C.; Kearney, M. S.; Turner, R.</p> <p>2012-12-01</p> <p>Twenty-four Landsat data sets (1984-2011), collected as close to peak vegetation growth as possible, were used to evaluate marsh vegetation health and marsh loss in Terrebonne, Barataria, and <span class="hlt">Breton</span> Sound Basins. Marsh loss varies spatially and temporally in the basins: freshwater and most intermediate marshes located west of the Mississippi River and more than 40 km from the coast were determined to be more stable than marshes closer to the coast. In most areas of the three basins, vegetation health and marsh area from 1984-1992 were relatively stable with minor inter-annual fluctuations throughout each basin and only a few areas of localized marsh loss. By 1994, shoreline erosion, tidal creek erosion, and erosion of soil banks adjacent to canals had increased in marshes located <40 km from the Gulf of Mexico, although some sites suffered substantially greater erosion than most coastal areas. Wave erosion also increased around the shores of Lakes Salvador, Cataouatche, Levy and other large lakes by 1994. Marsh loss also occurred in marshes immediately west of the Mississippi River, especially in areas close to diversion inlets. Hurricane Ivan in 2004 produced little sustained widespread damage in the basin marshes. However, Hurricanes Katrina and Rita in 2005 and Gustav and Ike in 2008 caused extensive erosion of vegetation and the marsh substrate, especially near the inlet to Caernarvon diversion, but also near the Naomi and West Point a La Hache diversions inlets. We attribute the significant marsh damage from hurricanes to greater flooding, and greater wave and storm surge impacts due to diminished marsh soil strength from the effects of excess nutrients causing lower rhizome and root biomass and increased substrate decomposition rates.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ECSS..135..146L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ECSS..135..146L"><span id="translatedtitle">Differences in extreme low salinity timing and duration differentially affect eastern oyster (Crassostrea virginica) size class growth and mortality in <span class="hlt">Breton</span> Sound, LA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>La Peyre, Megan K.; Eberline, Benjamin S.; Soniat, Thomas M.; La Peyre, Jerome F.</p> <p>2013-12-01</p> <p>Understanding how different life history stages are impacted by extreme or stochastic environmental variation is critical for predicting and modeling organism population dynamics. This project examined recruitment, growth, and mortality of seed (25-75 mm) and market (>75 mm) sized oysters along a salinity gradient over two years in <span class="hlt">Breton</span> Sound, LA. In April 2010, management responses to the Deepwater Horizon oil spill resulted in extreme low salinity (<5) at all sites through August 2010; in 2011, a 100-year Mississippi River flood event resulted in low salinity in late spring. Extended low salinity (<5) during hot summer months (>25 °C) significantly and negatively impacted oyster recruitment, survival and growth in 2010, while low salinity (<5) for a shorter period that did not extend into July (<25 °C) in 2011 had minimal impacts on oyster growth and mortality. In 2011, recruitment was limited, which may be due to a combination of low spring time salinities, high 2010 oyster mortality, minimal 2010 recruitment, cumulative effects from 10 years of declining oyster stock in the area, and poor cultch quality. In both 2010 and 2011, Perkinsus marinus infection prevalence remained low throughout the year at all sites and almost all infection intensities were light. Oyster plasma osmolality failed to match surrounding low salinity waters in 2010, while oysters appeared to osmoconform throughout 2011 indicating that the high mortality in 2010 may be due to extended valve closing and resulting starvation or asphyxiation in response to the combination of low salinity during high temperatures (>25 °C). With increasing management of our freshwater inputs to estuaries combined with predicted climate changes, how extreme events affect different life history stages is key to understanding variation in population demographics of commercially important species and predicting future populations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23508886','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23508886"><span id="translatedtitle">Rural income and forest reliance in <span class="hlt">highland</span> Guatemala.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Prado Córdova, José Pablo; Wunder, Sven; Smith-Hall, Carsten; Börner, Jan</p> <p>2013-05-01</p> <p>This paper estimates rural household-level forest reliance in the western <span class="hlt">highlands</span> of Guatemala using quantitative methods. Data were generated by the way of an in-depth household income survey, repeated quarterly between November 2005 and November 2006, in 11 villages (n = 149 randomly selected households). The main sources of income proved to be small-scale agriculture (53 % of total household income), wages (19 %) and environmental resources (14 %). The latter came primarily from forests (11 % on average). In the poorest quintile the forest income share was as high as 28 %. All households harvest and consume environmental products. In absolute terms, environmental income in the top quintile was 24 times higher than in the lowest. Timber and poles, seeds, firewood and leaf litter were the most important forest products. Households can be described as 'regular subsistence users': the share of subsistence income is high, with correspondingly weak integration into regional markets. Agricultural systems furthermore use important inputs from surrounding forests, although forests and agricultural uses compete in household specialization strategies. We find the main household determinants of forest income to be household size, education and asset values, as well as closeness to markets and agricultural productivity. Understanding these common but spatially differentiated patterns of environmental reliance may inform policies aimed at improving livelihoods and conserving forests.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/7845274','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/7845274"><span id="translatedtitle">Family characteristics of suicides in Cameron <span class="hlt">Highlands</span>: a controlled study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Maniam, T</p> <p>1994-09-01</p> <p>Cameron <span class="hlt">Highlands</span> has one of the highest suicide rates in the world, especially among Indians. Forty Indian families (19 suicides; 21 controls) were studied to compare family characteristics such as income, overcrowding, birth order of index cases of suicide, family history of suicidal behaviour or mental illness, marital disharmony, presence of alcohol abuse, availability of, and knowledge about, weedicides/insecticides, talk/threat of suicide among family members and experience of significant losses in the past year. Controls were matched for age, sex and educational level with the index cases of suicide. A significant difference was only found for one of the above factors, namely increased experience of significant losses in the past year in the family of index cases of suicide. More than 75% in both groups had alcohol related problems. About equal proportions in each group had a family history of suicidal behaviour and mental illness. There was more marital disharmony in families of suicides but this failed to reach significance. These results and methodological limitations of this study are discussed. PMID:7845274</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70013892','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70013892"><span id="translatedtitle">Crustal structure of the Appalachian <span class="hlt">Highlands</span> in Tennessee</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Prodehl, C.; Schlittenhardt, J.; Stewart, S.W.</p> <p>1984-01-01</p> <p>Crustal structure of the southern Appalachians and adjacent Interior Low Plateaus in Tennessee is derived from seismic-refraction measurements observed by the U.S. Geological Survey in 1965 along reversed lines, normal (NW-SE) and parallel (NE-SW) to the structure of the Appalachian <span class="hlt">Highlands</span>' major geologic divisions. Its easternmost part is located approximately 80 km southwest of the westernmost part of the COCORP seismic-reflection traverse within the Blue Ridge province. The velocity-depth models derived for both observational directions consist of three crustal layers with surprisingly high velocities, being about 6.1-6.2 km/s in the upper crust down to 7-10 km depth, 6.7-6.8 km/s for the middle crust between about 17 and 34 km and varying from 7.1 to 7.4 km/s for the lower crust at about 40-47 km depth. The boundaries between the three crustal layers as well as the crust-mantle boundary are transition zones of up to 11 km thickness. Similar to old orogens in other parts of the earth, the main result is a thick crust, at places in excess of 50 km, with high average velocity and a broad crust-mantle transition zone. ?? 1984.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EnMan..51.1034P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EnMan..51.1034P"><span id="translatedtitle">Rural Income and Forest Reliance in <span class="hlt">Highland</span> Guatemala</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prado Córdova, José Pablo; Wunder, Sven; Smith-Hall, Carsten; Börner, Jan</p> <p>2013-05-01</p> <p>This paper estimates rural household-level forest reliance in the western <span class="hlt">highlands</span> of Guatemala using quantitative methods. Data were generated by the way of an in-depth household income survey, repeated quarterly between November 2005 and November 2006, in 11 villages ( n = 149 randomly selected households). The main sources of income proved to be small-scale agriculture (53 % of total household income), wages (19 %) and environmental resources (14 %). The latter came primarily from forests (11 % on average). In the poorest quintile the forest income share was as high as 28 %. All households harvest and consume environmental products. In absolute terms, environmental income in the top quintile was 24 times higher than in the lowest. Timber and poles, seeds, firewood and leaf litter were the most important forest products. Households can be described as `regular subsistence users': the share of subsistence income is high, with correspondingly weak integration into regional markets. Agricultural systems furthermore use important inputs from surrounding forests, although forests and agricultural uses compete in household specialization strategies. We find the main household determinants of forest income to be household size, education and asset values, as well as closeness to markets and agricultural productivity. Understanding these common but spatially differentiated patterns of environmental reliance may inform policies aimed at improving livelihoods and conserving forests.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.jstor.org/stable/2694809','USGSPUBS'); return false;" href="http://www.jstor.org/stable/2694809"><span id="translatedtitle">Figurines, flint clay sourcing, the Ozark <span class="hlt">Highlands</span>, and Cahokian acquisition</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Emerson, T.E.; Hughes, R.E.</p> <p>2000-01-01</p> <p>At the pinnacle of Eastern Woodlands' prehistoric cultural development, Cahokia has been interpreted as a political and economic power participating in prestige-goods exchanges and trade networks stretching from the Great Plains to the South Atlantic. Among the more spectacular of the Cahokian elite artifacts were stone pipes and figurines made from a distinctive red stone previously identified as Arkansas bauxite. In this research, we used a combination of X-ray diffraction, sequential acid dissolution, and inductively coupled plasma analyses to establish the source of the raw material used in the manufacture of the red figurines and pipes that epitomize the Cahokian-style. Our research demonstrates that these objects were made of locally available flint clays. This finding, in conjunction with other evidence, indicate Cahokian exploitation of many mineral and stone resources focuses on the northern Ozark <span class="hlt">Highlands</span> to the exclusion of other areas. These findings indicate that we must reassess the direction, extent, and role of Cahokian external contacts and trade in elite goods. Copyright ?? 2000 by the Society for American Archaeology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/19901901','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/19901901"><span id="translatedtitle">Cytotoxicity screening of endemic plants from Guayana <span class="hlt">highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guil-Guerrero, José Luis; Campra, Pablo</p> <p>2009-08-01</p> <p>A chemical-ecology approach has been used to screen plants growing in Guyana <span class="hlt">Highlands</span> as an indicator of production of biologically active secondary metabolites. Extracts of leaves from 19 species, most of them endemic in this area, and collected at the top of Roraima Tepui (2,723 m) were screened in vitro at different concentrations for their potential cytotoxic activity against three tumour cell lines: HT29 (colon), A549 (lung) and MDA-MB-231 (breast). MTT (tetrazolium blue) colorimetric assay was employed as cytotoxicity test. Extracts of nine species caused less than 30% growth in at least one cell line. From these species, high cytotoxic activity was detected in Casearia sylvestris var. lingua and Ledotamnus sessiliflorus extracts; medium activity was found in Cyathea sp. Two other species, Cyrilla racemiflora and Heliamphora minor showed lower but significant cytotoxicity. Further cytotoxicity-directed fractionation of these extracts would be advisable to isolate and identify the active principles of these plants. PMID:19901901</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5822616','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5822616"><span id="translatedtitle">Pristine <span class="hlt">highland</span> clasts in consortium breccia 14305 Petrology and geochemistry</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Shervais, J.W.; Taylor, L.A.</p> <p>1984-11-15</p> <p>Data are presented on the petrography and mineral chemistry of six pristine <span class="hlt">highland</span> clasts chipped from the polymict lunar breccia 14305. Major and trace elements in the clasts were determined by instrumental neutron activation analysis, and mineral analyses were performed by electron microprobe. Mg-suite clasts have eastern geochemical affinities, reaffirming the importance of local variations in geochemistry. These local variations are superimposed on the moon-wide, longitudinal variations noted by Warren and Wasson (1980). Alkali anorthosites and Mg-suite troctolites and anorthosites are not comagmatic, and cannot be related to a single parent magma by either fractional crystallization or variable assimilation of KREEP. Both magma suites may have assimilated varied amounts of KREEP into distinct parent magmas. Alternatively, alkali anorthosites may have crystallized directly from a KREEP-basalt parent magma. A thick crust of ferroan anorthosite probably never existed on the western lunar nearside, or was removed by basin-forming impacts prior to intrusion of later plutonic suites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/23508886','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/23508886"><span id="translatedtitle">Rural income and forest reliance in <span class="hlt">highland</span> Guatemala.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Prado Córdova, José Pablo; Wunder, Sven; Smith-Hall, Carsten; Börner, Jan</p> <p>2013-05-01</p> <p>This paper estimates rural household-level forest reliance in the western <span class="hlt">highlands</span> of Guatemala using quantitative methods. Data were generated by the way of an in-depth household income survey, repeated quarterly between November 2005 and November 2006, in 11 villages (n = 149 randomly selected households). The main sources of income proved to be small-scale agriculture (53 % of total household income), wages (19 %) and environmental resources (14 %). The latter came primarily from forests (11 % on average). In the poorest quintile the forest income share was as high as 28 %. All households harvest and consume environmental products. In absolute terms, environmental income in the top quintile was 24 times higher than in the lowest. Timber and poles, seeds, firewood and leaf litter were the most important forest products. Households can be described as 'regular subsistence users': the share of subsistence income is high, with correspondingly weak integration into regional markets. Agricultural systems furthermore use important inputs from surrounding forests, although forests and agricultural uses compete in household specialization strategies. We find the main household determinants of forest income to be household size, education and asset values, as well as closeness to markets and agricultural productivity. Understanding these common but spatially differentiated patterns of environmental reliance may inform policies aimed at improving livelihoods and conserving forests. PMID:23508886</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70035700','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70035700"><span id="translatedtitle">Watershed morphology of <span class="hlt">highland</span> and mountain ecoregions in eastern Oklahoma</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Splinter, D.K.; Dauwalter, D.C.; Marston, R.A.; Fisher, W.L.</p> <p>2011-01-01</p> <p>The fluvial system represents a nested hierarchy that reflects the relationship among different spatial and temporal scales. Within the hierarchy, larger scale variables influence the characteristics of the next lower nested scale. Ecoregions represent one of the largest scales in the fluvial hierarchy and are defined by recurring patterns of geology, climate, land use, soils, and potential natural vegetation. Watersheds, the next largest scale, are often nested into a single ecoregion and therefore have properties that are indicative of a given ecoregion. Differences in watershed morphology (relief, drainage density, circularity ratio, relief ratio, and ruggedness number) were evaluated among three ecoregions in eastern Oklahoma: Ozark <span class="hlt">Highlands</span>, Boston Mountains, and Ouachita Mountains. These ecoregions were selected because of their high-quality stream resources and diverse aquatic communities and are of special management interest to the Oklahoma Department of Wildlife Conservation. One hundred thirty-four watersheds in first-through fourth-order streams were compared. Using a nonparametric, two-factor analysis of variance (?? = 0.05) we concluded that the relief, drainage density, relief ratio, and ruggedness number all changed among ecoregion and stream order, whereas circularity ratio only changed with stream order. Our study shows that ecoregions can be used as a broad-scale framework for watershed management. ?? 2011 by Association of American Geographers.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.P13D1699C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.P13D1699C"><span id="translatedtitle">New Elemental Maps of the Nearside Lunar <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Carter, J. A.; Grande, M.; Bisi, M. M.</p> <p>2011-12-01</p> <p>A set of elemental maps obtained by the Chandrayaan-1 X-ray Spectrometer (C1XS) and covering the Southern Nearside Lunar <span class="hlt">Highland</span> region will be presented. This region broadly covers the area below 10 S latitude and between -10 to +30 E longitude. It has never been the subject of a sample return mission; the nearest ground truth measurements are Apollo 16 at 8.56 S, 15.3 E and Surveyor 7 at 41 S, -11 E - this is mainly due to the uneven, mountainous terrain which makes spacecraft landings hazardous. The region has very high relief, with large slopes and rough surface features - these characteristics complicate the analysis of X-ray fluorescence analysis. Chandrayaan-1 flew at a time coinciding with a predicted increase in solar activity. For an X-ray fluorescence instrument, which relies on incident solar X-rays to illuminate the surface, this increase in activity would be enough to guarantee ~100% surface coverage in Mg, Al and Si, and significant areas in Fe, Ti, and Ca. However, the solar cycle was delayed, and instead C1XS launched into the quietest solar conditions seen in 100 years. Regardless, the excellent stability and low noise level of the instrument meant that small flares (A and B class) were able to generate statistically significant findings. The elements mapped will include Magnesium, Silicon and Aluminium, as well as relevant elemental ratios. These will be compared to other datasets including Lunar Prospector, Clementine and M3 mineral maps.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/5048797','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/5048797"><span id="translatedtitle">Coleman <span class="hlt">Highlands</span> subsurface air utilization study. Final report</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Shapiro, M.D.</p> <p>1982-11-15</p> <p>An investigation was conducted into the feasibility of using a 1 million square foot developed cave within the Downtown Industrial Park as a heating and cooling source for a proposed residential subdivision on an adjacent vacant tract of land. Both sites are located near the Coleman <span class="hlt">Highlands</span> neighborhood in the Westport Community of Kansas City, Missouri. Characteristics of the cave and surface sites were studied, as well as potential heating and cooling sources and transfer media. BTU capacity of the cave and demand for the prototype houses was calculated. The preferred system included a water source in the cave, water transfer medium, and water-to-air heat pumps in the individual homes. Analysis of that system showed it would be marginally effective due to the limited heat valve available in the cave and substantial shortfalls of cooling capacity for summertime operation. Estimated system costs appeared to be in an affordable range, but it was felt that those capital costs could be better applied to other energy-conserving measures.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/1297176','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/1297176"><span id="translatedtitle">Rift Valley fever epizootic in the central <span class="hlt">highlands</span> of Madagascar.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Morvan, J; Rollin, P E; Laventure, S; Rakotoarivony, I; Roux, J</p> <p>1992-01-01</p> <p>Between February and April 1991, unusual numbers of bovine abortion around Antananarivo (central <span class="hlt">highlands</span>, Madagascar) were reported by official veterinary services. Rift Valley fever (RVF) virus isolations were made from sixteen aborted foetuses and one dead calf in different foci. Using monoclonal antibodies, the isolated viruses were found to be different from the 1979 RVF strains isolated in Madagascar from mosquitoes and human laboratory infection, and closer to African RVF strains. In a bovine population--previously characterized by a negative or very low RVF antibody prevalence--a high prevalence of IgM antibodies (264/994: 26.5% positive) was revealed; the IgM prevalence in recently aborting females varied from 40 to 91%. Among 994 human sera tested by IgG-IFA (immunofluorescent antibody assay) and IgM ELISA, 8.2% and 4.5%, respectively, proved positive. A total of 11,371 mosquitoes (61% Culex antennatus) were collected in the epizootic areas and tested without any virus isolation. Extensive studies were conducted to determine the geographical extension and the impact of this epidemic on the highly susceptible livestock and human populations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/7845274','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/7845274"><span id="translatedtitle">Family characteristics of suicides in Cameron <span class="hlt">Highlands</span>: a controlled study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Maniam, T</p> <p>1994-09-01</p> <p>Cameron <span class="hlt">Highlands</span> has one of the highest suicide rates in the world, especially among Indians. Forty Indian families (19 suicides; 21 controls) were studied to compare family characteristics such as income, overcrowding, birth order of index cases of suicide, family history of suicidal behaviour or mental illness, marital disharmony, presence of alcohol abuse, availability of, and knowledge about, weedicides/insecticides, talk/threat of suicide among family members and experience of significant losses in the past year. Controls were matched for age, sex and educational level with the index cases of suicide. A significant difference was only found for one of the above factors, namely increased experience of significant losses in the past year in the family of index cases of suicide. More than 75% in both groups had alcohol related problems. About equal proportions in each group had a family history of suicidal behaviour and mental illness. There was more marital disharmony in families of suicides but this failed to reach significance. These results and methodological limitations of this study are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1817506D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1817506D"><span id="translatedtitle">Long-term landscape evolution of the southeast Brazilian <span class="hlt">highlands</span>: comparison of two alkaline intrusions areas</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Doranti Tiritan, Carolina; Hackspacher, Peter Christian; Glasmacher, Ulrich Anton</p> <p>2016-04-01</p> <p>The southeast Brazilian <span class="hlt">highlands</span> records a long history of tectonic and magmatic events that were consequence of the South Atlantic Ocean opening. After the rifting process has ceased, an epeirogenic uplift of the continental crust has started in response to the drifting of the South American Platform over a thermal anomaly that accompanied an intense alkaline and basaltic magmatism. Related Late Cretaceous alkaline intrusions are distributed from the southeast Brazilian coast to the interior of the South American Platform. The landscape evolution is associated with several distinct exhumation events at the South American passive continental margin (Hackspacher 2004; Doranti et al, 2014). The present study intent providing insights on the behaviour of the coupled magmatic tectonic-erosional system, comparing thermochronological data from two alkaline intrusions, Poços de Caldas Alkaline Massif (PCAM) and São Sebastião Island (SSI). The PCAM is the biggest alkaline structure located in the interior of the continent, 300km from the coastline (Rio de Janeiro). The structure is formed as a caldera, covering over 800km2, intruding Precambrian basement around 83Ma, nepheline syenites, phonolites and tinguaites intruded in a continuous and rapid sequence lasting between 1 to 2 Ma. Meanwhile, the SSI (236km²) is located at the coast, 200 km southeast of the city of São Paulo and is characterized by an intrusion in Precambrian granitic-gnaissic rocks affected by the Panafrican/Brazilian Orogen. This crystalline basement is intruded by Early Cretaceous subalkaline basic and acid dykes, as well as by Late Cretaceous alkaline stocks (syenites) and dykes (basanite to phonolite). The Apatite Fission-Track ages for PCAM range from 333.3±27.6 to 94.0±13.7 Ma at the surrounded metamorphic basement area, and 76.8±10.9 to 48.7±10.7 Ma in the alkaline Massif. The older ages, are concentrated on the lower topography region (700 until 1200m) in the north side alkaline massif</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.water.usgs.gov/wri99-4087/','USGSPUBS'); return false;" href="http://pubs.water.usgs.gov/wri99-4087/"><span id="translatedtitle">Characterization and simulation of the quantity and quality of water in the <span class="hlt">Highland</span> Lakes, Texas, 1983-92</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Raines, Timothy H.; Rast, Walter</p> <p>1999-01-01</p> <p>Results from the simulations indicate that saline inflows to the <span class="hlt">Highland</span> Lakes similar to those of the releases from Natural Dam Salt Lake during 1987–89 are unlikely to cause large increases in future concentrations of dissolved solids, chloride, and sulfate in the <span class="hlt">Highland</span> Lakes. The results also indicate that high-salinity water will continue to be diluted as it is transported downstream through the <span class="hlt">Highland</span> Lakes, even during extended dry periods.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-01-26/pdf/2011-1619.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-01-26/pdf/2011-1619.pdf"><span id="translatedtitle">76 FR 4725 - Apria Healthcare Customer Service Department; Fourteen Locations in Missouri Cameron, <span class="hlt">Cape</span>...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-01-26</p> <p>... St. Peters, Missouri. The notice was published in the Federal Register on September 3, 2010 (75 FR... Missouri Cameron, <span class="hlt">Cape</span> Girardeau, Columbia, Farmington, Fenton, Joplin, Lee's Summit, Pleasant Valley... Healthcare, Customer Service Department, Thirteen Locations in Missouri: Cameron, <span class="hlt">Cape</span> Girardeau,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20873187','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20873187"><span id="translatedtitle">[Capabilities of the application of the perspective technique during the medical supply of the outfits in <span class="hlt">highlands</span>].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Belevitin, A B; Shelepov, A M; Soldatov, E A; Shurupov, D A</p> <p>2010-07-01</p> <p>During the organization of the medical evacuation of the outfits in <span class="hlt">highlands</span> it is necessary to consider that the workability of the stretchermen in <span class="hlt">highland</span> goes down to 50% and more; equipment of the aid man must corresponds to the conditions of the <span class="hlt">highlands</span> (immobilize vacuum mattress--IVMv-01, collapsible immobilize pinion stretchers--IPS-01); application of the wheel-type machines and helicopters is difficult and dangerously. Application of the modern techniques of informational support, unmanned drones and others modern techniques requires the output of new organization principles of the system of the medical evacuation in <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/20873187','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/20873187"><span id="translatedtitle">[Capabilities of the application of the perspective technique during the medical supply of the outfits in <span class="hlt">highlands</span>].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Belevitin, A B; Shelepov, A M; Soldatov, E A; Shurupov, D A</p> <p>2010-07-01</p> <p>During the organization of the medical evacuation of the outfits in <span class="hlt">highlands</span> it is necessary to consider that the workability of the stretchermen in <span class="hlt">highland</span> goes down to 50% and more; equipment of the aid man must corresponds to the conditions of the <span class="hlt">highlands</span> (immobilize vacuum mattress--IVMv-01, collapsible immobilize pinion stretchers--IPS-01); application of the wheel-type machines and helicopters is difficult and dangerously. Application of the modern techniques of informational support, unmanned drones and others modern techniques requires the output of new organization principles of the system of the medical evacuation in <span class="hlt">highlands</span>. PMID:20873187</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/27498855','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/27498855"><span id="translatedtitle">MtDNA analysis reveals enriched pathogenic mutations in Tibetan <span class="hlt">highlanders</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kang, Longli; Zheng, Hong-Xiang; Zhang, Menghan; Yan, Shi; Li, Lei; Liu, Lijun; Liu, Kai; Hu, Kang; Chen, Feng; Ma, Lifeng; Qin, Zhendong; Wang, Yi; Wang, Xiaofeng; Jin, Li</p> <p>2016-01-01</p> <p>Tibetan <span class="hlt">highlanders</span>, including Tibetans, Monpas, Lhobas, Dengs and Sherpas, are considered highly adaptive to severe hypoxic environments. Mitochondrial DNA (mtDNA) might be important in hypoxia adaptation given its role in coding core subunits of oxidative phosphorylation. In this study, we employed 549 complete <span class="hlt">highlander</span> mtDNA sequences (including 432 random samples) to obtain a comprehensive view of <span class="hlt">highlander</span> mtDNA profile. In the phylogeny of a total of 36,914 sequences, we identified 21 major haplogroups representing founding events of <span class="hlt">highlanders</span>, most of which were coalesced in 10 kya. Through founder analysis, we proposed a three-phase model of colonizing the plateau, i.e., pre-LGM Time (30 kya, 4.68%), post-LGM Paleolithic Time (16.8 kya, 29.31%) and Neolithic Time (after 8 kya, 66.01% in total). We observed that pathogenic mutations occurred far more frequently in 22 <span class="hlt">highlander</span>-specific lineages (five lineages carrying two pathogenic mutations and six carrying one) than in the 6,857 haplogroups of all the 36,914 sequences (P = 4.87 × 10(-8)). Furthermore, the number of possible pathogenic mutations carried by <span class="hlt">highlanders</span> (in average 3.18 ± 1.27) were significantly higher than that in controls (2.82 ± 1.40) (P = 1.89 × 10(-4)). Considering that function-altering and pathogenic mutations are enriched in <span class="hlt">highlanders</span>, we therefore hypothesize that they may have played a role in hypoxia adaptation. PMID:27498855</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016E%26PSL.441...60M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016E%26PSL.441...60M"><span id="translatedtitle">Formation of Australian continental margin <span class="hlt">highlands</span> driven by plate-mantle interaction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Müller, R. Dietmar; Flament, Nicolas; Matthews, Kara J.; Williams, Simon E.; Gurnis, Michael</p> <p>2016-05-01</p> <p>Passive margin <span class="hlt">highlands</span> occur on most continents on Earth and play a critical role in the cycle of weathering, erosion, and atmospheric circulation. Yet, in contrast to the well-developed understanding of collisional mountain belts, such as the Alps and Himalayas, the origin of less elevated (1-2 km) passive margin <span class="hlt">highlands</span> is still unknown. The eastern Australian <span class="hlt">highlands</span> are a prime example of these plateaus, but compared to others they have a well-documented episodic uplift history spanning 120 million years. We use a series of mantle convection models to show that the time-dependent interaction of plate motion with mantle downwellings and upwellings accounts for the broad pattern of margin uplift phases. Initial dynamic uplift of 400-600 m from 120-80 Ma was driven by the eastward motion of eastern Australia's margin away from the sinking eastern Gondwana slab, followed by tectonic quiescence to about 60 Ma in the south (Snowy Mountains). Renewed uplift of ∼700 m in the Snowy Mountains is propelled by the gradual motion of the margin over the edge of the large Pacific mantle upwelling. In contrast the northernmost portion of the <span class="hlt">highlands</span> records continuous uplift from 120 Ma to present-day totalling about 800 m. The northern <span class="hlt">highlands</span> experienced a continuous history of dynamic uplift, first due to the end of subduction to the east of Australia, then due to moving over a large passive mantle upwelling. In contrast, the southern <span class="hlt">highlands</span> started interacting with the edge of the large Pacific mantle upwelling ∼ 40- 50 million years later, resulting in a two-phase uplift history. Our results are in agreement with published uplift models derived from river profiles and the Cretaceous sediment influx into the Ceduna sub-basin offshore southeast Australia, reflecting the fundamental link between dynamic uplift, fluvial erosion and depositional pulses in basins distal to passive margin <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4976311','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4976311"><span id="translatedtitle">MtDNA analysis reveals enriched pathogenic mutations in Tibetan <span class="hlt">highlanders</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kang, Longli; Zheng, Hong-Xiang; Zhang, Menghan; Yan, Shi; Li, Lei; Liu, Lijun; Liu, Kai; Hu, Kang; Chen, Feng; Ma, Lifeng; Qin, Zhendong; Wang, Yi; Wang, Xiaofeng; Jin, Li</p> <p>2016-01-01</p> <p>Tibetan <span class="hlt">highlanders</span>, including Tibetans, Monpas, Lhobas, Dengs and Sherpas, are considered highly adaptive to severe hypoxic environments. Mitochondrial DNA (mtDNA) might be important in hypoxia adaptation given its role in coding core subunits of oxidative phosphorylation. In this study, we employed 549 complete <span class="hlt">highlander</span> mtDNA sequences (including 432 random samples) to obtain a comprehensive view of <span class="hlt">highlander</span> mtDNA profile. In the phylogeny of a total of 36,914 sequences, we identified 21 major haplogroups representing founding events of <span class="hlt">highlanders</span>, most of which were coalesced in 10 kya. Through founder analysis, we proposed a three-phase model of colonizing the plateau, i.e., pre-LGM Time (30 kya, 4.68%), post-LGM Paleolithic Time (16.8 kya, 29.31%) and Neolithic Time (after 8 kya, 66.01% in total). We observed that pathogenic mutations occurred far more frequently in 22 <span class="hlt">highlander</span>-specific lineages (five lineages carrying two pathogenic mutations and six carrying one) than in the 6,857 haplogroups of all the 36,914 sequences (P = 4.87 × 10−8). Furthermore, the number of possible pathogenic mutations carried by <span class="hlt">highlanders</span> (in average 3.18 ± 1.27) were significantly higher than that in controls (2.82 ± 1.40) (P = 1.89 × 10−4). Considering that function-altering and pathogenic mutations are enriched in <span class="hlt">highlanders</span>, we therefore hypothesize that they may have played a role in hypoxia adaptation. PMID:27498855</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title46-vol1/pdf/CFR-2012-title46-vol1-sec7-60.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title46-vol1/pdf/CFR-2012-title46-vol1-sec7-60.pdf"><span id="translatedtitle">46 CFR 7.60 - <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-10-01</p> <p>... 46 Shipping 1 2012-10-01 2012-10-01 false <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. 7.60 Section 7.60... Atlantic Coast § 7.60 <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. (a) A line drawn from the southernmost extremity to <span class="hlt">Cape</span> Fear to latitude 33°49.5′ N. longitude 78°03.7′ W. (<span class="hlt">Cape</span> Fear River Entrance Lighted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title46-vol1/pdf/CFR-2011-title46-vol1-sec7-60.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title46-vol1/pdf/CFR-2011-title46-vol1-sec7-60.pdf"><span id="translatedtitle">46 CFR 7.60 - <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-10-01</p> <p>... 46 Shipping 1 2011-10-01 2011-10-01 false <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. 7.60 Section 7.60... Atlantic Coast § 7.60 <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. (a) A line drawn from the southernmost extremity to <span class="hlt">Cape</span> Fear to latitude 33°49.5′ N. longitude 78°03.7′ W. (<span class="hlt">Cape</span> Fear River Entrance Lighted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title46-vol1/pdf/CFR-2010-title46-vol1-sec7-60.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title46-vol1/pdf/CFR-2010-title46-vol1-sec7-60.pdf"><span id="translatedtitle">46 CFR 7.60 - <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-10-01</p> <p>... 46 Shipping 1 2010-10-01 2010-10-01 false <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. 7.60 Section 7.60... Atlantic Coast § 7.60 <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. (a) A line drawn from the southernmost extremity to <span class="hlt">Cape</span> Fear to latitude 33°49.5′ N. longitude 78°03.7′ W. (<span class="hlt">Cape</span> Fear River Entrance Lighted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title46-vol1/pdf/CFR-2013-title46-vol1-sec7-60.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title46-vol1/pdf/CFR-2013-title46-vol1-sec7-60.pdf"><span id="translatedtitle">46 CFR 7.60 - <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-10-01</p> <p>... 46 Shipping 1 2013-10-01 2013-10-01 false <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. 7.60 Section 7.60... Atlantic Coast § 7.60 <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. (a) A line drawn from the southernmost extremity to <span class="hlt">Cape</span> Fear to latitude 33°49.5′ N. longitude 78°03.7′ W. (<span class="hlt">Cape</span> Fear River Entrance Lighted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title46-vol1/pdf/CFR-2014-title46-vol1-sec7-60.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title46-vol1/pdf/CFR-2014-title46-vol1-sec7-60.pdf"><span id="translatedtitle">46 CFR 7.60 - <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-10-01</p> <p>... 46 Shipping 1 2014-10-01 2014-10-01 false <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. 7.60 Section 7.60... Atlantic Coast § 7.60 <span class="hlt">Cape</span> Fear, NC to Sullivans Island, SC. (a) A line drawn from the southernmost extremity to <span class="hlt">Cape</span> Fear to latitude 33°49.5′ N. longitude 78°03.7′ W. (<span class="hlt">Cape</span> Fear River Entrance Lighted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-03-08/pdf/2010-4926.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-03-08/pdf/2010-4926.pdf"><span id="translatedtitle">75 FR 10500 - Environmental Assessment Prepared for Proposed <span class="hlt">Cape</span> Wind Energy Project in Nantucket Sound, MA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-03-08</p> <p>... Minerals Management Service Environmental Assessment Prepared for Proposed <span class="hlt">Cape</span> Wind Energy Project in... review and comment of an EA and Draft FONNSI prepared by MMS for the <span class="hlt">Cape</span> Wind Energy Project proposed... Environmental Impact Statement (FEIS) for the <span class="hlt">Cape</span> Wind Energy Project. The FEIS assessed the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-11-15/pdf/2010-28710.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-11-15/pdf/2010-28710.pdf"><span id="translatedtitle">75 FR 69700 - Final Environmental Impact Statement and <span class="hlt">Cape</span> Hatteras National Seashore Off-Road Vehicle...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-11-15</p> <p>... National Park Service Final Environmental Impact Statement and <span class="hlt">Cape</span> Hatteras National Seashore Off-Road... Environmental Impact Statement for the <span class="hlt">Cape</span> Hatteras National Seashore Off-Road Vehicle Management Plan. SUMMARY... <span class="hlt">Cape</span> Hatteras National Seashore (Seashore) Off-Road Vehicle Management Plan (Plan/ FEIS). The...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-11-06/pdf/2013-26515.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-11-06/pdf/2013-26515.pdf"><span id="translatedtitle">78 FR 66763 - Notice of December 2, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-11-06</p> <p>... National Park Service Notice of December 2, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory... the date of the 291st Meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The public meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on Monday, December 2, 2013,...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-03-06/pdf/2013-05180.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-03-06/pdf/2013-05180.pdf"><span id="translatedtitle">78 FR 14588 - Notice of March 25, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-03-06</p> <p>... National Park Service Notice of March 25, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission... of the Two Hundred Eighty- Eighth Meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The public meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-10-01/pdf/2012-24126.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-10-01/pdf/2012-24126.pdf"><span id="translatedtitle">77 FR 59970 - Notice of November 14, 2012, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-10-01</p> <p>... National Park Service Notice of November 14, 2012, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory... the date of the Two Hundred Eighty- Sixth Meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The public meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-04-22/pdf/2013-09334.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-04-22/pdf/2013-09334.pdf"><span id="translatedtitle">78 FR 23783 - Notice of May 13, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-04-22</p> <p>... National Park Service Notice of May 13, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission... of the Two Hundred Eighty- Ninth Meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission. DATES: The public meeting of the <span class="hlt">Cape</span> Cod National Seashore Advisory Commission will be held on Monday,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-04/pdf/2010-10486.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-04/pdf/2010-10486.pdf"><span id="translatedtitle">75 FR 23798 - Environmental Assessment Prepared for Proposed <span class="hlt">Cape</span> Wind Energy Project in Nantucket Sound...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-04</p> <p>... Minerals Management Service Environmental Assessment Prepared for Proposed <span class="hlt">Cape</span> Wind Energy Project in...), announces the availability of an EA and FONNSI for the <span class="hlt">Cape</span> Wind Energy Project proposed for Nantucket Sound... Impact Statement (FEIS) for the <span class="hlt">Cape</span> Wind Energy Project. The FEIS assessed the physical, biological,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec167-250.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec167-250.pdf"><span id="translatedtitle">33 CFR 167.250 - In the approaches to the <span class="hlt">Cape</span> Fear River: General.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: General. 167.250 Section 167.250 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF... <span class="hlt">Cape</span> Fear River: General. The traffic separation scheme (TSS) in the approaches to the <span class="hlt">Cape</span> Fear...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-530.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-530.pdf"><span id="translatedtitle">33 CFR 80.530 - <span class="hlt">Cape</span> Fear, NC to Little River Inlet, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false <span class="hlt">Cape</span> Fear, NC to Little River... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.530 <span class="hlt">Cape</span> Fear, NC to... latitude 33°52.4′ N., longitude 78°00.1′ W., across the <span class="hlt">Cape</span> Fear River Entrance to Oak Island Light....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-530.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-530.pdf"><span id="translatedtitle">33 CFR 80.530 - <span class="hlt">Cape</span> Fear, NC to Little River Inlet, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> Fear, NC to Little River... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.530 <span class="hlt">Cape</span> Fear, NC to... latitude 33°52.4′ N. longitude 78°00.1′ W. across the <span class="hlt">Cape</span> Fear River Entrance to Oak Island Light....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-530.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-530.pdf"><span id="translatedtitle">33 CFR 80.530 - <span class="hlt">Cape</span> Fear, NC to Little River Inlet, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false <span class="hlt">Cape</span> Fear, NC to Little River... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.530 <span class="hlt">Cape</span> Fear, NC to... latitude 33°52.4′ N. longitude 78°00.1′ W. across the <span class="hlt">Cape</span> Fear River Entrance to Oak Island Light....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-01-10/pdf/2012-172.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-01-10/pdf/2012-172.pdf"><span id="translatedtitle">77 FR 1406 - Drawbridge Operation Regulations; Northeast <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-01-10</p> <p>... SECURITY Coast Guard 33 CFR Part 117 Drawbridge Operation Regulations; Northeast <span class="hlt">Cape</span> Fear River... operation of the Isabel S. Holmes Bridge, mile 1.0, across the Northeast <span class="hlt">Cape</span> Fear River, at Wilmington, NC... Northeast <span class="hlt">Cape</span> Fear River. The drawbridge will be able to open in the event of an emergency. The Coast...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-515.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-515.pdf"><span id="translatedtitle">33 CFR 165.515 - Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear River... § 165.515 Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. (a) Location. The following area is a safety zone: (1) The waters of the <span class="hlt">Cape</span> Fear River bounded by a line connecting the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-515.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-515.pdf"><span id="translatedtitle">33 CFR 165.515 - Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear River... § 165.515 Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. (a) Location. The following area is a safety zone: (1) The waters of the <span class="hlt">Cape</span> Fear River bounded by a line connecting the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-250.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-250.pdf"><span id="translatedtitle">33 CFR 167.250 - In the approaches to the <span class="hlt">Cape</span> Fear River: General.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: General. 167.250 Section 167.250 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF... <span class="hlt">Cape</span> Fear River: General. The traffic separation scheme (TSS) in the approaches to the <span class="hlt">Cape</span> Fear...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-10-08/pdf/2010-25380.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-10-08/pdf/2010-25380.pdf"><span id="translatedtitle">75 FR 62320 - Safety Zone; Fireworks for USS GRAVELY Commissioning Ceremony, <span class="hlt">Cape</span> Fear River, Wilmington, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-10-08</p> <p>... Ceremony, <span class="hlt">Cape</span> Fear River, Wilmington, NC AGENCY: Coast Guard, DHS. ACTION: Temporary final rule. SUMMARY: The Coast Guard is establishing a safety zone on the navigable waters of <span class="hlt">Cape</span> Fear River in Wilmington... fireworks display on the western shore of the <span class="hlt">Cape</span> Fear River at Battleship Park. The fireworks...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec167-250.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec167-250.pdf"><span id="translatedtitle">33 CFR 167.250 - In the approaches to the <span class="hlt">Cape</span> Fear River: General.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: General. 167.250 Section 167.250 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF... <span class="hlt">Cape</span> Fear River: General. The traffic separation scheme (TSS) in the approaches to the <span class="hlt">Cape</span> Fear...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-515.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-515.pdf"><span id="translatedtitle">33 CFR 165.515 - Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear River... § 165.515 Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. (a) Location. The following area is a safety zone: (1) The waters of the <span class="hlt">Cape</span> Fear River bounded by a line connecting the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-530.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-530.pdf"><span id="translatedtitle">33 CFR 80.530 - <span class="hlt">Cape</span> Fear, NC to Little River Inlet, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false <span class="hlt">Cape</span> Fear, NC to Little River... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.530 <span class="hlt">Cape</span> Fear, NC to... latitude 33°52.4′ N. longitude 78°00.1′ W. across the <span class="hlt">Cape</span> Fear River Entrance to Oak Island Light....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-530.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-530.pdf"><span id="translatedtitle">33 CFR 80.530 - <span class="hlt">Cape</span> Fear, NC to Little River Inlet, NC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false <span class="hlt">Cape</span> Fear, NC to Little River... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Fifth District § 80.530 <span class="hlt">Cape</span> Fear, NC to... latitude 33°52.4′ N., longitude 78°00.1′ W., across the <span class="hlt">Cape</span> Fear River Entrance to Oak Island Light....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-515.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-515.pdf"><span id="translatedtitle">33 CFR 165.515 - Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear River... § 165.515 Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. (a) Location. The following area is a safety zone: (1) The waters of the <span class="hlt">Cape</span> Fear River bounded by a line connecting the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-515.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-515.pdf"><span id="translatedtitle">33 CFR 165.515 - Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2010-07-01 2010-07-01 false Safety Zone: <span class="hlt">Cape</span> Fear River... § 165.515 Safety Zone: <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. (a) Location. The following area is a safety zone: (1) The waters of the <span class="hlt">Cape</span> Fear River bounded by a line connecting the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec167-250.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec167-250.pdf"><span id="translatedtitle">33 CFR 167.250 - In the approaches to the <span class="hlt">Cape</span> Fear River: General.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: General. 167.250 Section 167.250 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF... <span class="hlt">Cape</span> Fear River: General. The traffic separation scheme (TSS) in the approaches to the <span class="hlt">Cape</span> Fear...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED189236','ERIC'); return false;" href="http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED189236"><span id="translatedtitle"><span class="hlt">Cape</span> Verdeans in the United States (Continuing a Story of Struggle, Creativity and Persistence).</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Houston, Laura Pires</p> <p></p> <p>This article focuses on the history of the <span class="hlt">Cape</span> Verde Islands, the nature of <span class="hlt">Cape</span> Verdean immigration to the United States, and the ethnic experience of <span class="hlt">Cape</span> Verdeans in the U.S. The colonization of the Atlantic archipelago by the Portuguese as part of their expanding slave trade is described and the Islands' economic, ecologic, racial and…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED183469','ERIC'); return false;" href="http://eric.ed.gov/?q=Cape+AND+Verde&pg=2&id=ED183469"><span id="translatedtitle">Nho Lobo: Folk Tales of the <span class="hlt">Cape</span> Verdean People. Teacher's Guide.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Nyhan, Patricia; Almeida, Raymond A.</p> <p></p> <p>The teacher's guide presents two <span class="hlt">Cape</span> Verdean folktales, background information, discussion questions, and activity suggestions for grades 4-6. The objective is to teach students about <span class="hlt">Cape</span> Verde and its culture through folklore. The guide contains five sections. Section I offers a description of <span class="hlt">Cape</span> Verdean folklore, describes five ways folklore…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70036695','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70036695"><span id="translatedtitle">Strategic analysis for the MER <span class="hlt">Cape</span> Verde approach</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Gaines, D.; Belluta, P.; Herman, J.; Hwang, P.; Mukai, R.; Porter, D.; Jones, B.; Wood, E.; Grotzinger, J.; Edgar, L.; Hayes, A.; Hare, T.; Squyres, S.</p> <p>2009-01-01</p> <p>The Mars Exploration Rover Opportunity has recently completed a two year campaign studying Victoria Crater. The campaign culminated in a close approach of <span class="hlt">Cape</span> Verde in order to acquire high resolution imagery of the exposed stratigraphy in the cliff face. The close approach to <span class="hlt">Cape</span> Verde provided significant challenges for every subsystem of the rover as the rover needed to traverse difficult, uncharacterised terrain and approach a cliff face with the potential of blocking out solar energy and communications with Earth. In this paper we describe the strategic analyses performed by the science and engineering teams so that we could successfully achieve the science objectives while keeping the rover safe. ??2009 IEEE.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=20150008662&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=20150008662&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DCape%2BVerde"><span id="translatedtitle">Strategic Analysis for the MER <span class="hlt">Cape</span> Verde Approach</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gaines, Daniel; Belluta, Paolo; Herman, Jennifer; Hwang, Pauline; Mukai, Ryan; Porter, Dan; Jones, Byron; Wood, Eric; Grotzinger, John; Edgar, Lauren; Hayes, Alex; Hare, Trent; Squyres, Steve</p> <p>2009-01-01</p> <p>The Mars Exploration Rover Opportunity has recently completed a two year campaign studying Victoria Crater. The campaign culminated in a close approach of <span class="hlt">Cape</span> Verde in order to acquire high resolution imagery of the exposed stratigraphy in the cliff face. The close approach to <span class="hlt">Cape</span> Verde provided significant challenges for every subsystem of the rover as the rover needed to traverse difficult, uncharacterised terrain and approach a cliff face with the potential of blocking out solar energy and communications with Earth. In this paper we describe the strategic analyses performed by the science and engineering teams so that we could successfully achieve the science objectives while keeping the rover safe.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/43659','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/43659"><span id="translatedtitle">Hydrologic overlay maps of the <span class="hlt">Cape</span> Canaveral Quadrangle, Florida</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Frazee, James M.; Laughlin, Charles P.</p> <p>1979-01-01</p> <p>Brevard County is an area of some 1,300 square miles located on the east coast of central Florida.  The <span class="hlt">Cape</span> Canaveral quadrangle, in central Brevard, includes part of the Merritt Island National Wildlife Refuge, John F. Kennedy Space Center (NASA), and <span class="hlt">Cape</span> Canaveral Air Force Station.  The eastern part of the quadrangle is occupied by the Atlantic Ocean and the western part by estuarine waters of the Banana River.  Topography is characterized by numerous elongate sand dumes, with altitudes up to 10 feet or greater, which roughly parallel the estuary and ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1727878','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1727878"><span id="translatedtitle">Gallstone disease in Peruvian coastal natives and <span class="hlt">highland</span> migrants</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Moro, P; Checkley, W; Gilman, R; Cabrera, L; Lescano, A; Bonilla, J; Silva, B</p> <p>2000-01-01</p> <p>BACKGROUND—In a previous study, we found that gallstones were a common occurrence in the high altitude villages of the Peruvian Andes.
AIMS—To determine if high altitude (⩾ 1500 m) is a contributing risk factor for gallstone disease.
METHODS—We conducted a cross sectional study in a periurban community in Lima, Peru, and compared the prevalence of gallstone disease between coastal natives, <span class="hlt">highland</span> (Sierra) natives and Sierra natives who had migrated to the coast. We also compared the prevalence rates from this study with those from a previous study conducted at high altitude. We examined 1534 subjects >15 years of age for gallstone disease. Subjects were interviewed for the presence or absence of risk factors.
RESULTS—Gallstone disease was more common in females (16.1 cases per 100, 95% CI 13.8-18.2) than in males (10.7 per 100, 95% CI 8.0-13.4). Females had a greater risk of gallstone disease, especially if they had used oral contraception and/or had four or more children. The age adjusted prevalence was not significantly different between coastal natives, Sierra migrants, and Andean villagers. The prevalence of gallstone disease was not associated with time since migration or with having native Sierra parents. After adjusting for other risk factors, Sierra natives who migrated to the coast had a lower prevalence of gallstone disease than coastal natives (odds ratio 0.74, 95% CI 0.58-0.94).
CONCLUSIONS—This study indicates that high altitude is not a positive risk factor for gallstone disease and confirms that this disease is common in Peruvians, which may be attributable to Peruvian-Indian ethnicity.


Keywords: gallstone disease; cholelithiasis; high altitude; risk factors; epidemiology; Peru PMID:10716689</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=20090014123&hterms=Anorthosite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DAnorthosite','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=20090014123&hterms=Anorthosite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D80%26Ntt%3DAnorthosite"><span id="translatedtitle">The LHT (Lunar <span class="hlt">Highlands</span> Type) Regolith Simulant Series</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Stoeser, Douglas; Wilson, Steve; Weinstein, Michael; Rickman, Douglas; Lowers, Heather; Meeker, Gregory; Schrader, Christian; McLemore, Carole; Fikes, John</p> <p>2008-01-01</p> <p>Three NU-LHT (NASA/USGS-Lunar <span class="hlt">Highlands</span> Type) regolith simulants have been produced to date: NU-LHT-1M, -ID, and -2M. A fourth simulant is currently in production: NU-LHT-3C. The "M" (medium) designation indicates a simulant with a grain size of <1 mm, "D" (dust) a simulant with a grain size of <36 microns, and "C" (coarse) a simulant with a 10 cm maximum particle size. The composition of these simulants is based on a NASA average Apollo 16 regolith chemical composition, However, the mixing model used to create our simulants is based on cationic nonnative mineral proportions derived from the target chemical composition to approximate lunar modal mineralogy rather than chemical composition per se. Accordingly, the amount of plagioclase, pyroxenes, olivine, and trace minerals in the simulant crystalline fraction approximates that of the lunar regolith. We also added synthetic agglutinate in amounts approximate for low-medium regolith maturity. A pure glass fraction was also added to simulate other types of lunar glasses present in the regolith. In addition, the 3C simulant will include synthetic impact melt breccia clasts for the >1 cm particles. The bulk raw materials used to create these simulants include clinopyroxene-norite, anorthosite, hartzburgite and noritic mill waste from the Stillwater Mine, Nye, MT, and olivine from the Twin Sisters dunite, WA. Added trace minerals include beach sand ilmenite, chromite, synthetic p-tricaicium phosphate (whitiockite), gem grade fluor-apatite, and pyrite. The agglutinate, glasses, and synthetic breccia were designed and prepared at an industrial plasma melting facility in Boulder, CO, using Stillwater mill waste feedstock for the melt. These simulants do not include nanophase-feO. The M and C simulant grain size distribution (down to 0.4 microns) approximates that of Apollo 16 regolith and the regolith in general.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3928908','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3928908"><span id="translatedtitle"><span class="hlt">Highland</span> cattle and Radix labiata, the hosts of Fascioloides magna</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2014-01-01</p> <p>Background Fascioloides magna is a pathogenic fluke introduced to Europe ca 140 years ago. As it is spreading over the continent, new intermediate and definitive hosts might be involved in transmission of the parasite. In Europe, several studies reported potential new intermediate snail hosts (Radix spp.) for F. magna, and also several cases of fascioloidosis of wild and domestic animals were published. However, the data based on molecular and histological analyses confirming these findings remained unreported. This study aims to refer to unique findings of F. magna in European snails and domestic animals (the first observation in the Czech Republic in the last 30 years) and demonstrate the use of molecular techniques in determination of F. magna. Results Two snails of R. labiata naturally infected with F. magna were found; mature cercariae and daughter rediae were observed. Maturity of cercariae was checked by histological methods, however, their ability to encyst was not confirmed. Co-infection of F. magna and Fasciola hepatica in the liver of two <span class="hlt">highland</span> cattle bulls was proved. Adult fasciolid flukes producing eggs were found in the liver pseudocysts (F. magna) and the bile ducts (F. hepatica). Identification of intermediate hosts, intramolluscan stages, adult flukes and eggs was performed by sequencing the ITS2 region. Connection of F. magna pseudocysts with the gut (via the bile ducts) was not confirmed by means of histological and coprological examinations. Conclusions For the first time, Radix labiata was confirmed as the snail host for F. magna under natural conditions and, together with the finding of F. magna infection in cattle, we can expect further transmission of F. magna from wildlife to livestock in localities shared by these hosts. PMID:24517409</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2778131','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2778131"><span id="translatedtitle">Ranking Malaria Risk Factors to Guide Malaria Control Efforts in African <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Protopopoff, Natacha; Van Bortel, Wim; Speybroeck, Niko; Van Geertruyden, Jean-Pierre; Baza, Dismas; D'Alessandro, Umberto; Coosemans, Marc</p> <p>2009-01-01</p> <p>Introduction Malaria is re-emerging in most of the African <span class="hlt">highlands</span> exposing the non immune population to deadly epidemics. A better understanding of the factors impacting transmission in the <span class="hlt">highlands</span> is crucial to improve well targeted malaria control strategies. Methods and Findings A conceptual model of potential malaria risk factors in the <span class="hlt">highlands</span> was built based on the available literature. Furthermore, the relative importance of these factors on malaria can be estimated through “classification and regression trees”, an unexploited statistical method in the malaria field. This CART method was used to analyse the malaria risk factors in the Burundi <span class="hlt">highlands</span>. The results showed that Anopheles density was the best predictor for high malaria prevalence. Then lower rainfall, no vector control, higher minimum temperature and houses near breeding sites were associated by order of importance to higher Anopheles density. Conclusions In Burundi <span class="hlt">highlands</span> monitoring Anopheles densities when rainfall is low may be able to predict epidemics. The conceptual model combined with the CART analysis is a decision support tool that could provide an important contribution toward the prevention and control of malaria by identifying major risk factors. PMID:19946627</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26631558','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26631558"><span id="translatedtitle">Temperature and population density determine reservoir regions of seasonal persistence in <span class="hlt">highland</span> malaria.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Siraj, Amir S; Bouma, Menno J; Santos-Vega, Mauricio; Yeshiwondim, Asnakew K; Rothman, Dale S; Yadeta, Damtew; Sutton, Paul C; Pascual, Mercedes</p> <p>2015-12-01</p> <p>A better understanding of malaria persistence in highly seasonal environments such as <span class="hlt">highlands</span> and desert fringes requires identifying the factors behind the spatial reservoir of the pathogen in the low season. In these 'unstable' malaria regions, such reservoirs play a critical role by allowing persistence during the low transmission season and therefore, between seasonal outbreaks. In the <span class="hlt">highlands</span> of East Africa, the most populated epidemic regions in Africa, temperature is expected to be intimately connected to where in space the disease is able to persist because of pronounced altitudinal gradients. Here, we explore other environmental and demographic factors that may contribute to malaria's <span class="hlt">highland</span> reservoir. We use an extensive spatio-temporal dataset of confirmed monthly Plasmodium falciparum cases from 1995 to 2005 that finely resolves space in an Ethiopian <span class="hlt">highland</span>. With a Bayesian approach for parameter estimation and a generalized linear mixed model that includes a spatially structured random effect, we demonstrate that population density is important to disease persistence during the low transmission season. This population effect is not accounted for in typical models for the transmission dynamics of the disease, but is consistent in part with a more complex functional form of the force of infection proposed by theory for vector-borne infections, only during the low season as we discuss. As malaria risk usually decreases in more urban environments with increased human densities, the opposite counterintuitive finding identifies novel control targets during the low transmission season in African <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-12-17/pdf/2012-30317.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-12-17/pdf/2012-30317.pdf"><span id="translatedtitle">77 FR 74694 - Notice of January 14, 2013, Meeting for <span class="hlt">Cape</span> Cod National Seashore Advisory Commission</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-12-17</p> <p>... Wetland Restoration Wind Turbines/Cell Towers Shorebird Management Planning <span class="hlt">Highlands</span> Center Update... superintendent prior to the meeting. Before including your address, phone number, email address, or...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JVGR..298...27M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JVGR..298...27M"><span id="translatedtitle"><span class="hlt">Cape</span> Wanbrow: A stack of Surtseyan-style volcanoes built over millions of years in the Waiareka-Deborah volcanic field, New Zealand</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Moorhouse, B. L.; White, J. D. L.; Scott, J. M.</p> <p>2015-06-01</p> <p>Volcanic fields typically include many small, monogenetic, volcanoes formed by single eruptions fed by short-lived magma plumbing systems that solidify after eruption. The <span class="hlt">Cape</span> Wanbrow coastline of the northeast Otago region in the South Island of New Zealand exposes an Eocene-Oligocene intraplate basaltic field that erupted in Surtseyan style onto a submerged continental shelf, and the stratigraphy of <span class="hlt">Cape</span> Wanbrow suggests that eruptions produced multiple volcanoes whose edifices overlapped within a small area, but separated by millions of years. The small <span class="hlt">Cape</span> Wanbrow <span class="hlt">highland</span> is shown to include the remains of 6 volcanoes that are distinguished by discordant to locally concordant inter-volcano contacts marked by biogenic accumulations or other slow-formed features. The 6 volcanoes contain several lithofacies associations: (a) the dominantly pyroclastic E1 comprising well-bedded tuff and lapilli-tuff, emplaced by traction-dominated unsteady, turbulent high-density currents; (b) E2, massive to diffusely laminated block-rich tuff deposited by grain-dominant cohesionless debris flows; (c) E3, broadly cross-stratified tuff with local lenses of low- to high-angle cross-stratification which was deposited by either subaerial pyroclastic currents or subaqueously by unstable antidune- and chute-and-pool-forming supercritical flows; (d) E4, very-fine- to medium-grained tuff deposited by turbidity currents; (e) E5, bedded bioclast-rich tuff with increasing glaucony content upward, emplaced by debris flows; (f) E6, pillow lava and inter-pillow bioclastic sediment; and (g) E7, hyaloclastite breccia. These lithofacies associations aid interpretation of the eruptive evolution of each separate volcano, which in turn grew and degraded during build-up of the overall volcanic pile. Sedimentary processes played a prominent role in the evolution of the volcanic pile with both syn- and post-eruptive re-mobilization of debris from the growing pile of primary pyroclastic deposits of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016LPICo1926.6053H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016LPICo1926.6053H"><span id="translatedtitle">Massive Late Noachian South Polar/Southern Upland Ice Deposits: Predictions and Tests of the Late Noachian "Cold and Icy <span class="hlt">Highlands</span>" Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Head, J. W.</p> <p>2016-09-01</p> <p>New Noachian climate models predict a "cold and icy <span class="hlt">highlands</span>": glacial ice dominates the southern <span class="hlt">highlands</span> around a huge south polar ice deposit. We document the predicted nature of these polar/circumpolar deposits and test it with observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20050179462','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20050179462"><span id="translatedtitle">Pervasive Layering in the Lunar <span class="hlt">Highland</span> Crust: Evidence from Apollos 15, 16,and 17</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lowman, Paul D., Jr.; Yang, Tiffany</p> <p>2005-01-01</p> <p>This paper presents results of a photogeologic reconnaissance of 70 mm photographs taken on the lunar surface during the Apollo 15, 16, and 17 missions, whose primary objective was to investigate the lunar <span class="hlt">highland</span> crust. Photographs at all three sites, notably the Apennine Front, show pervasive layered structure. These layers are easily distinguished from lighting artifacts, and are considered genuine crustal structures. Their number, thickness, and extent implies that they are lava flows, not ejecta blankets or intrusive features. They appear to be the upper part of the earliest lunar crust, possibly forming a layer tens of kilometers thick. Remote sensing studies (X-ray fluorescence and reflectance spectroscopy), indicate that the <span class="hlt">highland</span> crust is dominantly a feldspathic basalt. It is concluded that the <span class="hlt">highland</span> layers represent a global crust formed by eruptions of high-alumina basalt in the first few hundred million years of the Moon's history.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940017194','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940017194"><span id="translatedtitle">The early Martian environment: Clues from the cratered <span class="hlt">highlands</span> and the Precambrian Earth</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Craddock, R. A.; Maxwell, T. A.</p> <p>1993-01-01</p> <p>There is abundant geomorphic evidence to suggest that Mars once had a much denser and warmer atmosphere than present today. Outflow channel, ancient valley networks, and degraded impact craters in the <span class="hlt">highlands</span> all suggest that ancient Martian atmospheric conditions supported liquid water on the surface. The pressure, composition, and duration of this atmosphere is largely unknown. However, we have attempted to place some constraints on the nature of the early Martian atmosphere by analyzing morphologic variations of <span class="hlt">highland</span> impact crater populations, synthesizing results of other investigators, and incorporating what is know about the geologic history of the early Earth. This is important for understanding the climatic evolution of Mars, the relative abundance of martian volatiles, and the nature of <span class="hlt">highland</span> surface materials.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.T43A4677A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.T43A4677A"><span id="translatedtitle">GPS Constraints on the Spatial Distribution of Extension in the Ethiopian <span class="hlt">Highlands</span> and Main Ethiopian Rift</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Amere, Y. B.; Bendick, R. O.; Fisseha, S.; Lewi, E.; Reilinger, R. E.; King, R. W.; Kianji, G.</p> <p>2014-12-01</p> <p>27 campaign and 17 continuous GPS sites spanning the Ethiopian <span class="hlt">Highlands</span>, Main Ethiopian Rift (MER), and Somali Platform in Ethiopia and Eritrea were measured for varying durations between 1995 and 2014. Velocities at these sites show that present day strain in NE Africa is not localized only in the Afar depression and MER system. Rather, velocities as high as 6 mm/yr relative to stable Nubia occur in the central Ethiopian <span class="hlt">highlands</span> west of the rift bounding faults; the northern and southern Ethiopian <span class="hlt">highlands</span> host velocities as high as 3 mm/yr. These approach the magnitude of Nubia-Somalia spreading accommodated within the rift itself of 6 + 1 mm/yr with an azimuth of N770E. The combination of distributed low strain rate deformation contiguous with higher strain rate plate boundary deformation is similar to that expressed in other tectonically active continental settings like Basin and Range and Tibetan Plateau.Keywords: deformation, localized, distributed, strain, stable Nubia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/12296236','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/12296236"><span id="translatedtitle">Female spirit cults as a window on gender relations in the <span class="hlt">highlands</span> of Papua New Guinea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stewart, P J; Strathern, A</p> <p>1999-09-01</p> <p>Early writings on male cults in the <span class="hlt">highlands</span> of Papua New Guinea tended to stress the exclusion of women and the collective agency of men. Looking at a subset of these cults from the Western and Southern <span class="hlt">Highlands</span> Provinces, centering on Female Spirit figures, the authors argue that in these cases the cults are better understood as expressions of a collaborative model, in which gendered cooperation, both in practice and in terms of ritual symbolism, is activated in order to produce fertility and wealth. Positive collaboration is involved as well as structural complementarity. The collaborative model is therefore suggested as an alternative to the model of "male exclusivity" in the analysis of certain cult practices in these parts of the New Guinea <span class="hlt">highlands</span> region. PMID:12296236</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.water.usgs.gov/wri85-4252','USGSPUBS'); return false;" href="http://pubs.water.usgs.gov/wri85-4252"><span id="translatedtitle">Preliminary evaluation of the <span class="hlt">Highland</span> Rim aquifer system in Tennessee for receiving injected wastes</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Bradley, M.W.</p> <p>1986-01-01</p> <p>The EPA has authority under the Safe Drinking Water Act to protect underground sources of drinking water from contamination by deep well injection. An aquifer, however, may be exempted from protection and used for injected wastes where the aquifer meets criteria established in the Agency 's Underground Injection Control program. The <span class="hlt">Highland</span> Rim aquifer system in Tennessee consists of Mississippian age carbonate rocks and occurs from the Valley and Ridge of East Tennessee to west of the Tennessee River. This aquifer contains potable water and is an important source of drinking water for municipal and domestic supplies on the <span class="hlt">Highland</span> Rim. The <span class="hlt">Highland</span> Rim aquifer system under parts of the Cumberland Plateau is not currently used as a source of drinking water and is not expected to be used in the future. These areas meet parts of the EPA 's Underground Injection Control criteria for exempting aquifers to receive injected waste. (Author 's abstract)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/wri/2000/4000/pdf/wrir2000-4000.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/wri/2000/4000/pdf/wrir2000-4000.pdf"><span id="translatedtitle">Delineation of groundwater recharge areas, western <span class="hlt">Cape</span> Cod, Massachusetts</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Masterson, John P.; Walter, Donald A.</p> <p>2000-01-01</p> <p>For additional information on the hydrology and geology of western <span class="hlt">Cape</span> Cod, the reader is referred to the following reports: LeBlanc and others (1986), Barlow and Hess (1993), Masterson and others (1997a), Masterson and others (1997b), Masterson and others (1998), Ogden Environmental and Energy Services, Inc. (1998) and Jacobs Engineering Group, Inc. (1999).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://acwi.gov/sos/pubs/2ndJFIC/Contents/5C_Boudreau_02_25_10_paper.pdf','USGSPUBS'); return false;" href="http://acwi.gov/sos/pubs/2ndJFIC/Contents/5C_Boudreau_02_25_10_paper.pdf"><span id="translatedtitle">Sediment transport on <span class="hlt">Cape</span> Sable, Everglades National Park, Florida</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Zucker, Mark; Boudreau, Carrie</p> <p>2010-01-01</p> <p>The <span class="hlt">Cape</span> Sable peninsula is located on the southwestern tip of the Florida peninsula within Everglades National Park (ENP). Lake Ingraham, the largest lake within <span class="hlt">Cape</span> Sable, is now connected to the Gulf of Mexico and western Florida Bay by canals built in the early 1920's. Some of these canals breached a natural marl ridge located to the north of Lake Ingraham. These connections altered the landscape of this area allowing for the transport of sediments to and from Lake Ingraham. Saline intrusion into the formerly fresh interior marsh has impacted the local ecology. Earthen dams installed in the 1950's and 1960's in canals that breached the marl ridge have repeatedly failed. Sheet pile dams installed in the early 1990's subsequently failed resulting in the continued alteration of Lake Ingraham and the interior marsh. The <span class="hlt">Cape</span> Sable Canals Dam Restoration Project, funded by ENP, proposes to restore the two failed dams in Lake Ingraham. The objective of this study was to collect discharge and water quality data over a series of tidal cycles and flow conditions to establish discharge and sediment surrogate relations prior to initiating the <span class="hlt">Cape</span> Sable Canals Dam Restoration Project. A dry season synoptic sampling event was performed on April 27-30, 2009.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec117-829.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec117-829.pdf"><span id="translatedtitle">33 CFR 117.829 - Northeast <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false Northeast <span class="hlt">Cape</span> Fear River. 117... Fear River. (a) The draw of the Isabel S. Holmes Bridge, at mile 1.0, at Wilmington, North Carolina... Fear River. (2) The draw shall be left in the open position to vessels and will only be closed for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec117-829.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec117-829.pdf"><span id="translatedtitle">33 CFR 117.829 - Northeast <span class="hlt">Cape</span> Fear River.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false Northeast <span class="hlt">Cape</span> Fear River. 117... Fear River. (a) The draw of the Isabel S. Holmes Bridge, at mile 1.0, at Wilmington, North Carolina... Fear River. (2) The draw shall be left in the open position to vessels and will only be closed for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Cape+AND+Verde&id=EJ277513','ERIC'); return false;" href="http://eric.ed.gov/?q=Cape+AND+Verde&id=EJ277513"><span id="translatedtitle">The Politics of an Emancipatory Literacy in <span class="hlt">Cape</span> Verde.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Macedo, Donaldo P.</p> <p>1983-01-01</p> <p>Examines the literacy program in <span class="hlt">Cape</span> Verde against theories of cultural production and reproduction. Argues that the use of Portuguese rather than the Capeverdean dialect reproduces a colonial, elitist mentality, and that functional literacy in Portuguese fails to provide Capeverdeans with opportunities for critical reflection and social…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2013EGUGA..1512209M&link_type=ABSTRACT','NASAADS'); return false;" href="http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2013EGUGA..1512209M&link_type=ABSTRACT"><span id="translatedtitle">Source Apportionment of Particulate Matter Sampled in <span class="hlt">Cape</span> Verde</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Marta Almeida, Susana; Almeida-Silva, Marina; Pio, Casimiro; Nunes, Teresa; Cardoso, João; Cerqueira, Mário; Reis, Miguel; Chaves, Paula Cristina; Taborda, Ana</p> <p>2013-04-01</p> <p>Due to its geographical position, <span class="hlt">Cape</span> Verde is highly affected by the transport of dust from the Sahara desert. Consequently, very high concentrations of particles are registered in this archipelago, being essential to elucidate the role that Saharan dust may play in the degradation of <span class="hlt">Cape</span> Verde air quality, human health, wellbeing, visibility, tourism and economy. The objective of this study was to identify the main sources and origins of particles sampled in <span class="hlt">Cape</span> Verde. PM10 was sampled during 2011 and chemical characterization of particles was performed by Neutron Activation Analysis and Particle Induced X-ray Emission for elemental measurements, by Ion Chromatography for the determination of water soluble ions and by a Thermal-optical system for the measurement of carbonaceous aerosol. Source apportionment was performed by integrating Positive Matrix Factorization and Backward Trajectory Analysis. Results showed that in average 68% of the PM10 mass in <span class="hlt">Cape</span> Verde had a natural origin, being 48% associated with the soil and 20% associated with the sea. During the transport of dust from the Sahara desert the contribution of mineral aerosol increased significantly (69% during periods affected by trajectories provided from Sahara desert versus 13% during periods affected by local sources).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/15005896','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/15005896"><span id="translatedtitle">Long-Term Changes in Soil Carbon under Different Fertilizer, Manure, and Rotation: Testing the Mathematical Model ecosys with Data from the <span class="hlt">Breton</span> Plots</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Grant, R F.; Juma, N G.; Robertson, J A.; Izaurralde, R Cesar C. ); Mcgill, William B.</p> <p>2001-01-01</p> <p>Soil C contents can be raised by land use practices in which rates of C input exceed those of C oxidation. Rates of C inputs of soil can be raised by continuous cropping, especially with perennial legumes, and by soil amendments, especially manure. We have summarized our understanding of the processes by which changes in soil C content are determined by rates of soil C input in the mathematical model ecosys. We compared model output for changes in soil C with those measured in a Gray Luvisol (Typic Cryboralf) at <span class="hlt">Breton</span>, Alberta, during 70 yr of a 2-yr wheat (Triticum aestivum L.)-fallow rotation vs. a 5-yr wheat-oat (Avena sativa L.)-barley (Hordeum vulgare L.)-forage-forage rotation with unamended, fertilized, and manured treatments. Model results indicated that rates of C input in the 2-yr rotation were inadequate to maintain soil C in the upper 0.15 m of the soil profile unless manure was added, but that those in the 5-yr rotation were more than adequate. Consequent changes of soil C in the model were corroborated by declines of 14 and 7 g C m-2 yr-1 measured in the control and fertilized treatments of the 2-yr rotation; by gains of 7 g C m-2 yr-1 measured in the manured treatment of the 2-yr rotation; and by gains of 4, 14, an d28 g C m-2 yr-1 measured in the control, fertilized, and manured treatments of the 5-yr rotation. Model results indicated that soil C below 0.15 m declined in all treatments of both rotations, but more so in the 2-yr than in the 5-yr rotation. These declines were corroborated by lower soil C contents measured between 0.15 and 0.40 m after 70 yr in the 2- vs. 5-yr rotation. Land use practices that favor C storage appear to interact positively with each other, so that gains in soil C under one such practice are greater when it is combined with other such practices.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=race+AND+bottom&pg=5&id=ED331940','ERIC'); return false;" href="http://eric.ed.gov/?q=race+AND+bottom&pg=5&id=ED331940"><span id="translatedtitle"><span class="hlt">Highlander</span> Folk School and the Labor Movement, 1932-1953. The Relationship between Education and Social Movements.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Zacharakis-Jutz, Jeff</p> <p></p> <p>The mission of the <span class="hlt">Highlander</span> Folk School (Tennessee), which flourished between 1932 and 1961, was intimately intertwined with the labor movement of the 1930s and 1940s and the civil rights movement of the 1950s and 1960s. <span class="hlt">Highlander</span> began as an Appalachian community school seeking to understand the issues and problems of the community it served.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-09-30/pdf/2011-25244.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-09-30/pdf/2011-25244.pdf"><span id="translatedtitle">76 FR 60935 - Notice of Application from ExxonMobil Corporation, <span class="hlt">Highland</span> Uranium Mine and Millsite, To Amend...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-09-30</p> <p>... accordance with the NRC E-Filing rule (72 FR 49139, August 28, 2007). The E-Filing process requires... COMMISSION Notice of Application from ExxonMobil Corporation, <span class="hlt">Highland</span> Uranium Mine and Millsite, To Amend... concentration limits and to extend the NRC Long-Term Surveillance Boundary at its <span class="hlt">Highland</span> Uranium Mine and...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16382176','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16382176"><span id="translatedtitle">Role of vagal activity on bradicardic and hypotensive effects of caffeic acid phenethyl ester (<span class="hlt">CAPE</span>).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Iraz, Mustafa; Fadillioglu, Ersin; Tasdemir, Seda; Erdogan, Selim</p> <p>2005-01-01</p> <p>Caffeic acid phenethyl ester (<span class="hlt">CAPE</span>) is a phenolic active component of propolis of honeybee hives and reduces heart rate and blood pressure in rats. The objective of this study was to investigate the role of vagal activity and atropine blockage on the bradycardic and hypotensive effects of <span class="hlt">CAPE</span> in rats. The rats were divided into five groups (n = 8). Saline and vehicle (10% ethanol) of <span class="hlt">CAPE</span> were given to the first and second groups, respectively. Group 3 was treated with 5 mg/kg <span class="hlt">CAPE</span>. Group 4 bivagotomized and treated with 5 mg/kg <span class="hlt">CAPE</span>. Group 5 treated with atropine (5 microg/microL/min) continuously and treated with <span class="hlt">CAPE</span>. The electrophysiological monitoring was done for each experiment under urethane anesthetize. As a result, <span class="hlt">CAPE</span> caused intense and transient bradycardia and hypotension. Vagotomy completely abolished bradycardia occurred via <span class="hlt">CAPE</span> injection; however atropine attenuated bradycardic effects of <span class="hlt">CAPE</span>. On the other hand, hypotensive effect of <span class="hlt">CAPE</span> was affected from neither bilateral vagotomy nor atropine treatment. It was thought that <span class="hlt">CAPE</span> may exert its effects on heart rate via a central parasympathetic control mechanism, but not on central parasympathetic blood pressure control system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/22934065','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/22934065"><span id="translatedtitle">Malaria in East African <span class="hlt">highlands</span> during the past 30 years: impact of environmental changes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Himeidan, Yousif E; Kweka, Eliningaya J</p> <p>2012-01-01</p> <p>East African <span class="hlt">highlands</span> are one of the most populated regions in Africa. The population densities in the <span class="hlt">highlands</span> ranged between 158 persons/km(2) in Ethiopia and 410 persons/km(2) in Rwanda. According to the United Nations Population Fund, the region has the world's highest population growth rate. These factors are likely behind the high rates of poverty among the populations. As there were no employment opportunities other than agricultural, this demographic pressure of poor populations have included in an extensive unprecedented land use and land cover changes such as modification of bushland, woodland, and grassland on hillsides to farmland and transformation of papyrus swamps in valley bottoms to dairy pastures and cropland and changing of fallows on hillsides from short or seasonal to longer or perennial. Areas harvested for food crops were therefore increased by more than 100% in most of the <span class="hlt">highlands</span>. The lost of forest areas, mainly due to subsistence agriculture, between 1990 and 2010 ranged between 8000 ha in Rwanda and 2,838,000 ha in Ethiopia. These unmitigated environmental changes in the <span class="hlt">highlands</span> led to rise temperature and optimizing the spread and survival of malaria vectors and development of malaria parasites. Malaria in <span class="hlt">highlands</span> was initially governed by low ambient temperature, trend of malaria transmission was therefore increased and several epidemics were observed in late 1980s and early 2000s. Although, malaria is decreasing through intensified interventions since mid 2000s onwards, these environmental changes might expose population in the <span class="hlt">highlands</span> of east Africa to an increase risk of malaria and its epidemic particularly if the current interventions are not sustained. PMID:22934065</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3429085','PMC'); return false;" href="http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3429085"><span id="translatedtitle">Malaria in East African <span class="hlt">highlands</span> during the past 30 years: impact of environmental changes</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Himeidan, Yousif E.; Kweka, Eliningaya J.</p> <p>2012-01-01</p> <p>East African <span class="hlt">highlands</span> are one of the most populated regions in Africa. The population densities in the <span class="hlt">highlands</span> ranged between 158 persons/km2 in Ethiopia and 410 persons/km2 in Rwanda. According to the United Nations Population Fund, the region has the world's highest population growth rate. These factors are likely behind the high rates of poverty among the populations. As there were no employment opportunities other than agricultural, this demographic pressure of poor populations have included in an extensive unprecedented land use and land cover changes such as modification of bushland, woodland, and grassland on hillsides to farmland and transformation of papyrus swamps in valley bottoms to dairy pastures and cropland and changing of fallows on hillsides from short or seasonal to longer or perennial. Areas harvested for food crops were therefore increased by more than 100% in most of the <span class="hlt">highlands</span>. The lost of forest areas, mainly due to subsistence agriculture, between 1990 and 2010 ranged between 8000 ha in Rwanda and 2,838,000 ha in Ethiopia. These unmitigated environmental changes in the <span class="hlt">highlands</span> led to rise temperature and optimizing the spread and survival of malaria vectors and development of malaria parasites. Malaria in <span class="hlt">highlands</span> was initially governed by low ambient temperature, trend of malaria transmission was therefore increased and several epidemics were observed in late 1980s and early 2000s. Although, malaria is decreasing through intensified interventions since mid 2000s onwards, these environmental changes might expose population in the <span class="hlt">highlands</span> of east Africa to an increase risk of malaria and its epidemic particularly if the current interventions are not sustained. PMID:22934065</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA04960&hterms=1890s&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3D1890s','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA04960&hterms=1890s&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3D1890s"><span id="translatedtitle"><span class="hlt">Cape</span> Town, South Africa, Anaglyph, Landsat Image over SRTM Elevation</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2004-01-01</p> <p><p/> <span class="hlt">Cape</span> Town and the <span class="hlt">Cape</span> of Good Hope, South Africa, appear on the left (west) of this anaglyph view generated from a Landsat satellite image and elevation data from the Shuttle Radar Topography Mission (SRTM). The city center is located between Table Bay (upper left) and Table Mountain (just to the south), a 1,086-meter (3,563-foot) tall sandstone and granite natural landmark. <p/> <span class="hlt">Cape</span> Town enjoys a Mediterranean climate but must deal with the limited water supply characteristic of that climate. Until the 1890s the city relied upon streams and springs along the base of Table Mountain, then built a small reservoir atop Table Mountain to capture and store rainfall there (visible in this anaglyph when viewed at full resolution). Now the needs of a much larger population are met in part by much larger reservoirs such as seen well inland (upper right) at the Theewaterskloof Dam. <p/> False Bay is the large bay to the southeast (lower right) of <span class="hlt">Cape</span> Town, just around the <span class="hlt">Cape</span> of Good Hope. It is one of the largest bays along the entire South African coast, but nearby <span class="hlt">Cape</span> Town has its harbor at Table Bay. False Bay got its name because mariners approaching <span class="hlt">Cape</span> Town from the east would see the prominent bay and falsely assume it to be the entrance to <span class="hlt">Cape</span> Town harbor. Similarly, people often mistake the <span class="hlt">Cape</span> of Good Hope as the southernmost point of Africa. But the southernmost point is actually <span class="hlt">Cape</span> Agulhas, located just to the southeast (lower right) of this scene. <p/> This anaglyph was created by draping a Landsat visible light image over an SRTM elevation model, and then generating two differing perspectives, one for each eye. When viewed through special glasses, the anaglyph is a vertically exaggerated view of the Earth's surface in its full three dimensions. Anaglyph glasses cover the left eye with a red filter and cover the right eye with a blue filter. <p/> Elevation data used in this image was acquired by the Shuttle Radar Topography Mission (SRTM) aboard</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19840004991','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19840004991"><span id="translatedtitle">Workshop on Pristine <span class="hlt">Highlands</span> Rocks and the early History of the Moon</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Longhi, J. (Editor); Ryder, G. (Editor)</p> <p>1983-01-01</p> <p>Oxide composition of the Moon, evidence for an initially totally molten Moon, geophysical contraints on lunar composition, random sampling of a layered intrusion, lunar <span class="hlt">highland</span> rocks, early evolution of the Moon, mineralogy and petrology of the pristine rocks, relationship of the pristine nonmore rocks to the <span class="hlt">highlands</span> soils and breccias, ferroan anorthositic norite, early lunar igneous history, compositional variation in ferroan anosthosites, a lunar magma ocean, deposits of lunar pristine rocks, lunar and planetary compositions and early fractionation in the solar nebula, Moon composition models, petrogenesis in a Moon with a chondritic refractory lithophile pattern, a terrestrial analog of lunar ilmenite bearing camulates, and the lunar magma ocean are summarized.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19910042964&hterms=magnet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DTitle%26N%3D0%26No%3D70%26Ntt%3Dmagnet','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19910042964&hterms=magnet&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DTitle%26N%3D0%26No%3D70%26Ntt%3Dmagnet"><span id="translatedtitle">Magnetic beneficiation of <span class="hlt">highland</span> and hi-Ti mare soils - Magnet requirements</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Oder, R. R.; Taylor, L. A.</p> <p>1990-01-01</p> <p>Magnetic beneficiation of immature <span class="hlt">highland</span> soil 67511 recovered 22 wt pct of the sample with an iron oxide content of 0.6 pct. Magnetic isolates of immature <span class="hlt">highland</span> soils are candidates for the manufacture of silicon, aluminum, and other metals. Fifty-seven percent of the ilmenite in immature mare soil 71061 was recovered in magnetic processing. Ilmenite can be recovered by magnetic separation but may be difficult to 'high'grade'. A parametric description is given of magnetic separators suitable for supplying ilmenite for the production of 22.7 metric tons per year oxygen.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/prof/p1565c/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/prof/p1565c/"><span id="translatedtitle">Geochemistry and stratigraphic relations of middle Proterozoic rocks of the New Jersey <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Volkert, Richard A.; Drake, Avery Ala</p> <p>1999-01-01</p> <p>Middle Proterozoic rocks of the New Jersey <span class="hlt">Highlands</span> consist of a basement of dacitic, tonalitic, trondhjemitic, and charnockitic rocks that constitute the Losee metamorphic suite. These rocks are unconformably overlain by a layered supracrustal sequence of quartzo-feldspathic and calcareous rocks. Abundant sheets of hornblende- and biotite-bearing rocks of the Byram intrusive suite and clinopyroxene-bearing rocks of the Lake Hopatcong intrusive suite were synkinematically emplaced at about 1,090 Ma. These intrusive suites constitute the Vernon Supersuite. The postorogenic Mount Eve Granite has been dated at 1,020?4 Ma and is confined to the extreme northern <span class="hlt">Highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.8506W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.8506W"><span id="translatedtitle">IN and CCN Measurements on RV Polarstern and <span class="hlt">Cape</span> Verde</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Welti, André; Herenz, Paul; Henning, Silvia; Stratmann, Frank</p> <p>2016-04-01</p> <p>Two field campaigns, one situated on RV Polarstern (Oct. - Dec. 2015) and one on the <span class="hlt">Cape</span> Verde islands (Jan. - Feb. 2016) measuring ice nuclei (IN) and cloud condensation nuclei (CCN) concentrations as a function of supersaturation and temperature are presented. The Polarstern cruise from Bremerhaven to <span class="hlt">Cape</span> Town yields a cross section of IN and CCN concentrations from 54°N to 35°S and passes the <span class="hlt">Cape</span> Verde Islands at 15°N. Measurements were conducted using the commercial CCNC and SPIN instruments from DMT. During both campaigns, a comprehensive set of aerosol characterization data including size distribution, optical properties and chemical information were measured in parallel. The ship based measurements provide a measure of variability in IN/CCN concentration with geographic position. As an example a clear influence on IN and CCN number concentration of the Saharan desert dust outflow between the Canary Islands and <span class="hlt">Cape</span> Verde or the continental aerosol from Europe and South Africa was observed. The measurements on <span class="hlt">Cape</span> Verde provide information on the temporal variability at a fixed position varying between clean marine and dust influenced conditions. Both datasets are related to auxiliary data of aerosol size distribution and chemical composition. The datasets are used to distinguish the influence of local sources and background concentration of IN/CCN. By combining of the geographically fix measurements with the geographical cross section, typical ranges of IN and CCN concentration are derived. The datasets will be part of the BACCHUS database thereby providing valuable input for future climate modeling activities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11770206','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11770206"><span id="translatedtitle">Village poultry production systems in the central <span class="hlt">highlands</span> of Ethiopia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dessie, T; Ogle, B</p> <p>2001-12-01</p> <p>Participatory rural appraisal (PRA), supported by checklists and intensive case studies on individual households, was carried out in three villages at three different altitudes in the central <span class="hlt">highlands</span> of Ethiopia. The chicken production system in each village is described and the problems are discussed. More than 60% of the families kept chickens, and in most cases the women owned and managed the birds and controlled the cash from the sales. The production systems followed were mainly low-input and small-scale, with 7-10 mature birds per household, reared in the back yards with inadequate housing, feeding and health care. The average egg production per clutch was 15-20, with 3-4 clutches per year. The mean number of eggs set per bird was 12.9 +/- 2.2 (n = 160), depending on the size of the bird and season, and the hatching rate was 80.9% +/- 11.1%, range 44%-100% (n = 160). Poultry meat and eggs were generally accepted and appreciated in all three villages. In addition to the small amount of cash income they provide, scavenging chickens have nutritional, cultural and social functions. The flock composition, price of poultry and poultry products, disease outbreaks and hatching of chicks were strongly affected by season. Disease was cited as the most important problem by most of the members of the community, followed by predation, lack of feed, poor housing, insufficient water and parasites. Disease periodically decimated the flocks, and consequently, about 50% of the eggs produced were incubated in order to replace the birds that had died. The major source of loss in the system was the high mortality of chicks (61%) that occurred between hatching and the end of brooding at 8 weeks of age. The system was characterized by no or few inputs and a low output level. The major input was the cost of foundation stock, but after that virtually no cost was involved. The major source of feed for the birds was from the scavenging feed resource base, which comprised table</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-06-16/pdf/2010-14469.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-06-16/pdf/2010-14469.pdf"><span id="translatedtitle">75 FR 33999 - Safety Zone; Fourth of July Fireworks Event, <span class="hlt">Cape</span> Charles City Harbor, <span class="hlt">Cape</span> Charles, VA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-06-16</p> <p>... Coast Guard is establishing a 420-foot radius safety zone on the navigable waters of <span class="hlt">Cape</span> Charles City..., vessel traffic will be temporarily restricted within 420 feet of the fireworks launch site. Discussion of... Harbor within the area bounded by a 420-foot radius circle centered on position 37 15'59'' N/ 076...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED137152.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED137152.pdf"><span id="translatedtitle"><span class="hlt">Cape</span> Verde and Its People: A Short History, Part I [And] Folk Tales of the <span class="hlt">Cape</span> Verdean People.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Almeida, Raymond A.; Nyhan, Patricia</p> <p></p> <p>Two booklets provide an overview of the history and folklore of <span class="hlt">Cape</span> Verde, a group of islands lying 370 miles off the west coast of Africa. One booklet describes the history of the islands which were probably settled initially by Africans from the west coast of Africa. By the 15th century the islands were colonized by Portuguese and other…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-540.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-540.pdf"><span id="translatedtitle">33 CFR 165.540 - Regulated Navigation Area; <span class="hlt">Cape</span> Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... Commandant to command the Captain of the Port Zone as described in 33 CFR 3.25-20. Control vessel means the... CFR 160.207 are encouraged to notify the COTP at least 48-hours before the vessel enters the RNA to... Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. 165.540 Section 165.540...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-540.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-540.pdf"><span id="translatedtitle">33 CFR 165.540 - Regulated Navigation Area; <span class="hlt">Cape</span> Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... Commandant to command the Captain of the Port Zone as described in 33 CFR 3.25-20. Control vessel means the... CFR 160.207 are encouraged to notify the COTP at least 48-hours before the vessel enters the RNA to... Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. 165.540 Section 165.540...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-540.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-540.pdf"><span id="translatedtitle">33 CFR 165.540 - Regulated Navigation Area; <span class="hlt">Cape</span> Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... Commandant to command the Captain of the Port Zone as described in 33 CFR 3.25-20. Control vessel means the... CFR 160.207 are encouraged to notify the COTP at least 48-hours before the vessel enters the RNA to... Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. 165.540 Section 165.540...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-540.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-540.pdf"><span id="translatedtitle">33 CFR 165.540 - Regulated Navigation Area; <span class="hlt">Cape</span> Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... Commandant to command the Captain of the Port Zone as described in 33 CFR 3.25-20. Control vessel means the... CFR 160.207 are encouraged to notify the COTP at least 48-hours before the vessel enters the RNA to... Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. 165.540 Section 165.540...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-540.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-540.pdf"><span id="translatedtitle">33 CFR 165.540 - Regulated Navigation Area; <span class="hlt">Cape</span> Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... Commandant to command the Captain of the Port Zone as described in 33 CFR 3.25-20. Control vessel means the... CFR 160.207 are encouraged to notify the COTP at least 48-hours before the vessel enters the RNA to... Fear River, Northeast <span class="hlt">Cape</span> Fear River, Wilmington, North Carolina. 165.540 Section 165.540...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=PIA11048&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=PIA11048&hterms=Cape+Verde&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCape%2BVerde"><span id="translatedtitle">Dusk Lighting of Layered Textures in '<span class="hlt">Cape</span> Verde'</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2008-01-01</p> <p><p/> Full-shade lighting in the late Martian afternoon helps make details visible in this view of the layered cliff face of the '<span class="hlt">Cape</span> Verde' promontory making up part of the rim of Victoria Crater in the Meridiani Planum region of equatorial Mars. <p/> NASA's Mars Exploration Rover Opportunity used its panoramic camera (Pancam) to shoot the dozens of individual images that have been combined into this mosaic. Opportunity was inside Victoria Crater and near the base of the cliff when it took these images on the 1,579th and 1,580th Martian days, or sols, of the mission (July 2 and 3, 2008). <p/> Photographing the promontory from this position in Victoria Crater presented challenges for the rover team. The geometry was such that <span class="hlt">Cape</span> Verde was between the rover and the sun, which could cause a range of negative effects, from glinting off Pancam's dusty lenses to shadowing on the cliff face. The team's solution was to take the images for this mosaic just after the sun disappeared behind the crater rim, at about 5:30 p.m. local solar time. The atmosphere was still lit, but no direct sunlight was illuminating the wall of <span class="hlt">Cape</span> Verde. <p/> The result is a high-resolution view of <span class="hlt">Cape</span> Verde in relatively uniform diffuse sky lighting across the scene. <p/> Pancam used a clear filter for taking the images for this mosaic. Capturing images in low-light situations was one of the main motivations for including the clear filter among the camera's assortment of filters available for use. <p/> The face of <span class="hlt">Cape</span> Verde is about 6 meters (20 feet) tall. Victoria Crater, at about 800 meters (one-half mile) wide, is the largest and deepest crater that Opportunity has visited. It sits more than 5 kilometers (almost 4 miles) away from Opportunity's Eagle Crater landing site. Researchers sent Opportunity into Victoria Crater to study the rock layers exposed inside. The textures seen in the rock layers of <span class="hlt">Cape</span> Verde suggest that the exposed layers were originally deposited by wind.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/26184141','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/26184141"><span id="translatedtitle"><span class="hlt">CAPE</span> Analogs Induce Growth Arrest and Apoptosis in Breast Cancer Cells.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Beauregard, Annie-Pier; Harquail, Jason; Lassalle-Claux, Grégoire; Belbraouet, Mehdi; Jean-Francois, Jacques; Touaibia, Mohamed; Robichaud, Gilles A</p> <p>2015-01-01</p> <p>Breast cancer is the second leading cause of death amongst women worldwide. As a result, many have turned their attention to new alternative approaches to treat this disease. Caffeic acid phenylethyl ester (<span class="hlt">CAPE</span>), a well-known active compound from bee propolis, has been previously identified as a strong antioxidant, anti-inflammatory, antiviral and anticancer molecule. In fact, <span class="hlt">CAPE</span> is well documented as inducing cell death by inhibiting NFκB and by inducing pro-apoptotic pathways (i.e., p53). With the objective of developing stronger anticancer compounds, we studied 18 recently described <span class="hlt">CAPE</span> derivatives for their ability to induce apoptosis in breast cancer cell lines. Five of the said compounds, including <span class="hlt">CAPE</span>, were selected and subsequently characterised for their anticancer mechanism of action. We validated that <span class="hlt">CAPE</span> is a potent inducer of caspase-dependent apoptosis. Interestingly, some newly synthesized <span class="hlt">CAPE</span> derivatives also showed greater cell death activity than the lead <span class="hlt">CAPE</span> structure. Similarly to <span class="hlt">CAPE</span>, analog compounds elicited p53 activation. Interestingly, one compound in particular, analog 10, induced apoptosis in a p53-mutated cell line. These results suggest that our new <span class="hlt">CAPE</span> analog compounds may display the capacity to induce breast cancer apoptosis in a p53-dependent and/or independent manner. These <span class="hlt">CAPE</span> analogs could thus provide new therapeutic approaches for patients with varying genotypic signatures (such as p53 mutations) in a more specific and targeted fashion. PMID:26184141</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=312294','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=312294"><span id="translatedtitle">Biophysical and economic assessment of a community-based rehabilitated gully in the Ethiopian <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p>In the last fifty years, sediment concentrations in the Ethiopian <span class="hlt">highlands</span> have increased two- to three-fold. The current severity of gully erosion is a major cause of increased sediment loads, but gully rehabilitation has proven to be challenging, with limited success. This paper describes gully r...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=312252','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=312252"><span id="translatedtitle">Participatory community-based gully rehabilitation on the Ethiopian <span class="hlt">Highlands</span>: the case of Birr watershed</span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p>In the last fifty years, sediment concentrations in the Ethiopian <span class="hlt">highlands</span> have increased two- to three-fold. The current severity of gully erosion is a major cause of increased sediment loads, but gully rehabilitation has proven to be challenging as success rates have been small. This paper descri...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2607295','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2607295"><span id="translatedtitle">Malaria treatment-seeking behaviour and recovery from malaria in a <span class="hlt">highland</span> area of Kenya</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Sumba, Peter O; Wong, S Lindsey; Kanzaria, Hemal K; Johnson, Kelsey A; John, Chandy C</p> <p>2008-01-01</p> <p>Background Malaria epidemics in <span class="hlt">highland</span> areas of Kenya cause significant morbidity and mortality. Methods To assess treatment-seeking behaviour for malaria in these areas, a questionnaire was administered to 117 randomly selected households in the <span class="hlt">highland</span> area of Kipsamoite, Kenya. Self-reported episodes of malaria occurred in 100 adults and 66 children. Results The most frequent initial sources of treatment for malaria in adults and children were medical facilities (66.0% and 66.7%) and local shops (19.0% and 30.3%). Adults and children who initially visited a medical facility for treatment were significantly more likely to recover and require no further treatment than those who initially went to a local shop (adults, 84.9% v. 36.8%, P < 0.0001, and children, 79.6% v. 40.0%, P = 0.002, respectively). Individuals who attended medical facilities recalled receiving anti-malarial medication significantly more frequently than those who visited shops (adults, 100% vs. 29.4%, and children, 100% v. 5.0%, respectively, both P < 0.0001). Conclusion A significant proportion of this <span class="hlt">highland</span> population chooses local shops for initial malaria treatment and receives inappropriate medication at these localshops, reslting in delay of effective treatment. Shopkeeper education has the potential to be a component of prevention or containment strategies for malaria epidemics in <span class="hlt">highland</span> areas. PMID:19036154</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3315256','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3315256"><span id="translatedtitle">Building Climate Resilience in the Blue Nile/Abay <span class="hlt">Highlands</span>: A Role for Earth System Sciences</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Zaitchik, Benjamin F.; Simane, Belay; Habib, Shahid; Anderson, Martha C.; Ozdogan, Mutlu; Foltz, Jeremy D.</p> <p>2012-01-01</p> <p>The Blue Nile (Abay) <span class="hlt">Highlands</span> of Ethiopia are characterized by significant interannual climate variability, complex topography and associated local climate contrasts, erosive rains and erodible soils, and intense land pressure due to an increasing population and an economy that is almost entirely dependent on smallholder, low-input agriculture. As a result, these <span class="hlt">highland</span> zones are highly vulnerable to negative impacts of climate variability. As patterns of variability and precipitation intensity alter under anthropogenic climate change, there is concern that this vulnerability will increase, threatening economic development and food security in the region. In order to overcome these challenges and to enhance sustainable development in the context of climate change, it is necessary to establish climate resilient development strategies that are informed by best-available Earth System Science (ESS) information. This requirement is complicated by the fact that climate projections for the Abay <span class="hlt">Highlands</span> contain significant and perhaps irreducible uncertainties. A critical challenge for ESS, then, is to generate and to communicate meaningful information for climate resilient development in the context of a highly uncertain climate forecast. Here we report on a framework for applying ESS to climate resilient development in the Abay <span class="hlt">Highlands</span>, with a focus on the challenge of reducing land degradation. PMID:22470302</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Interrogation&pg=4&id=EJ1105425','ERIC'); return false;" href="http://eric.ed.gov/?q=Interrogation&pg=4&id=EJ1105425"><span id="translatedtitle">Making Hope and History Rhyme: Reflections on Popular Education and Leadership Following a Visit to <span class="hlt">Highlander</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Connolly, Bríd; Finnegan, Fergal</p> <p>2016-01-01</p> <p>This article draws on our backgrounds as adult educators in Ireland and our experience at <span class="hlt">Highlander</span> in 2014. We review our development as critical educators, exposed to deep inequalities in Irish society. We explore role of popular education in fostering social change, beginning with the commitment to equality and freedom, whereby, we produce…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76695&keyword=health+AND+Sport&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68447660&CFTOKEN=25282162','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76695&keyword=health+AND+Sport&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68447660&CFTOKEN=25282162"><span id="translatedtitle">DECISION TOOL FOR RIPARIAN ECOSYSTEM MANAGMENT IN THE MID-ATLANTIC <span class="hlt">HIGHLANDS</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>In the Canaan Valley <span class="hlt">Highlands</span> of the Mid-Atlantic, riparian zone restoration has been identified as a critical watershed management practice not only for the ecosystem services provided but also for the potential socioeconomic growth from environmental investment and job creatio...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=desertion+AND+school&id=EJ463865','ERIC'); return false;" href="http://eric.ed.gov/?q=desertion+AND+school&id=EJ463865"><span id="translatedtitle">Economic Determinants of Academic Failure and School Desertion in the Guatemala <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Carvajal, Manuel J.; And Others</p> <p>1993-01-01</p> <p>Explores, from an economic perspective, elementary school system adequacy in the rural, indigenous Guatemalan <span class="hlt">highlands</span>. Estimates least-squares coefficients and elasticities separately for academic failure and school abandonment for each of four indigenous groups. The model explains academic failure better than school desertion. A national policy…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED470917.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED470917.pdf"><span id="translatedtitle">A Study of Service-Learning at Virginia <span class="hlt">Highlands</span> Community College and Mountain Empire Community College.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Hughes, Alice</p> <p></p> <p>This qualitative study was conducted to explore student perceptions of service learning as well as the importance of service learning to community college students. Data were collected through interviews with 24 community college participants from Virginia <span class="hlt">Highlands</span> Community College and Mountain Empire Community College, both in southwest…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=65380&keyword=total+AND+physical+AND+response&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=80525269&CFTOKEN=97425678','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=65380&keyword=total+AND+physical+AND+response&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=80525269&CFTOKEN=97425678"><span id="translatedtitle">DEVELOPMENT OF AN INDEX OF BIOTIC INTEGRITY FOR THE MID-ATLANTIC <span class="hlt">HIGHLANDS</span> REGION</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>From 1993 to 1996, fish assemblage data were collected from 309 wadeable streams in the U.S. Mid-Atlantic <span class="hlt">Highlands</span> region as part of the U.S. Environmental Protection Agency's Environmental Monitoring and Assessment Program. Stream sites were selected with a probabilistic sampl...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED494433.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED494433.pdf"><span id="translatedtitle"><span class="hlt">Highland</span> Children's Education Project: A Pilot Project on Bilingual Education in Cambodia</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Middleborg, Jorn</p> <p>2005-01-01</p> <p>The report was produced by UNESCO in partnership with CARE International in Cambodia for the "<span class="hlt">Highland</span> Children's Education Project" (HCEP) to show how bilingual primary education has been implemented among the Tampuen and Kreung ethnic minority groups in six remote villages in the northeastern province of Ratanakiri, Cambodia. Central to HCEP is…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=310709','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=310709"><span id="translatedtitle">Improving efficacy of landscape interventions in the (semi) humid Ethiopian <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p>Despite millions of dollars invested in soil and water conservation practices and other landscape interventions in Ethiopian <span class="hlt">highlands</span> and billions of hours of food-for-work farm labor, sediment concentration in rivers is increasing. Possible ways to reverse the current trend has been investigated b...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016SGC....24..381P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016SGC....24..381P"><span id="translatedtitle">Tectonostratigraphy of the Mesozoic complexes of the northwestern part of the Koryak <span class="hlt">Highland</span>, Ust' Belaya Mountains</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Palechek, T. N.; Moiseev, A. V.; Gul'pa, I. V.</p> <p>2016-07-01</p> <p>New data on the structure, age, and composition of the tectonostratigraphic complexes of the western part of the Koryak <span class="hlt">Highland</span> are presented. The conclusions on the sedimentation conditions are drawn and primary relations are interpreted for most complexes. New Kimmeridgian-Tithonian and Berriasian assemblages of radiolarians are established. Campanian radiolarians are found for the first time in the region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26933635','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26933635"><span id="translatedtitle">Response of soil respiration to experimental warming in a <span class="hlt">highland</span> barley of the Tibet.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhong, Zhi-Ming; Shen, Zhen-Xi; Fu, Gang</p> <p>2016-01-01</p> <p><span class="hlt">Highland</span> barley is an important dominant crop in the Tibet and the croplands of the Tibet are experiencing obvious climatic warming. However, information about how soil respiration will respond to climatic warming in the <span class="hlt">highland</span> barley system is still lacking. A field warming experiment using infrared heaters with two warming magnitudes was conducted in a <span class="hlt">highland</span> barley system of the Tibet in May 2014. Five daily cycles of soil respiration was measured using a CO2 flux system (Li-8100, Li-COR Biosciences, Lincoln, NE, USA) during the period from early June to early September in 2014. The high and low experimental warming significantly increased soil temperature by 1.98 and 1.52 °C over the whole study period, respectively. The high experimental warming significantly decreased soil moisture. Soil respiration and its temperature sensitivity did not significantly change under both the high and low experimental warming. The response of soil respiration to experimental warming did not linearly correlate with warming magnitudes because a greater experimental warming resulted in a higher soil drying. Our findings suggested that clarifying the response of soil CO2 production and its temperature sensitivity to climatic warming need consider water availability in the <span class="hlt">highland</span> barley system of the Tibet.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=81034&keyword=Longitude&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=78937397&CFTOKEN=29922056','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=81034&keyword=Longitude&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=78937397&CFTOKEN=29922056"><span id="translatedtitle">PREDICTION OF FUNDAMENTAL ASSEMBLAGES OF MID-ATLANTIC <span class="hlt">HIGHLAND</span> STREAM FISHES</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>A statistical software tool, the Stream Fish Assemblage Predictor (SFAP), based on stream sampling data collected by the EPA in the mid-Atlantic <span class="hlt">Highlands</span>, was developed to predict potential stream fish communities using characteristics of the stream and its watershed. <br>Step o...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76155&keyword=Longitude&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=78937397&CFTOKEN=29922056','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=76155&keyword=Longitude&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=78937397&CFTOKEN=29922056"><span id="translatedtitle">STATISTICAL TECHNIQUES FOR DETERMINATION AND PREDICTION OF FUNDAMENTAL FISH ASSEMBLAGES OF THE MID-ATLANTIC <span class="hlt">HIGHLANDS</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>A statistical software tool, Stream Fish Community Predictor (SFCP), based on EMAP stream sampling in the mid-Atlantic <span class="hlt">Highlands</span>, was developed to predict stream fish communities using stream and watershed characteristics. Step one in the tool development was a cluster analysis t...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED325570.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED325570.pdf"><span id="translatedtitle">Profiles of the <span class="hlt">Highland</span> Lao Communities in the United States. Final Report.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Yang, Doua; North, David</p> <p></p> <p>This collection of statistical data on the 90 <span class="hlt">Highland</span> Lao communities in the United States is designed to help members of those communities and people working in refugee-serving agencies to better assist this refugee group. Information was provided by community leaders, state refugee coordinators, and county human resource officials in 1988.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22470302','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22470302"><span id="translatedtitle">Building climate resilience in the Blue Nile/Abay <span class="hlt">Highlands</span>: a role for Earth system sciences.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zaitchik, Benjamin F; Simane, Belay; Habib, Shahid; Anderson, Martha C; Ozdogan, Mutlu; Foltz, Jeremy D</p> <p>2012-02-01</p> <p>The Blue Nile (Abay) <span class="hlt">Highlands</span> of Ethiopia are characterized by significant interannual climate variability, complex topography and associated local climate contrasts, erosive rains and erodible soils, and intense land pressure due to an increasing population and an economy that is almost entirely dependent on smallholder, low-input agriculture. As a result, these <span class="hlt">highland</span> zones are highly vulnerable to negative impacts of climate variability. As patterns of variability and precipitation intensity alter under anthropogenic climate change, there is concern that this vulnerability will increase, threatening economic development and food security in the region. In order to overcome these challenges and to enhance sustainable development in the context of climate change, it is necessary to establish climate resilient development strategies that are informed by best-available Earth System Science (ESS) information. This requirement is complicated by the fact that climate projections for the Abay <span class="hlt">Highlands</span> contain significant and perhaps irreducible uncertainties. A critical challenge for ESS, then, is to generate and to communicate meaningful information for climate resilient development in the context of a highly uncertain climate forecast. Here we report on a framework for applying ESS to climate resilient development in the Abay <span class="hlt">Highlands</span>, with a focus on the challenge of reducing land degradation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=vietnam+AND+economy&pg=2&id=EJ818283','ERIC'); return false;" href="http://eric.ed.gov/?q=vietnam+AND+economy&pg=2&id=EJ818283"><span id="translatedtitle">Competing for Coffee Space: Development-Induced Displacement in the Central <span class="hlt">Highlands</span> of Vietnam</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Doutriaux, Sylvie; Geisler, Charles; Shively, Gerald</p> <p>2008-01-01</p> <p>Vietnam has emerged as the world's second largest producer of coffee. The benefits of this expanding coffee economy are substantial but not universal; their distribution follows ethnic lines despite government commitment to equalize welfare. Focusing on Dak Lak Province in Vietnam's Central <span class="hlt">Highlands</span>, we investigate this commercial transformation…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GeoRL..43.6844B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GeoRL..43.6844B"><span id="translatedtitle">GPS constraints on broad scale extension in the Ethiopian <span class="hlt">Highlands</span> and Main Ethiopian Rift</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Birhanu, Yelebe; Bendick, Rebecca; Fisseha, Shimeles; Lewi, Elias; Floyd, Michael; King, Robert; Reilinger, Robert</p> <p>2016-07-01</p> <p>Measurements from GPS sites spanning the Ethiopian <span class="hlt">Highlands</span>, Main Ethiopian Rift, and Somali Platform in Ethiopia and Eritrea show that present-day finite strain rates throughout NE Africa can be approximated at the continent scale by opening on the MER. Most sites in the Ethiopian <span class="hlt">Highlands</span> are consistent with the motion of the Nubian plate at the level of 1 mm/yr with 95% confidence. However, sites at least as far as 60 km west of the rift show higher velocities relative to the stable Nubian frame of 1-2 mm/yr, requiring a combination of localized and distributed deformation to accommodate the African extensional domain. Off-rift velocities are consistent with ongoing strain related to either high gravitational potential energy or intrusive magmatism away from midrift magmatic segments either on the western rift margin or within the Ethiopian <span class="hlt">Highlands</span>, especially when combined with likely rheological differences between the Ethiopian Rift and <span class="hlt">Highlands</span>. Velocities from the Somali Platform are less well determined with uncertainties and residuals from a Somali frame definition at the level of 2-3 mm/yr but without spatially correlated residuals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=sanitation+AND+urban&pg=2&id=ED085203','ERIC'); return false;" href="http://eric.ed.gov/?q=sanitation+AND+urban&pg=2&id=ED085203"><span id="translatedtitle">The <span class="hlt">Highland</span> Park Environmental Health Plan: Evaluation and Recommendations for Improving the Urban Environment.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Michigan State Dept. of Commerce, Lansing. Community Planning Div.</p> <p></p> <p>The <span class="hlt">Highland</span> Park environmental health plan includes the following components: Legal and administrative and programmatic relationships, planning studies, residential environment, disease vector control, water and sewage systems, sanitation, air pollution, food protection, industrial and radiological health, and solid waste facilities. (JR)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED125631.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED125631.pdf"><span id="translatedtitle"><span class="hlt">Highland</span> High School Vocational Television; a Salt Lake Schools Exemplary Vocational Program.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Nagle, LaMar C.</p> <p></p> <p>The <span class="hlt">Highland</span> High School (Salt Lake City, Utah) vocational television production program was designed to provide students with marketable skills in color television studio operation. Among the skills covered in the program were camera set-up and operation, video engineering, production switching, directing, television lighting, audio engineering,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=20010044510&hterms=Magnetism&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DMagnetism','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=20010044510&hterms=Magnetism&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DMagnetism"><span id="translatedtitle">Constraints on Sources of Strong Crustal Magnetism in the Southern <span class="hlt">Highlands</span> of Mars</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Raymond, C. A.; Smrekar, S. E.</p> <p>2001-01-01</p> <p>Magnetic models, guided by results of gravity-topography admittance studies, suggest that the anomaly pattern in the central southern <span class="hlt">highlands</span> of Mars results from large blocks of coherently magnetized crust separated by 'non-magnetic' areas. Additional information is contained in the original extended abstract.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=320969','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=320969"><span id="translatedtitle">Morphological dynamics of gully systems in the subhumid Ethiopian <span class="hlt">Highlands</span>: The Debre Mawi watershed</span></a></p> <p><a target="_blank" href="http://www.ars.usda.gov/services/TekTran.htm">Technology Transfer Automated Retrieval System (TEKTRAN)</a></p> <p></p> <p></p> <p>Gully expansion in the Ethiopian <span class="hlt">highlands</span> dissects vital agricultural lands with the eroded materials adversely impacting downstream resources, for example as they accumulate in reservoirs. While gully expansion and rehabilitation have been more extensively researched in the semi-arid region of Eth...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-09-19/pdf/2012-23064.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-09-19/pdf/2012-23064.pdf"><span id="translatedtitle">77 FR 58181 - Power Resources, Inc., Smith Ranch <span class="hlt">Highland</span> Uranium Project; License Renewal Request, Opportunity...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-09-19</p> <p>... NRC E-Filing rule (72 FR 49139, August 28, 2007). The E-Filing process requires participants to submit... 2.311.\\3\\ \\3\\ Requesters should note that the filing requirements of the NRC's E-Filing Rule (72 FR... COMMISSION Power Resources, Inc., Smith Ranch <span class="hlt">Highland</span> Uranium Project; License Renewal Request,...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=history+AND+Peru&pg=6&id=EJ200441','ERIC'); return false;" href="http://eric.ed.gov/?q=history+AND+Peru&pg=6&id=EJ200441"><span id="translatedtitle">The Politics of Schooling in the Nonliterate Third World: The Case of <span class="hlt">Highland</span> Peru.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Hazen, Dan C.</p> <p>1978-01-01</p> <p>Presents a case study of a village in <span class="hlt">highland</span> South America to show how different segments of a society view literacy education. Topics discussed include collapse of traditional society as a result of education, values, changing economic and social conditions, the school role in creating an active citizenry, and school drop-out rates. (Author/DB)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-09-22/pdf/2011-24331.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-09-22/pdf/2011-24331.pdf"><span id="translatedtitle">76 FR 58850 - <span class="hlt">Highland</span> Capital Management, L.P., et al.; Notice of Application</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-09-22</p> <p>... From the Federal Register Online via the Government Publishing Office SECURITIES AND EXCHANGE COMMISSION <span class="hlt">Highland</span> Capital Management, L.P., et al.; Notice of Application September 15, 2011. AGENCY: Securities and Exchange Commission (``Commission''). ACTION: Notice of an application under section 6(c) of the Investment Company Act of 1940...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=physical+AND+education&pg=5&id=EJ1061439','ERIC'); return false;" href="http://eric.ed.gov/?q=physical+AND+education&pg=5&id=EJ1061439"><span id="translatedtitle">Incorporating Scottish <span class="hlt">Highland</span> Games and Activities into Your Physical Education Classes</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Prewitt, Steven L.; Hannon, James C.; Brusseau, Timothy</p> <p>2015-01-01</p> <p>The purpose of this article is to introduce a potentially new and exciting group of activities that can be taught in physical education. Activities based on Scottish <span class="hlt">Highland</span> Games can be an interesting way to incorporate history and literature into the curriculum, as well as introduce students to a variety of unique physical activities. This…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-11-16/pdf/2012-27875.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-11-16/pdf/2012-27875.pdf"><span id="translatedtitle">77 FR 68854 - <span class="hlt">Highland</span> Associates, Inc. and Financial Investors Trust; Notice of Application</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-11-16</p> <p>... without shareholder approval. Applicants: <span class="hlt">Highland</span> Associates, Inc. (the ``Adviser'') and Financial... shareholders representing a majority of each Redmont Fund's shares. \\1\\ Applicants also request relief with... Agreements will be approved by shareholders and by the Board, including a majority of the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.P31E1740G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.P31E1740G"><span id="translatedtitle">The Bulk Density of the Tyrrhena Patera <span class="hlt">Highland</span> Volcano, Mars</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Grott, M.; Wieczorek, M. A.</p> <p>2011-12-01</p> <p>Tyrrhena Patera is a low-relief, central-vent volcano located in the southern <span class="hlt">highlands</span> of Mars, northeast of the Hellas impact basin. The main edifice contains few primary lave flow features and the flanks of the volcano are heavily eroded, indicating that they are composed of friable material which could have been formed by pyroclastic flows. The volcano itself was emplaced in the Noachian, but was subsequently modified during the Hesperian period, with episodes of resurfacing - probably driven by erosion - stretching well into the Amazonian period. Resurfacing of the caldera rille floor and upper shield probably mark the cessation of volcanic activity at Tyrrhena Patera around 800 Ma ago, and the geological evidence suggests that activity at Tyrrhena Patera transitioned from dominantly explosive to dominantly effusive eruptions. In summary, Tyrrhena Patera is generally thought to be predominantly composed of multi-layered, compacted ignimbrite deposits. The Tyrrhena Patera volcano is associated with a well localized positive free-air gravity anomaly and a good correlation exists with the features topography. We have used the latest gravity field model for Mars expanded up to degree and order 110 to model the localized admittance spectrum at Tyrrhena Patera considering surface as well as subsurface loading. We use a spherical cap localization window with a cap diameter of 7 degrees and a spherical harmonic bandwidth of 37. Ignoring the lowest degree terms that may be influenced by the Tharsis signal, we analyze the localized admittance in the degree range 42 to 57. The observed admittance is then compared to a forward model which is localized in the same manner as the data. In this way, we have quantified the range of admissible load densities as well as the admissible magnitude of a potentially present subsurface load. Modelling suggests that load densities need to be between 3290 and 3450 kg/m3 if no subsurface loads are present. If subsurface loads in the form</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3176254','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3176254"><span id="translatedtitle">New <span class="hlt">highland</span> distribution records of multiple Anopheles species in the Ecuadorian Andes</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2011-01-01</p> <p>Background Several recent climate change reviews have stressed the possibility of some malaria vectors occupying regions of higher altitudes than previously recorded. Indeed, <span class="hlt">highland</span> malaria has been observed in several African nations, possibly attributable to changes in land use, vector control and local climate. This study attempts to expand the current knowledge of the distribution of common Anopheles species in Ecuador, with particular attention to <span class="hlt">highland</span> regions (> 500 m) of the Andes. Methods Extensive field collections of larvae were undertaken in 2008, 2009 and 2010 throughout all regions of Ecuador (except the lower-altitude Amazonian plain) and compared to historical distribution maps reproduced from the 1940s. Larvae were identified using both a morphological key and sequencing of the 800 bp region of the CO1 mitochondrial gene. In addition, spatial statistics (Getis-Ord Hotspot Analysis: Gi*) were used to determine high and low-density clusters of each species in Ecuador. Results Distributions have been updated for five species of Anopheles in Ecuador: Anopheles albimanus, Anopheles pseudopunctipennis, Anopheles punctimacula, Anopheles eiseni and Anopheles oswaldoi s.l.. Historical maps indicate that An. pseudopunctipennis used to be widespread in <span class="hlt">highland</span> Andean valleys, while other species were completely restricted to lowland areas. By comparison, updated maps for the other four collected species show higher maximum elevations and/or more widespread distributions in <span class="hlt">highland</span> regions than previously recorded. Gi* analysis determined some <span class="hlt">highland</span> hot spots for An. albimanus, but only cold spots for all other species. Conclusions This study documents the establishment of multiple anopheline species in high altitude regions of Ecuador, often in areas where malaria eradication programs are not focused. PMID:21835004</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015Icar..255..127L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015Icar..255..127L"><span id="translatedtitle">Bulk hydrogen abundances in the lunar <span class="hlt">highlands</span>: Measurements from orbital neutron data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lawrence, David J.; Peplowski, Patrick N.; Plescia, Jeffrey B.; Greenhagen, Benjamin T.; Maurice, Sylvestre; Prettyman, Thomas H.</p> <p>2015-07-01</p> <p>The first map of bulk hydrogen concentrations in the lunar <span class="hlt">highlands</span> region is reported. This map is derived using data from the Lunar Prospector Neutron Spectrometer (LP-NS). We resolve prior ambiguities in the interpretation of LP-NS data with respect to non-polar hydrogen concentrations by comparing the LP-NS data with maps of the 750 nm albedo reflectance, optical maturity, and the wavelength position of the thermal infrared Christiansen Feature. The best explanation for the variations of LP-NS epithermal neutron data in the lunar <span class="hlt">highlands</span> is variable amounts of solar-wind-implanted hydrogen. The average hydrogen concentration across the lunar <span class="hlt">highlands</span> and away from the lunar poles is 65 ppm. The highest hydrogen values range from 120 ppm to just over 150 ppm. These values are consistent with the range of hydrogen concentrations from soils and regolith breccias at the Apollo 16 <span class="hlt">highlands</span> landing site. Based on a moderate-to-strong correlation of epithermal neutrons and orbit-based measures of surface maturity, the map of <span class="hlt">highlands</span> hydrogen concentration represents a new global maturity index that can be used for studies of the lunar soil maturation process. We interpret these hydrogen concentrations to represent a bulk soil property related to the long-term impact of the space environment on the lunar surface. Consequently, the derived hydrogen concentrations are not likely related to the surficial enhancements (top tens to hundreds of microns) or local time variations of OH/H2O measured with spectral reflectance data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15598618','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15598618"><span id="translatedtitle">The meteorology of the Western Indian Ocean, and the influence of the East African <span class="hlt">Highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Slingo, Julia; Spencer, Hilary; Hoskins, Brian; Berrisford, Paul; Black, Emily</p> <p>2005-01-15</p> <p>This paper reviews the meteorology of the Western Indian Ocean and uses a state-of-the-art atmospheric general circulation model to investigate the influence of the East African <span class="hlt">Highlands</span> on the climate of the Indian Ocean and its surrounding regions. The new 44-year re-analysis produced by the European Centre for Medium range Weather Forecasts (ECMWF) has been used to construct a new climatology of the Western Indian Ocean. A brief overview of the seasonal cycle of the Western Indian Ocean is presented which emphasizes the importance of the geography of the Indian Ocean basin for controlling the meteorology of the Western Indian Ocean. The principal modes of inter-annual variability are described, associated with El Nino and the Indian Ocean Dipole or Zonal Mode, and the basic characteristics of the subseasonal weather over the Western Indian Ocean are presented, including new statistics on cyclone tracks derived from the ECMWF re-analyses. Sensitivity experiments, in which the orographic effects of East Africa are removed, have shown that the East African <span class="hlt">Highlands</span>, although not very high, play a significant role in the climate of Africa, India and Southeast Asia, and in the heat, salinity and momentum forcing of the Western Indian Ocean. The hydrological cycle over Africa is systematically enhanced in all seasons by the presence of the East African <span class="hlt">Highlands</span>, and during the Asian summer monsoon there is a major redistribution of the rainfall across India and Southeast Asia. The implied impact of the East African <span class="hlt">Highlands</span> on the ocean is substantial. The East African <span class="hlt">Highlands</span> systematically freshen the tropical Indian Ocean, and act to focus the monsoon winds along the coast, leading to greater upwelling and cooler sea-surface temperatures.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12347196','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12347196"><span id="translatedtitle"><span class="hlt">Highland</span>-lowland conflict over natural resources: a case of Mae Soi, Chiang Mai, Thailand.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tungittiplakorn, W</p> <p>1995-01-01</p> <p>Interviews were conducted among 150 Hmong <span class="hlt">highland</span> and ethnic Thai lowland villagers during May-August 1992 in Chiang Mai in northern Thailand. Officials from national and international drug abuse control and development agencies were also interviewed. The aim was to determine the nature of the conflict between the <span class="hlt">highlanders</span> and the lowlanders. The lowlanders perceived that the conflict was due to environmental causes brought on by the Hmongs' destruction of forest and pollution of the river. The Mai Soi stream that was relied on by lowlanders was viewed as threatened by drought and water reduction from forest destruction. Shinawatra researched water runoff from major rivers during seasonal changes and found reduced volume during 1970-80. Alford found no significant change in stream flow. 71% of lowlanders reported that stream flow was reduced over a 3-6 year period. 40% reported that the forests were fenced off in order to protect the forests, but 22% were forced by village headmen to do so. 32% were promised land in the allocation areas. The <span class="hlt">highlanders</span> perceived the conflict in diverse ways. Many attributed the conflict to the murder of a lowlander cattle thief in a Hmong village in 1984. A 1983 report confirmed ethnic conflict and the killing and stealing of Hmong animals. Some <span class="hlt">highlanders</span> and lowlanders believe the conflict arose due to one person, Ajahn Pongsak Techadhammo, who tried to create environmental awareness among all tribes and ethnic groups. He was against lowlanders' misuse of forests and wanted relocation of the hill tribes that cultivated opium. Social status differences fuel the conflict. Lowlanders consider themselves superior to hill tribes that do not speak Thai and are not Buddhists. The hill tribes create discord because of their economic success with cash crops. The authors recommend forest, soil, and water conservation among <span class="hlt">highlanders</span> and lowlanders and broadening development to include other communities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014SPIE.9218E..1IK','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014SPIE.9218E..1IK"><span id="translatedtitle">Remote sensing capabilities of the GEO-<span class="hlt">CAPE</span> airborne simulator</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kowalewski, Matthew G.; Janz, Scott J.</p> <p>2014-09-01</p> <p>The Geostationary Coastal and Air Pollution Events (GEO-<span class="hlt">CAPE</span>) Airborne Simulator (GCAS) was designed and built at the NASA Goddard Space Flight Center (GSFC) as a technology demonstration instrument for the atmospheric science study group of GEO-<span class="hlt">CAPE</span> and potential validation instrument for NASA's Tropospheric Emissions: Monitoring Pollution (TEMPO) mission. GCAS was designed to make high altitude remote sensing observations of tropospheric and boundary layer pollutants, coastal and ocean water leaving radiances, and visible imagery for cloud and surface information. The instrument has participated in one flight campaign in Houston, TX as part of the Deriving Information on Surface Conditions from Column and Vertically Resolved Observations Relevant to Air Quality (DISCOVER-AQ) in September 2013. An overview of the instrument's design, characterization, and preliminary slant column retrievals of nitrogen dioxide (NO2) and ozone (O3) during the DISCOVER-AQ campaign will be provided in this paper.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20458874','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20458874"><span id="translatedtitle">Hepatic capillariasis in a <span class="hlt">Cape</span> ground squirrel (Xerus inaurus).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Erlwanger, K H; De Witt, B A; Fick, L G; Hetem, R S; Meyer, L C R; Mitchell, D; Wilson, W A; Mitchell, B</p> <p>2009-12-01</p> <p>We report, for the first time, an incidental finding of Calodium hepaticum infestation in a sub-adult female <span class="hlt">Cape</span> ground squirrel (Xerus inaurus). Post mortem examination of the squirrel revealed severe haemoperitoneum, splenomegaly and hepatomegaly with miliary white spots distributed diffusely throughout the hepatic parenchyma. Histologically the portal tracts in the liver showed granulomatous inflammation with fibrosis and numerous giant cells. Occasional adult worms were identified and there were multiple C. hepaticum eggs distributed diffusely throughout the portal tracts and the parenchyma. The spleen also contained C. hepaticum eggs. The genus Rattus is the primary host and reservoir of C. hepaticum, but C. hepaticum infections have been reported previously in other Sciuridae. Based on our findings, people should be cautious of the zoonotic potential of C. hepaticum, when they come into contact with the <span class="hlt">Cape</span> ground squirrel.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17774125','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17774125"><span id="translatedtitle">Preliminary Results of Recent Deep Drilling on <span class="hlt">Cape</span> Cod, Massachusetts.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Koteff, C; Cotton, J E</p> <p>1962-07-01</p> <p>In 1961 a 1000-foot drill hole near Harwich on <span class="hlt">Cape</span> Cod, Massachusetts, penetrated 435 feet of Pleistocene deposits above 50 to 60 feet of crystalline limestone and phyllitic schist, and more than 500 feet of phyllitic schist with abundant quartz veins. Similar rock is known in the Pennsylvanian and Precambrian (?) sections of Massachusetts and Rhode Island. Material of Eocene age was found in earlier drilling near Provincetown, but none was identified from this hole.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/de0514.photos.384122p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/de0514.photos.384122p/"><span id="translatedtitle">9. Photocopy of photograph of tower under construction at <span class="hlt">Cape</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>9. Photocopy of photograph of tower under construction at <span class="hlt">Cape</span> Henlopen, Delaware, May 1924 (original photograph in National Archives and Records Service, Still Pictures in Branch, RG 26, 26-LG-19-14-B), photographer unknown, May 23, 1924. - Mispillion Lighthouse, Beacon Tower, South bank of Mispillion River at it confluence with Delaware River at northeast end of County Road 203, 7 miles east of Milford, Milford, Sussex County, DE</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('//www.loc.gov/pictures/collection/hh/item/de0514.photos.384123p/','SCIGOV-HHH'); return false;" href="//www.loc.gov/pictures/collection/hh/item/de0514.photos.384123p/"><span id="translatedtitle">10. Photocopy of photograph of tower as constructed at <span class="hlt">Cape</span> ...</span></a></p> <p><a target="_blank" href="http://www.loc.gov/pictures/collection/hh/">Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey</a></p> <p></p> <p></p> <p>10. Photocopy of photograph of tower as constructed at <span class="hlt">Cape</span> Henlopen, Delaware, September 1926 (original photograph in National Archives and Records Service, Still Pictures Branch, RG 26, 26-LG-22-A), photographer G.W. Hitchens, September 10, 1926. "New Tower. Camera Station West 100 ft." - Mispillion Lighthouse, Beacon Tower, South bank of Mispillion River at it confluence with Delaware River at northeast end of County Road 203, 7 miles east of Milford, Milford, Sussex County, DE</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2015MNSSA..74..204G&link_type=ABSTRACT','NASAADS'); return false;" href="http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2015MNSSA..74..204G&link_type=ABSTRACT"><span id="translatedtitle">The Magnetic Observatory Buildings at the Royal Observatory, <span class="hlt">Cape</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Glass, I. S.</p> <p>2015-10-01</p> <p>During the 1830s there arose a strong international movement, promoted by Carl Friedrich Gauss and Alexander von Humboldt, to characterise the earth's magnetic field. By 1839 the Royal Society in London, driven by Edward Sabine, had organised a "Magnetic Crusade" - the establishment of a series of magnetic and meteorological observatories around the British Empire, including New Zealand, Australia, St Helena and the <span class="hlt">Cape</span>. This article outlines the history of the latter installation, its buildings and what became of them.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006OSJ....41...59J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006OSJ....41...59J"><span id="translatedtitle">Heterotrophic euglenids from marine sediments of <span class="hlt">cape</span> tribulation, tropical australia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Je Lee, Won</p> <p>2006-06-01</p> <p>This paper presents new data on free-living heterotrophic euglenids (Euglenozoa, Protista) that occurred in the marine sediments at <span class="hlt">Cape</span> Tribulation, Queensland, Australia. Twenty-nine species from 9 genera are described with uninterpreted records based on light microscopy, including one new taxon: Notosolenus capetribulationi n. sp. There was little evidence for endemism because the majority of heterotrophic euglenid species encountered here have been reported or were found from other habitats.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://woodshole.er.usgs.gov/pubs/of2006-1169/','USGSPUBS'); return false;" href="http://woodshole.er.usgs.gov/pubs/of2006-1169/"><span id="translatedtitle">Submarine Hydrogeological Data from <span class="hlt">Cape</span> Cod National Seashore</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Cross, VeeAnn A.; Bratton, John F.; Crusius, John; Colman, John A.; McCobb, Timothy D.</p> <p>2008-01-01</p> <p>In order to test hypotheses about ground water flow under and into estuaries and the Atlantic Ocean, geophysical surveys, geophysical probing, submarine ground-water sampling, and sediment coring were conducted by U.S. Geological Survey (USGS) scientists at <span class="hlt">Cape</span> Cod National Seashore (CCNS) in Massachusetts from 2004 through 2006. This USGS Open-File Report presents the data collected as a result of these field efforts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=STS039-83-091&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D5w','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=STS039-83-091&hterms=5w&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D5w"><span id="translatedtitle">Current Boundries and Sun Glint, <span class="hlt">Cape</span> Hatteras, NC, USA</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1991-01-01</p> <p>In this view of <span class="hlt">Cape</span> Hatteras, NC (35.0N, 75.5W) the barrier islands appear off the coast in sunglint. Sun light reflected from the water's surface makes patterns that indicate the surface condition. Smooth water has a high reflectance and is seen as a bright area. Rough water on the other hand, disperses the light and appears dark. Ocean currents in this region are very dynamic because of the Gulf Stream interacting with ocean currents.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMEP23B0963P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMEP23B0963P"><span id="translatedtitle">Tidal Variability of Infragravity Waves Over <span class="hlt">Cape</span>-Associated Shoals</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paniagua-Arroyave, J. F.; Adams, P. N.; Valle-Levinson, A.; Parra, S. M.</p> <p>2015-12-01</p> <p>Particulate transport at <span class="hlt">cape</span>-related shoals is generally driven by water circulation that is derived from interactions among tides, waves, and wind. At inner-shelves with alongshore uniform slopes, it has been shown that gravity waves produce offshore-directed transport by means of infragravity (IG) motions. However, the influence of IG waves on the spatial and temporal patterns of particulate transport is not yet understood at <span class="hlt">cape</span>-related shoals (i.e. inner-shelves characterized by non-uniform bathymetry). To analyze the connection between IG waves and tides, cross-spectral and cross-wavelet analyses were performed on time series data of current profiles and pressure that were measured at both sides of a shoal (east swale and west swale) near <span class="hlt">Cape</span> Canaveral, Florida. Overall, IG wave heights were coherent with water levels at ~2 cycles/day with a 95% statistical confidence at both locations. However, the coherence at the west swale (closer to shore) was lower than at the east swale. High coherence squared (>0.8) between tidal motions and IG energy could be explained by changes in water depth that produced IG energy losses to sea-swell frequencies during low tide. The 1-m difference in mean depth between east and west locations may explain the difference in coherence as water is not shallow enough at the west swale to produce IG energy losses. This may highlight the sensitivity of IG waves to changes in water depth within this shoal complex. Our results agree with previous studies regarding tidal variability of IG energy in nearshore and inner-shelf environments and could be applied to improve understanding of the role of complicated bathymetry in particulate transport at <span class="hlt">cape</span>-associated shoals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMPA32A..05W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMPA32A..05W"><span id="translatedtitle"><span class="hlt">Cape</span> Adare - A sentinel for change in Antarctica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wilson, G. S.; Cary, C.; Cummings, V.; Hawes, I.; Hong, S. G.; Coleman, M.</p> <p>2015-12-01</p> <p><span class="hlt">Cape</span> Adare stretches some 40km beyond the Antarctic Continent across the Continental Shelf. It is flanked to the east by the northern Ross Sea and to the West by Robertson Bay. The following characteristics make it an ideal monitoring and observation point to understand the impact of warm ocean and climate propogating into Antarctica from the Southern Ocean: 1) Robertson Bay is some 500m deep and has the potential to record deep water inflow which is predicted as climate warms and is also indicated as the biggest risk for melting Antarctic ice shelves. 2) <span class="hlt">Cape</span> Adare also lies between the Antarctic continental high pressure and the Southern Ocean low pressure 3) Ridley Beach at the tip of the Peninsula is home to Antarctica's largest Adelie Penguin Colony In November 2015 we will conduct a pilot survey of the marine and terrestrial ecology and physical setting, with a view to determining what opportunities exist for a long term monitoring system. <span class="hlt">Cape</span> Adare and the Ridley Beach Penguin Colony also offers the advantage of being on the edge of the proposed Ross Sea marine protected area and may represent an opportunity to monitor the associated ecosystem.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1988QuRes..30..237O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1988QuRes..30..237O"><span id="translatedtitle">A late Wisconsinan marine incursion into <span class="hlt">Cape</span> Cod Bay, Massachusetts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Oldale, Robert N.</p> <p>1988-11-01</p> <p>Reinterpretation of seismic-reflection data from <span class="hlt">Cape</span> Cod Bay has produced a revised late Wisconsinan history. Acoustically laminated deposits, originally inferred to be glaciolacustrine, are shown to be glaciomarine by tracing them to glaciomarine mud in Stellwagen Basin, north of <span class="hlt">Cape</span> Cod Bay. A late Wisconsinan marine deposit of nonglacial origin overlies the glaciomarine deposits in <span class="hlt">Cape</span> Cod Bay. Both deposits indicate that the crust was isostatically depressed below the late Wisconsinan eustatic sea level and that deglaciation and marine submergence occurred simultaneously. Valleys cut into the marine deposits, both glacial and nonglacial, indicate that a low sea-level stand, the result of isostatic rebound, occurred shortly after the marine incursion. A transgressive uncomformity and marine deposits, both mostly of Holocene age, overlie the late Wisconsinan deposits. The marine incursion, regression, and Holocene transgression represent the northward passage of an isostatically induced peripheral bulge following deglaciation. In turn, the bulge, a response to crustal loading and unloading, indicates thick glacier ice in the terminal zone and lends support to arguments for a maximum Laurentide ice model. Evidence for a late Wisconsinan marine incursion, regression, and the passage of a peripheral bulge should be sought in the other bays and sounds of the New England terminal zone.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70013711','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70013711"><span id="translatedtitle">A late Wisconsinan marine incursion into <span class="hlt">Cape</span> Cod Bay, Massachusetts</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Oldale, R.N.</p> <p>1988-01-01</p> <p>Reinterpretation of seismic-reflection data from <span class="hlt">Cape</span> Cod Bay has produced a revised late Wisconsinan history. Acoustically laminated deposits, originally inferred to be glaciolacustrine, are shown to be glaciomarine by tracing them to glaciomarine mud in Stellwagen Basin, north of <span class="hlt">Cape</span> Cod Bay. A late Wisconsinan marine deposit of nonglacial origin overlies the glaciomarine deposits in <span class="hlt">Cape</span> Cod Bay. Both deposits indicate that the crust was isostatically depressed below the late Wisconsinan eustatic sea level and that deglaciation and marine submergence occurred simultaneously. Valleys cut into the marine deposits, both glacial and nonglacial, indicate that a low sea-level stand, the result of isostatic rebound, occurred shortly after the marine incursion. A transgressive uncomformity and marine deposits, both mostly of Holocene age, overlie the late Wisconsinan deposits. The marine incursion, regression, and Holocene transgression represent the northward passage of an isostatically induced peripheral bulge following deglaciation. In turn, the bulge, a response to crustal loading and unloading, indicates thick glacier ice in the terminal zone and lends support to arguments for a maximum Laurentide ice model. Evidence for a late Wisconsinan marine incursion, regression, and the passage of a peripheral bulge should be sought in the other bays and sounds of the New England terminal zone. ?? 1988.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19780010545','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19780010545"><span id="translatedtitle">LANDSAT application of remote sensing to shoreline-form analysis. [<span class="hlt">Cape</span> Hatteras, <span class="hlt">Cape</span> Lookout, and Assateague Island</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Dolan, R.; Hayden, B.; Heywood, J. (Principal Investigator)</p> <p>1978-01-01</p> <p>The author has identified the following significant results. Using Assateague Island, <span class="hlt">Cape</span> Hatteras, and <span class="hlt">Cape</span> Lookout, significantly high correlations were found for most of the six barrier island sections that were examined. Relationships were not consistent from island to island. It was concluded that coastal vulnerability to storm damage can not be assessed based on coastal orientation alone. When orientation data were combined with erosion data for individual barrier islands, the relationship could be used as a basis for barrier island classification. A method was developed to obtain large amounts of historical data on surface coastal process from aerial photography, which was called the orthogonal grid address system. Data on shoreline change and overwash penetration gathered on over 400 km of the mid-Atlantic coast, are being used by various federal and state agencies for planning purposes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150001322','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150001322"><span id="translatedtitle">Cubesat Application for Planetary Entry (<span class="hlt">CAPE</span>) Missions: Micro-Reentry Capsule (MIRCA)</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Esper, Jaime</p> <p>2014-01-01</p> <p>The Cubesat Application for Planetary Entry Missions (<span class="hlt">CAPE</span>) concept describes a high-performing Cubesat system which includes a propulsion module and miniaturized technologies capable of surviving atmospheric entry heating, while reliably transmitting scientific and engineering data. The Micro Return Capsule (MIRCA) is <span class="hlt">CAPEs</span> first planetary entry probe flight prototype. Within this context, this paper briefly describes <span class="hlt">CAPEs</span> configuration and typical operational scenario, and summarizes ongoing work on the design and basic aerodynamic characteristics of the prototype MIRCA vehicle. <span class="hlt">CAPE</span> not only opens the door to new planetary mission capabilities, it also offers relatively low-cost opportunities especially suitable to university participation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=65415&keyword=Composite+AND+restoration&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68447716&CFTOKEN=52881599','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=65415&keyword=Composite+AND+restoration&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68447716&CFTOKEN=52881599"><span id="translatedtitle">DEVELOPMENT AND EVALUATION OF A MACROINVERTEBRATE BIOTIC INTEGRITY INDEX (MBII) FOR REGIONALLY ASSESSING MID-ATLANTIC <span class="hlt">HIGHLANDS</span> STREAMS</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The multimetric Macroinvertebrate Biotic Integrity Index (MBII) was developed from data collected at 574 wadeable stream reaches in the Mid-Atlantic <span class="hlt">Highlands</span> region (MAHR) by the USEPA's Environmental Monitoring and Assessment Program (EMAP). Over 100 candidate metrics were eval...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780042902&hterms=Ants&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DAnts','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780042902&hterms=Ants&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DAnts"><span id="translatedtitle">Mineralogy, petrology and chemistry of ANT-suite rocks from the lunar <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Prinz, M.; Keil, K.</p> <p>1977-01-01</p> <p>Anorthositic-noritic-troctolitic (ANT) rocks are the oldest and most abundant rocks of the lunar surface, and comprise about 90% of the suite of the lunar <span class="hlt">highlands</span>. Consideration is given to the mineralogy, petrology, bulk chemistry, and origin of ANT-suite rocks. Problems associated in classifying and labeling lunar <span class="hlt">highland</span> rocks because of textural complexities occurring from impact modifications are discussed. The mineralogy of ANT-suite rocks, dominated by plagioclase, olivine and pyrozene, and containing various minor minerals, is outlined. The petrology of ANT-suite rocks is reviewed along with the major element bulk composition of these rocks, noting that they are extremely depleted in K2O and P2O5. Various models describing the origin of ANT-suite rocks are summarized, and it is suggested that this origin involves a parental liquid of high-alumina basalt with low Fe/Fe+Mg.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/scitech/biblio/7071703','SCIGOV-STC'); return false;" href="http://www.osti.gov/scitech/biblio/7071703"><span id="translatedtitle">Rural energy systems in Moroccan <span class="hlt">highlands</span>: A case study of Imlil</span></a></p> <p><a target="_blank" href="http://www.osti.gov/scitech">SciTech Connect</a></p> <p>Dougherty, W.W.</p> <p>1991-01-01</p> <p>In Morocco, strategies to provide energy to rural <span class="hlt">highland</span> communities are currently hampered by an inadequate knowledge of village energy systems. Little is known about the energy needs of specific groups toward which new energy delivery programs are being directed. The physical, sociological, and economic interdependencies regarding energy use are key determinants to successful technological intervention and were examined in the context of a cluster of representative <span class="hlt">highland</span> villages in Morocco. Field research was carried out in a valley of the High Atlas mountains known as Imlil. The study developed a comprehensive understanding of the operating energy system by an examination of the use of food, fuel, fodder, fertilizer, and animate energy resources. Energy use patterns were described in a threefold explanatory matrix. Sixteen summary characterizations are offered regarding the role of energy in the daily life of the Ait Mizane. Though strained, the Imlil energy system displays a functional state of equilibrium.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015E%26PSL.415..200B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015E%26PSL.415..200B"><span id="translatedtitle">Evidence for Amazonian highly viscous lavas in the southern <span class="hlt">highlands</span> on Mars</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brož, Petr; Hauber, Ernst; Platz, Thomas; Balme, Matt</p> <p>2015-04-01</p> <p>We have identified small-scale volcanic edifices, two cones and three domes with associated flows, within Terra Sirenum, a region situated in the martian southern <span class="hlt">highlands</span>. Based on thermal, morphological, and morphometrical properties, and the determination of absolute model ages, we conclude that these features were formed by volcanic activity of viscous lavas in the mid-Amazonian epoch, relatively recently in martian history. If our hypothesis is correct, this small volcanic field represents rare evidence of young volcanic activity in the martian <span class="hlt">highlands</span> in which martian equivalents of terrestrial lava domes and coulées might be present. On Earth, such landforms are usually formed by highly viscous evolved lavas, i.e., andesitic to rhyolitic, for which observational evidence is sparse on Mars. Hence, this field might be one of only a few where martian evolved lavas might be investigated in detail.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120011725','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120011725"><span id="translatedtitle">Fieldpath Lunar Meteorite Graves Nunataks 06157, a Magnesian Piece of the Lunar <span class="hlt">Highlands</span> Crust</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Zeigler, Ryan A.; Korotev, R. L.; Korotev, R. L.</p> <p>2012-01-01</p> <p>To date, 49 feldspathic lunar meteorites (FLMs) have been recovered, likely representing a minimum of 35 different sample locations in the lunar <span class="hlt">highlands</span>. The compositional variability among FLMs far exceeds the variability observed among <span class="hlt">highland</span> samples in the Apollo and Luna sample suites. Here we will discuss in detail one of the compositional end members of the FLM suite, Graves Nunataks (GRA) 06157, which was collected by the 2006-2007 ANSMET field team. At 0.79 g, GRA 06157 is the smallest lunar meteorite so far recovered. Despite its small size, its highly feldspathic and highly magnesian composition are intriguing. Although preliminary bulk compositions have been reported, thus far no petrographic descriptions are in the literature. Here we expand upon the bulk compositional data, including major-element compositions, and provide a detailed petrographic description of GRA 06157.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19910042965&hterms=rocks+minerals&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Drocks%2Bminerals','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19910042965&hterms=rocks+minerals&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Drocks%2Bminerals"><span id="translatedtitle">Magnetic beneficiation of <span class="hlt">highland</span> and hi-Ti mare soils - Rock, mineral, and glassy components</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Taylor, Lawrence A.; Oder, Robin R.</p> <p>1990-01-01</p> <p>The exploitation of lunar soil can provide valuable raw materials for in situ resource utilization at a lunar base. A study of magnetic characterization was undertaken of three mare and two <span class="hlt">highland</span> soils obtained from NASA. Beneficiation of mare and <span class="hlt">highland</span> soils by sizing and magnetic separation can effectively concentrate the important components of the soils (e.g., ilmenite, native Fe, plagioclase, and aggluminates). As a soil matures and the impact melts consume additional minerals and rocks, the modal percentage of the minerals will decrease. The 'normative' percentage will become much greater than the modal percentage. Therefore, greater efficiency of separation can be realized with the proper selection of maturity of the soil, as well as by secondary grinding to further liberate specific minerals from lithic fragments (e.g., ilmenite and plagioclase).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-10-26/pdf/2012-26371.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-10-26/pdf/2012-26371.pdf"><span id="translatedtitle">77 FR 65446 - Iowa Pacific Holdings, LLC and Permian Basin Railways-Control Exemption-<span class="hlt">Cape</span> Rail, Inc. and...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-10-26</p> <p>... interest in <span class="hlt">Cape</span>, the parent company of Mass Coastal, from the two existing <span class="hlt">Cape</span> shareholders, Podgurski... operates a network of about 100 miles of track and trackage rights in southeastern Massachusetts and...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70020267','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70020267"><span id="translatedtitle">The vernon supersuite: Mesoproterozoic A-type granitoid rocks in the New Jersey <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Volkert, R.A.; Drake, A.A.</p> <p>1998-01-01</p> <p>Abundant Mesoproterozoic A-type granitoid rocks of two intrusive suites underlie approximately 50 percent of the New Jersey <span class="hlt">Highlands</span>. These rocks, the Byram Intrusive and Lake Hopatcong Intrusive Suites, consist of granite, alaskite, quartz monzonite, monzonite, and minor pegmatite. Byram and Lake Hopatcong rocks, although different mineralogically, are similar geochemically and contain overlapping abundances of most major and trace elements. Petrographic relationships, geochronology, field relationships, and geochemical similarities support a comagmatic origin for both suites. They constitute the here named Vernon Supersuite.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=356958','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=356958"><span id="translatedtitle">Association between climate variability and malaria epidemics in the East African <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Zhou, Guofa; Minakawa, Noboru; Githeko, Andrew K.; Yan, Guiyun</p> <p>2004-01-01</p> <p>The causes of the recent reemergence of Plasmodium falciparum epidemic malaria in the East African <span class="hlt">highlands</span> are controversial. Regional climate changes have been invoked as a major factor; however, assessing the impact of climate in malaria resurgence is difficult due to high spatial and temporal climate variability and the lack of long-term data series on malaria cases from different sites. Climate variability, defined as short-term fluctuations around the mean climate state, may be epidemiologically more relevant than mean temperature change, but its effects on malaria epidemics have not been rigorously examined. Here we used nonlinear mixed-regression model to investigate the association between autoregression (number of malaria outpatients during the previous time period), seasonality and climate variability, and the number of monthly malaria outpatients of the past 10–20 years in seven <span class="hlt">highland</span> sites in East Africa. The model explained 65–81% of the variance in the number of monthly malaria outpatients. Nonlinear and synergistic effects of temperature and rainfall on the number of malaria outpatients were found in all seven sites. The net variance in the number of monthly malaria outpatients caused by autoregression and seasonality varied among sites and ranged from 18 to 63% (mean = 38.6%), whereas 12–63% (mean = 36.1%) of variance is attributed to climate variability. Our results suggest that there was a high spatial variation in the sensitivity of malaria outpatient number to climate fluctuations in the <span class="hlt">highlands</span>, and that climate variability played an important role in initiating malaria epidemics in the East African <span class="hlt">highlands</span>. PMID:14983017</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014E%26ES...18a2037Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014E%26ES...18a2037Z"><span id="translatedtitle">Mapping of government land encroachment in Cameron <span class="hlt">Highlands</span> using multiple remote sensing datasets</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zin, M. H. M.; Ahmad, B.</p> <p>2014-02-01</p> <p>The cold and refreshing <span class="hlt">highland</span> weather is one of the factors that give impact to socio-economic growth in Cameron <span class="hlt">Highlands</span>. This unique weather of the <span class="hlt">highland</span> surrounded by tropical rain forest can only be found in a few places in Malaysia. It makes this place a famous tourism attraction and also provides a very suitable temperature for agriculture activities. Thus it makes agriculture such as tea plantation, vegetable, fruits and flowers one of the biggest economic activities in Cameron <span class="hlt">Highlands</span>. However unauthorized agriculture activities are rampant. The government land, mostly forest area have been encroached by farmers, in many cases indiscriminately cutting down trees and hill slopes. This study is meant to detect and assess this encroachment using multiple remote sensing datasets. The datasets were used together with cadastral parcel data where survey lines describe property boundary, pieces of land are subdivided into lots of government and private. The general maximum likelihood classification method was used on remote sensing image to classify the land-cover in the study area. Ground truth data from field observation were used to assess the accuracy of the classification. Cadastral parcel data was overlaid on the classification map in order to detect the encroachment area. The result of this study shows that there is a land cover change of 93.535 ha in the government land of the study area between years 2001 to 2010, nevertheless almost no encroachment took place in the studied forest reserve area. The result of this study will be useful for the authority in monitoring and managing the forest.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22673720','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22673720"><span id="translatedtitle">Studies on hantavirus infection in small mammals captured in southern and central <span class="hlt">highland</span> area of Vietnam.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Luan, Vu Dinh; Yoshimatsu, Kumiko; Endo, Rika; Taruishi, Midori; Huong, Vo Thi; Dat, Dang Tuan; Tien, Pham Cong; Shimizu, Kenta; Koma, Takaaki; Yasuda, Shumpei P; Nhi, Le; Huong, Vu Thi Que; Arikawa, Jiro</p> <p>2012-09-01</p> <p>To investigate the distribution of hantaviruses among animals in Southern and Central <span class="hlt">Highland</span> area of Vietnam, a total of 1311 serum samples were obtained from rats and Asian house shrews (Suncus murinus) captured at 11 locations between 2006 and 2009. A total of 1066 serum samples from rats were examined for IgG antibodies against Hantaan virus, and there were 30 antibody-positive serum samples from rats that had been captured mainly in a port area and urban area in Ho Chi Minh City (HCMC) (2.8%). All of the antibody-positive rats were Rattus norvegicus, and they had Seoul virus (SEOV) genome in their lungs. SEOV sequences detected from rats captured in Southern Vietnam belonged to the same lineage as those from rats captured at Haiphong Port and a market area in Hanoi City. SEOV strain CSG5 was isolated from a rat captured at Saigon Harbor. Strain CSG5 showed a cross-neutralization pattern almost the same as that of a representative strain of SEOV. A total of 245 Asian house shrews were captured in the Central <span class="hlt">Highland</span> area and near HCMC. Sera were examined for IgG antibodies against Thottapalayam virus (TPMV), and 32 (13.1%) of the antibody-positive shrews were mainly from the Central <span class="hlt">Highland</span> area and showed a neutralizing antibody against TPMV. These results indicated that SEOV is distributed among R. norvegicus inhabiting harbor and urban areas of Southern Vietnam and that TPMV or an antigenically related virus is distributed among Asian house shrews in Central <span class="hlt">Highland</span> area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19800039413&hterms=Dunite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DDunite','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19800039413&hterms=Dunite&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DDunite"><span id="translatedtitle">A summary of the petrology and geochemistry of pristine <span class="hlt">highlands</span> rocks</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Norman, M. D.; Ryder, G.</p> <p>1979-01-01</p> <p>The petrology and geochemistry of pristine lunar <span class="hlt">highlands</span> rock samples consisting of ferroan anorthosites, norites, troctolites, spinel troctolites/dunite/lherzolite, and KREEP, are described. In addition, petrographic and chemical evidence is presented which shows that low-siderophile rocks are the result of endogenous igneous activity and not impact melt differentiation. For example, these rocks contain Fe-metal as a late-crystallizing phase, and have W/La ratios higher than polymict breccias.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/14983017','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/14983017"><span id="translatedtitle">Association between climate variability and malaria epidemics in the East African <span class="hlt">highlands</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhou, Guofa; Minakawa, Noboru; Githeko, Andrew K; Yan, Guiyun</p> <p>2004-02-24</p> <p>The causes of the recent reemergence of Plasmodium falciparum epidemic malaria in the East African <span class="hlt">highlands</span> are controversial. Regional climate changes have been invoked as a major factor; however, assessing the impact of climate in malaria resurgence is difficult due to high spatial and temporal climate variability and the lack of long-term data series on malaria cases from different sites. Climate variability, defined as short-term fluctuations around the mean climate state, may be epidemiologically more relevant than mean temperature change, but its effects on malaria epidemics have not been rigorously examined. Here we used nonlinear mixed-regression model to investigate the association between autoregression (number of malaria outpatients during the previous time period), seasonality and climate variability, and the number of monthly malaria outpatients of the past 10-20 years in seven <span class="hlt">highland</span> sites in East Africa. The model explained 65-81% of the variance in the number of monthly malaria outpatients. Nonlinear and synergistic effects of temperature and rainfall on the number of malaria outpatients were found in all seven sites. The net variance in the number of monthly malaria outpatients caused by autoregression and seasonality varied among sites and ranged from 18 to 63% (mean=38.6%), whereas 12-63% (mean=36.1%) of variance is attributed to climate variability. Our results suggest that there was a high spatial variation in the sensitivity of malaria outpatient number to climate fluctuations in the <span class="hlt">highlands</span>, and that climate variability played an important role in initiating malaria epidemics in the East African <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.er.usgs.gov/publication/70028056','USGSPUBS'); return false;" href="http://pubs.er.usgs.gov/publication/70028056"><span id="translatedtitle">Calcite-graphite thermometry of the Franklin Marble, New Jersey <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Peck, W.H.; Volkert, R.A.; Meredith, M.T.; Rader, E.L.</p> <p>2006-01-01</p> <p>We present new stable-isotope data for the Mesoproterozoic Franklin Marble from outcrops along an 80-km traverse parallel to and across strike of the structural grain of the western New Jersey <span class="hlt">Highlands</span>. Calcite and dolomite from marble have an average ??13C of 0.35??? ?? 0.73??? PDB (n = 46) and a more limited range than other Mesoproterozoic marbles from the Adirondacks and the Canadian Grenville Province. The small range of ??13C values from the New Jersey samples is consistent with the preservation of a primary marine isotopic signature and limited postdepositional isotopic modification, except proximal to Zn or Fe ore deposits and fault zones. Fractionations between calcite and well-formed graphite (??13C[Cal-Gr]) for analyzed Franklin Marble samples average 3.31???. ?? 0.25??? (n = 34), and dolomite-graphite fractionations average 3.07??? ?? 0.30??? (n = 6). Taken together, these indicate an average temperature of 769?? ?? 43??C during metamorphism associated with the Ottawan Orogeny in the New Jersey <span class="hlt">Highlands</span>. Thus, carbon isotope fractionations demonstrate that the Franklin Marble was metamorphosed at granulite facies conditions. Metamorphic temperatures are relatively constant for the area sampled and overprint the metamorphosed carbonatehosted Zn-Fe-Mn ore deposits. The results of this study support recent work proposing that pressure and temperature conditions during Ottawan orogenesis did not vary greatly across faults that partition the <span class="hlt">Highlands</span> into structural blocks. ?? 2006 by The University of Chicago. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19780050704&hterms=markov-chain+monte-carlo+analysis&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dmarkov-chain%2Bmonte-carlo%2Banalysis','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19780050704&hterms=markov-chain+monte-carlo+analysis&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dmarkov-chain%2Bmonte-carlo%2Banalysis"><span id="translatedtitle">A general cratering-history model and its implications for the lunar <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Woronow, A.</p> <p>1978-01-01</p> <p>Through analysis of a large number of Monte Carlo and Markov Chain simulations, a model for determining crater accumulation and crater obliteration histories has been derived. The model generally applies to populations of large craters. It predicts that the following relationships hold for subequilibrium-density crater populations: (1) the more negative the production function's exponent, alpha (N near D super alpha) the lower the crater density at which the population size-frequency distribution will significantly depart from its production function; (2) the more negative the production function's exponent, the less obliteration a crater population will sustain after a set number of impacts. Application of the model to the lunar <span class="hlt">highlands</span> implies (1) the production function for the large craters is highly structured, resembling the observed size-frequency distribution and not the function N near D to the -2; (2) even the densely cratered <span class="hlt">highlands</span> have not attained crater saturation or equilibrium. Direct simulations of the <span class="hlt">highlands</span>' crater population supports the model's implications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..1114137V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..1114137V"><span id="translatedtitle">Sediment yield in human-induced degraded catchments of the Northern Ethiopian <span class="hlt">Highlands</span>: magnitude and dynamics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vanmaercke, M.; Zenebe, A.; Poesen, J.; Nyssen, J.; Verstraeten, G.; Deckers, J.; Govers, G.</p> <p>2009-04-01</p> <p>The Northern Ethiopian <span class="hlt">Highlands</span> are a fragile environment, characterised by steep slopes, intense rainfall and a sparse vegetation cover. The extreme poverty, stagnating technology and high population and livestock densities induce serious soil erosion problems. This not only leads to lower crop yields but also reduces the life expectancy of many dams and reservoirs (used for power generation or water supply in the dry season) as a result of massive sedimentation. Although these problems demand for a thorough solution, little is known about the magnitude and dynamics of sediment transport in the Northern Ethiopian <span class="hlt">Highlands</span>. Therefore an intensive measuring campaign was conducted during the rainy season of 2006 in 10 subcatchments of the Geba (drainage area: 5180 km2), a tributary of the Tekeze (Atbara) river. These subcatchments range in size from 120 km2 to 4330 km2 and represent contrasting environments typical for the Northern Ethiopian <span class="hlt">Highlands</span>. In this paper, the results of this measuring campaign are discussed. The sediment yield for the 10 subcatchments range between 400 and 2500 t km-2 a-1, with an average value of 1400 t km-2 a-1. The uncertainties on these sediment yields were assessed by Monte Carlo simulations. Important spatial and temporal variations in suspended sediment export were noted. A few flash floods were recorded in detail for which clear positive hysteresis effects in sediment concentration were found. The environmental factors, causing the large differences in sediment yield between the studied catchments were assessed by means of a semi-quantitative model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19940016306&hterms=isotope+geochemistry&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Disotope%2Bgeochemistry','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19940016306&hterms=isotope+geochemistry&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Disotope%2Bgeochemistry"><span id="translatedtitle">Magnesian anorthosites from the western <span class="hlt">highlands</span> of the Moon: Isotope geochemistry and petrogenesis</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Snyder, Gregory A.; Taylor, Lawrence A.; Halliday, Alex N.</p> <p>1993-01-01</p> <p>Breccias from the Apollo 14 landing site have provided a wealth of information on the genesis of the lunar <span class="hlt">highlands</span>. Various pristine rock-types have been discovered in relative abundance including rare ferroan anorthosites and alkali-suite and magnesian-suite rocks. Mineral-chemical and radiogenic isotopic data are reported here for a newly discovered Mg-suite anorthosite from Apollo 14, sample 14303,347. Meyer et al. reported U-Pb zircon analyses of Mg-suite <span class="hlt">highlands</span> rocks from the western limb of the Moon. We have compiled these ages and generated a weighted average age of 4211 = 6 Ma; some 200 Ma younger than ferroan anorthosites. Utilizing this age for Mg-anorthosite 14303,347, our data results in an initial epsilon(sub Nd) value of -1.0 and initial Sr-87/Sr-86 of 0.69915. Based on trace-element, isotopic, and mineral-chemical data, the western <span class="hlt">highlands</span> Mg-suite is interpreted to be crustal precipitates of a picritic magma, which assimilated KREEPy trapped liquid from upper-mantle cumulates during its transport to the crust.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/20337259','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/20337259"><span id="translatedtitle">Climate change and <span class="hlt">highland</span> malaria: fresh air for a hot debate.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chaves, Luis Fernando; Koenraadt, Constantianus J M</p> <p>2010-03-01</p> <p>In recent decades, malaria has become established in zones at the margin of its previous distribution, especially in the <span class="hlt">highlands</span> of East Africa. Studies in this region have sparked a heated debate over the importance of climate change in the territorial expansion of malaria, where positions range from its neglect to the reification of correlations as causes. Here, we review studies supporting and rebutting the role of climatic change as a driving force for <span class="hlt">highland</span> invasion by malaria. We assessed the conclusions from both sides of the argument and found that evidence for the role of climate in these dynamics is robust. However, we also argue that over-emphasizing the importance of climate is misleading for setting a research agenda, even one which attempts to understand climate change impacts on emerging malaria patterns. We review alternative drivers for the emergence of this disease and highlight the problems still calling for research if the multidimensional nature of malaria is to be adequately tackled. We also contextualize <span class="hlt">highland</span> malaria as an ongoing evolutionary process. Finally, we present Schmalhausen's law, which explains the lack of resilience in stressed systems, as a biological principle that unifies the importance of climatic and other environmental factors in driving malaria patterns across different spatio-temporal scales. PMID:20337259</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4579291','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4579291"><span id="translatedtitle">Characteristics of soils in selected maize growing sites along altitudinal gradients in East African <span class="hlt">highlands</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Njuguna, Elijah; Gathara, Mary; Nadir, Stanley; Mwalusepo, Sizah; Williamson, David; Mathé, Pierre-Etienne; Kimani, Jackson; Landmann, Tobias; Juma, Gerald; Ong’amo, George; Gatebe, Erastus; Ru, Bruno Le; Calatayud, Paul-andré</p> <p>2015-01-01</p> <p>Maize is the main staple crop in the East African Mountains. Understanding how the edaphic characteristics change along altitudinal gradients is important for maximizing maize production in East African <span class="hlt">Highlands</span>, which are the key maize production areas in the region. This study evaluated and compared the levels of some macro and micro-elements (Al, Ca, Fe, K, Mg, Mn, Na and P) and other soil parameters (pH, organic carbon content, soil texture [i.e. % Sand, % Clay and % Silt], cation exchange capacity [CEC], electric conductivity [EC], and water holding capacity [HC]). Soil samples were taken from maize plots along three altitudinal gradients in East African <span class="hlt">highlands</span> (namely Machakos Hills, Taita Hills and Mount Kilimanjaro) characterized by graded changes in climatic conditions. For all transects, pH, Ca, K and Mg decreased with the increase in altitude. In contrast, % Silt, organic carbon content, Al and water holding capacity (HC) increased with increasing altitude. The research provides information on the status of the physical–chemical characteristics of soils along three altitudinal ranges of East African <span class="hlt">Highlands</span> and includes data available for further research. PMID:26509187</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19820048153&hterms=rust&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Drust','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19820048153&hterms=rust&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Drust"><span id="translatedtitle">Rust and schreibersite in Apollo 16 <span class="hlt">highland</span> rocks - Manifestations of volatile-element mobility</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hunter, R. H.; Taylor, L. A.</p> <p>1982-01-01</p> <p>Rust is a manifestation of halogen and volatile-metal mobility in the lunar environment. Schreibersite is stable as the primary phosphorus-bearing phase in the <span class="hlt">highland</span> rocks, a consequence of the inherently low oxygen fugacity within impact-generated melts. Apatite and whitlockite are subordinate in these rocks. The partitioning of P into phosphide in impact-generated melts, and the failure of phosphate to crystallize, effects a decoupling of the halogens and phosphorus. Of the Apollo 16 rocks, 63% contain rust, 70% contain schreibersite, and 52% contain both phases, thereby establishing the pervasiveness of volatile-elements throughout the <span class="hlt">highland</span> rocks. The major portion of these volatile-bearing phases occur in impact melt-rocks or in breccia matrices. Rhabdites of schreibersite in some of the FeNi grains indicate that there is a meteoritic contribution to the phosphorus in these rocks. Cl/P2O5 ratios in lunar <span class="hlt">highland</span> rocks are a function of secondary effects, with any apparent Cl-P correlations being coincidential. The present observations preclude the validity of models based on such elemental ratios in these rocks. The presence of rust in the clast laden matrices of pristine rocks indicates fugitive element localization. Pristine clasts may have been contaminated. The basis for a pristine volatile chemistry is questioned.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/27384226','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/27384226"><span id="translatedtitle">Water balance and irrigation water pumping of Lake Merdada for potato farming in Dieng <span class="hlt">Highland</span>, Indonesia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fadlillah, Lintang N; Widyastuti, M</p> <p>2016-08-01</p> <p>Lakes provide water resources for domestic use, livestock, irrigational use, etc. Water availability of lakes can be estimated using lake water balance. Lake water balance is calculated from the water input and output of a lake. Dieng <span class="hlt">Highland</span> has several volcanic lakes in its surroundings. Lake Merdada in Dieng <span class="hlt">Highland</span> has been experiencing extensive water pumping for several years more than other lakes in the surrounding area. It provides irrigation water for potato farming in Dieng <span class="hlt">Highland</span>. The hydrological model of this lake has not been studied. The modeled water balance in this research uses primary data, i.e., bathymetric data, soil texture, and outflow discharge, as well as secondary data, i.e., rainfall, temperature, Landsat 7 ETM+ band 8 image, and land use. Water balance input components consist of precipitation on the surface area, surface (direct) runoff from the catchment area, and groundwater inflow and outflow (G net), while the output components consist of evaporation, river outflow, and irrigation. It shows that groundwater is the dominant input and output of the lake. On the other hand, the actual irrigation water pumping plays the leading role as human-induced alteration of outflow discharge. The maximum irrigation pumping modeling shows that it will decrease lake storage up to 37.14 % per month and may affect the ecosystem inside the lake. PMID:27384226</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://ntrs.nasa.gov/search.jsp?R=19820048188&hterms=thorium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dthorium','NASA-TRS'); return false;" href="http://ntrs.nasa.gov/search.jsp?R=19820048188&hterms=thorium&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dthorium"><span id="translatedtitle">Thorium concentrations in the lunar surface. V - Deconvolution of the central <span class="hlt">highlands</span> region</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Metzger, A. E.; Etchegaray-Ramirez, M. I.; Haines, E. L.</p> <p>1982-01-01</p> <p>The distribution of thorium in the lunar central <span class="hlt">highlands</span> measured from orbit by the Apollo 16 gamma-ray spectrometer is subjected to a deconvolution analysis to yield improved spatial resolution and contrast. Use of two overlapping data fields for complete coverage also provides a demonstration of the technique's ability to model concentrations several degrees beyond the data track. Deconvolution reveals an association between Th concentration and the Kant Plateau, Descartes Mountain and Cayley plains surface formations. The Kant Plateau and Descartes Mountains model with Th less than 1 part per million, which is typical of farside <span class="hlt">highlands</span> but is infrequently seen over any other nearside <span class="hlt">highland</span> portions of the Apollo 15 and 16 ground tracks. It is noted that, if the Cayley plains are the result of basin-forming impact ejecta, the distribution of Th concentration with longitude supports an origin from the Imbrium basin rather than the Nectaris or Orientale basins. Nectaris basin materials are found to have a Th concentration similar to that of the Descartes Mountains, evidence that the latter may have been emplaced as Nectaris basin impact deposits.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRE..120..831Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRE..120..831Y"><span id="translatedtitle">Global occurrence trend of high-Ca pyroxene on lunar <span class="hlt">highlands</span> and its implications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yamamoto, S.; Nakamura, R.; Matsunaga, T.; Ogawa, Y.; Ishihara, Y.; Morota, T.; Hirata, N.; Ohtake, M.; Hiroi, T.; Yokota, Y.; Haruyama, J.</p> <p>2015-05-01</p> <p>We present details of the global distribution of high-Ca pyroxene (HCP)-rich sites in the lunar <span class="hlt">highlands</span> based on the global data set of hyperspectral reflectance obtained by the SELENE Spectral Profiler. Most HCP-rich sites in the lunar <span class="hlt">highlands</span> are found at fresh impact craters. In each crater, most of the detection points are distributed on the ejecta, rim, and floor of the impact craters rather than the central peaks, while the central peaks are dominated by purest anorthosite (PAN). This indicates that HCP-rich materials originate from relatively shallower regions of the lunar crust than PAN. In addition, while all ray craters with sizes larger than ˜40 km possess HCP-rich materials, small fresh craters with sizes less than ˜6-10 km do not, indicating that the uppermost mixing layers in the lunar crust are not dominated by HCP. Based on these results, we propose that in the upper lunar crust, a HCP-rich zone overlying the PAN layer exists below the uppermost mixing layer. This HCP-rich zone may originate from interstitial melt during the formation of the flotation anorthositic cumulate, while an impact ejecta origin, impact melt origin, and/or magmatic intrusion into the upper lunar crust may also account for the occurrence of HCP-rich sites in the <span class="hlt">highlands</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25749361','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25749361"><span id="translatedtitle">Agaricus section Arvenses: three new species in <span class="hlt">highland</span> subtropical Southwest China.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gui, Yang; Zhu, Guo-S; Callac, Philippe; Hyde, Kevin-D; Parra, Luis-A; Chen, Jie; Yang, Tong-J; Huang, Wan-B; Gong, Guang-L; Liu, Zuo-Y</p> <p>2015-03-01</p> <p>Agaricus is a genus of saprobic basidiomycetes with more than 400 species recognized worldwide, with about 50 species known in China. Our objective was to investigate three new species of section Arvenses in <span class="hlt">highland</span> subtropical Southwest China. Agaricus guizhouensis is a new species characterized by a white pileus with yellowish squamules, small ellipsoid spores and cheilocystidia with yellowish-brown pigments; another new species, Agaricus longistipes is recognized by its slender stipe, and its elongate-ellipsoid basidiospores; the third new one, Agaricus megalocarpus is remarkable by its large size and its pileus surface covered with fine brown squamules. It is firstly reported for Guizhou Province that Agaricus abruptibulbus, Agaricus flocculosipes, and Agaricus subrufescens are illustrated. Two probable new species require further studying. A phylogenetic analyses of rDNA-ITS sequence data belonging to section Arvenses showed that the section Arvenses is monophyletic and can be subdivided in five branches, the branch of A. subrufescens and four clades (A-D). The eight species from <span class="hlt">highland</span> subtropical Southwest China were distributed in all five branches, indicating that this <span class="hlt">highland</span> is at the climatic crossroads. The white pileus trait and the potential interest are discussed. These data suggest a potential species richness that remains to be discovered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1187274','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1187274"><span id="translatedtitle">Morphoea and Borrelia burgdorferi: results from the Scottish <span class="hlt">Highlands</span> in the context of the world literature</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Goodlad, J R; Davidson, M M; Gordon, P; Billington, R; Ho-Yen, D O</p> <p>2002-01-01</p> <p>Aims: Previous studies investigating the link between infection with Borrelia burgdorferi and morphoea have produced conflicting results. Often, these studies have been undertaken in patients from different regions or countries, and using methods of varying sensitivity for detecting Borrelia burgdorferi infection. This study aimed to establish whether a relation could be demonstrated in the <span class="hlt">Highlands</span> of Scotland, an area with endemic Lyme disease, with the use of a sensitive method for detecting the organism. Methods: The study was performed on biopsies of lesional skin taken from 16 patients from the <span class="hlt">Highlands</span> of Scotland with typical clinical features of morphoea. After histological confirmation of the diagnosis, a nested polymerase chain reaction (PCR) using primers to a unique conserved region of the Borrelia burgdorferi flagellin gene was performed on DNA extracts from each biopsy. A literature search was also performed for comparable studies. Results: None of the 16 patients had documented clinical evidence of previous infection with B burgdorferi. DNA was successfully extracted from 14 of the 16 cases but all of these were negative using PCR for B burgdorferi specific DNA, despite successful amplification of appropriate positive controls in every test. The results were compared with those of other documented studies. Conclusions: Examination of the literature suggests that there is a strong geographical relation between B burgdorferi and morphoea. These results, in which no such association was found, indicate that morphoea may not be associated with the subspecies of B burgdorferi found in the <span class="hlt">Highlands</span> of Scotland. PMID:12456775</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://dx.doi.org/10.1644/09-MAMM-A-346.1','USGSPUBS'); return false;" href="http://dx.doi.org/10.1644/09-MAMM-A-346.1"><span id="translatedtitle">Two new species of shrews (Soricidae) from the western <span class="hlt">highlands</span> of Guatemala</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Woodman, Neal</p> <p>2010-01-01</p> <p>The broad-clawed shrews (Soricomorpha: Soricidae: Cryptotis) encompass a clade of 5 species—Cryptotis alticolus (Merriam), C. goldmani (Merriam), C. goodwini Jackson, C. griseoventris Jackson, and C. peregrinus (Merriam)—that is known collectively as the Cryptotis goldmani group and is characterized by broadened forefeet, elongated and broadened fore claws, and broadened humeri. These shrews are distributed in <span class="hlt">highland</span> regions from central Mexico to Honduras. Two broad-clawed shrews, C. goodwini and C. griseoventris, occur in southern Mexico and Guatemala and are presumed sister species whose primary distinguishing feature is the larger size of C. goodwini. In an investigation of variation within and between these 2 species, I studied characteristics of the postcranial skeleton. Statistical analyses of a variety of character suites indicate that the forelimb morphology in this group exhibits less intraspecific variation and greater interspecific variation than cranio-mandibular morphology, although most skull characters support groupings based on forelimb characters. Together, these characters define 4 distinct groups among the specimens examined. C. griseoventris is restricted to the northern <span class="hlt">highlands</span> of Chiapas, Mexico, and C. goodwini occurs in the southern <span class="hlt">highlands</span> of Chiapas and Guatemala. Herein, I describe 2 new species of broad-clawed shrews from the Sierra de los Cuchumatanes, Guatemala.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4714085','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4714085"><span id="translatedtitle">Cuticular hydrocarbons corroborate the distinction between lowland and <span class="hlt">highland</span> Natal fruit fly (Tephritidae, Ceratitis rosa) populations</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Vaníčková, Lucie; Břízová, Radka; Pompeiano, Antonio; Ekesi, Sunday; Meyer, Marc De</p> <p>2015-01-01</p> <p>Abstract The cuticular hydrocarbons (CHs) and morphology of two Ceratitis rosa Karsch (Diptera: Tephritidae) populations, putatively belonging to two cryptic taxa, were analysed. The chemical profiles were characterised by two-dimensional gas chromatography with mass spectrometric detection. CHs of Ceratitis rosa that originated from the lowlands and <span class="hlt">highlands</span> of Kenya comprised of n-alkanes, monomethylalkanes, dimethylalkanes and unsaturated hydrocarbons in the range of the carbon backbone from C14 to C37. Hydrocarbons containing C29, C31, C33 and C35 carbon atoms predominated in these two populations. 2-Methyltriacontane was the predominant compound in both populations. Quantitative differences in the distribution of hydrocarbons of different chain lengths, mainly the C22, C32, C33 and C34 compounds of these two populations, were observed despite indistinct qualitative differences in these hydrocarbons. Morphological analyses of male legs confirmed that the flies belong to different morphotypes of Ceratitis rosa previously labelled as R1 and R2 for lowland and <span class="hlt">highland</span> populations, respectively. A statistical analysis of the CH compositions of the putative R1 and R2 species showed distinct interspecific identities, with several CHs specific for each of the lowland and <span class="hlt">highland</span> populations. This study supports a hypothesis that the taxon Ceratitis rosa consists of at least two biological species. PMID:26798275</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27384226','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27384226"><span id="translatedtitle">Water balance and irrigation water pumping of Lake Merdada for potato farming in Dieng <span class="hlt">Highland</span>, Indonesia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fadlillah, Lintang N; Widyastuti, M</p> <p>2016-08-01</p> <p>Lakes provide water resources for domestic use, livestock, irrigational use, etc. Water availability of lakes can be estimated using lake water balance. Lake water balance is calculated from the water input and output of a lake. Dieng <span class="hlt">Highland</span> has several volcanic lakes in its surroundings. Lake Merdada in Dieng <span class="hlt">Highland</span> has been experiencing extensive water pumping for several years more than other lakes in the surrounding area. It provides irrigation water for potato farming in Dieng <span class="hlt">Highland</span>. The hydrological model of this lake has not been studied. The modeled water balance in this research uses primary data, i.e., bathymetric data, soil texture, and outflow discharge, as well as secondary data, i.e., rainfall, temperature, Landsat 7 ETM+ band 8 image, and land use. Water balance input components consist of precipitation on the surface area, surface (direct) runoff from the catchment area, and groundwater inflow and outflow (G net), while the output components consist of evaporation, river outflow, and irrigation. It shows that groundwater is the dominant input and output of the lake. On the other hand, the actual irrigation water pumping plays the leading role as human-induced alteration of outflow discharge. The maximum irrigation pumping modeling shows that it will decrease lake storage up to 37.14 % per month and may affect the ecosystem inside the lake.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.8631W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.8631W"><span id="translatedtitle">Paraglacial fluvial bedrock incision in postglacial landscapes: the NW Scottish <span class="hlt">Highlands</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Whitbread, Katie; Jansen, John; Bishop, Paul; Fabel, Derek</p> <p>2010-05-01</p> <p>Glacial landscape forms are inherited by rivers following deglaciation. Hillslopes and valley floors configured by glacial erosion control the distribution of bedrock channels and potential sites for fluvial incision. The importance of 'stream power' parameters, channel slope and drainage area (discharge), in controlling the rate of incision is widely accepted, but the rate, timing and mechanisms of incision have yet to be quantified in these settings. The dual controls of glacially conditioned bedrock slopes and sediment supply set two of the key boundary conditions for temporally and spatially dynamic fluvial bedrock incision. Measurement of incision rates in these settings is key to understanding the influence of controls on fluvial erosion, and the role of the process in long-term evolution of deglaciated landscapes. In tectonically-passive, hard-rock terrains, such as the Scottish <span class="hlt">Highlands</span>, incisional fluvial features such as bedrock channels, gorges and waterfalls are common on glacially carved valley steps. Here we report preliminary data on fluvial incision rates measured with cosmogenic 10Be. Our results confirm a postglacial age of bedrock straths in the NW Scottish <span class="hlt">Highlands</span> and indicate a vertical incision rate of 0.3 mm/yr into resistant quartzites. Further work will explore erosion mechanisms and rates of incision across the Scottish <span class="hlt">Highlands</span>, and assess controls on fluvial incision, including the potential role of paraglacial sediment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20131136','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20131136"><span id="translatedtitle">From Biloxi to <span class="hlt">Cape</span> Town: curricular integration of service learning.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Richards, Elizabeth A Libby; Novak, Julie Cowan</p> <p>2010-01-01</p> <p>Team Reach Out started as a student-initiated service-learning project with the goal of providing on-going assistance to the victims of Hurricane Katrina. Four years after Hurricane Katrina, Team Reach Out refocused efforts to <span class="hlt">Cape</span> Town, South Africa, where 4 senior nursing students and 1 science student integrated their leadership skills with the application of public health knowledge, compassion, and concern to work in partnership with several international health agencies. This article reviews the service-learning framework, course planning, and implementation of a recent service-learning project.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncbi.nlm.nih.gov/pubmed/20131136','PUBMED'); return false;" href="http://www.ncbi.nlm.nih.gov/pubmed/20131136"><span id="translatedtitle">From Biloxi to <span class="hlt">Cape</span> Town: curricular integration of service learning.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Richards, Elizabeth A Libby; Novak, Julie Cowan</p> <p>2010-01-01</p> <p>Team Reach Out started as a student-initiated service-learning project with the goal of providing on-going assistance to the victims of Hurricane Katrina. Four years after Hurricane Katrina, Team Reach Out refocused efforts to <span class="hlt">Cape</span> Town, South Africa, where 4 senior nursing students and 1 science student integrated their leadership skills with the application of public health knowledge, compassion, and concern to work in partnership with several international health agencies. This article reviews the service-learning framework, course planning, and implementation of a recent service-learning project. PMID:20131136</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/7228329','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/7228329"><span id="translatedtitle">A survey of black mineworkers of the <span class="hlt">Cape</span> crocidolite mines.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Talent, J M; Harrison, W O; Solomon, A; Webster, I</p> <p>1980-01-01</p> <p>Between 1974-1978, a study group 970 mineworkers exposed from before July 1962 only to <span class="hlt">Cape</span> crocidolite were traced: 755 were alive and 215 dead. Of those still alive, 66.1% showed no radiological abnormalities of the chest; 8.9% had irregular small opacities only; 17.7% had pleural abnormalities only; and 7.3% had both. Five pleural mesotheliomas were found in living ex-workers; although only one was reported in those who had died, this was considered to be an underestimate. The incidences of pleural mesotheliomas in ex-employees of the mining industry outside of the study group are also described.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22668925','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22668925"><span id="translatedtitle">Fifty years of porphyria at the University of <span class="hlt">Cape</span> Town.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Meissner, Peter N; Corrigall, Anne V; Hift, Richard J</p> <p>2012-03-02</p> <p>The porphyrias are a group of disorders resulting from defective haem biosynthesis. One form, variegate porphyria, is common in South Africa as a result of a founder effect. Over the past 50 years, the University of <span class="hlt">Cape</span> Town Faculty of Health Sciences has built and maintained an international reputation for excellence in the field of porphyria. The porphyria group is respected for its research and for its accumulated experience in the management of these disorders. Equally important has been the comprehensive and holistic care offered to patients with porphyria, and to their families.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016Geote..50...21P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Geote..50...21P"><span id="translatedtitle">Ophiolitic association of <span class="hlt">Cape</span> Fiolent area, southwestern Crimea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Promyslova, M. Yu.; Demina, L. I.; Bychkov, A. Yu.; Gushchin, A. I.; Koronovsky, N. V.; Tsarev, V. V.</p> <p>2016-01-01</p> <p>An ophiolitic association consisting of serpentinized ultramafic rocks and serpentinite, layered mafic-ultramafic complex, gabbro and gabbrodolerite, fragments of parallel dike complex, pillow lava, black bedded chert, and jasper has been identified for the first time by authors in the <span class="hlt">Cape</span> Fiolent area. The chemistry of pillow lavas and dolerites, including REE patterns and a wide set of other microelements, indicates suprasubduction nature of the ophiolites and their belonging to a backarc basin that has reached the stage of spreading in its evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-705.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-705.pdf"><span id="translatedtitle">33 CFR 165.705 - Port Canaveral Harbor, <span class="hlt">Cape</span> Canaveral, Florida.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>....705 Port Canaveral Harbor, <span class="hlt">Cape</span> Canaveral, Florida. (a) Security Zone A—East (Trident) Basin, Port Canaveral Harbor, at <span class="hlt">Cape</span> Canaveral Air Force Station, Brevard County, Florida. All waters of the East Basin north of latitude 28°24′36″ N. (b) Security Zone B—Middle Basin, Port Canaveral Harbor, adjacent to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-705.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-705.pdf"><span id="translatedtitle">33 CFR 165.705 - Port Canaveral Harbor, <span class="hlt">Cape</span> Canaveral, Florida.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>....705 Port Canaveral Harbor, <span class="hlt">Cape</span> Canaveral, Florida. (a) Security Zone A—East (Trident) Basin, Port Canaveral Harbor, at <span class="hlt">Cape</span> Canaveral Air Force Station, Brevard County, Florida. All waters of the East Basin north of latitude 28°24′36″ N. (b) Security Zone B—Middle Basin, Port Canaveral Harbor, adjacent to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-05-24/pdf/2013-12444.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-05-24/pdf/2013-12444.pdf"><span id="translatedtitle">78 FR 31573 - Proposed Information Collection; Comment Request: Social Values of Ecosystem Services at <span class="hlt">Cape</span>...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-05-24</p> <p>... National Park Service Proposed Information Collection; Comment Request: Social Values of Ecosystem Services at <span class="hlt">Cape</span> Lookout National Seashore AGENCY: National Park Service, Interior. ACTION: Notice and request...: None. This is a new collection. Title: Social Values of Ecosystem Services at <span class="hlt">Cape</span> Lookout...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-120.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-120.pdf"><span id="translatedtitle">33 CFR 80.120 - <span class="hlt">Cape</span> Ann, MA to Marblehead Neck, MA.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> Ann, MA to Marblehead Neck, MA. 80.120 Section 80.120 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Atlantic Coast § 80.120 <span class="hlt">Cape</span> Ann, MA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=151144&keyword=corba&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68451667&CFTOKEN=87877860','EPA-EIMS'); return false;" href="http://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=151144&keyword=corba&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50&CFID=68451667&CFTOKEN=87877860"><span id="translatedtitle">DEVELOPMENT OF <span class="hlt">CAPE</span>-OPEN COMPLIANT PROCESS MODELING COMPONENTS IN MICROSOFT .NET</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The <span class="hlt">CAPE</span>-OPEN middleware standards were created to allow process modeling components (PMCs) developed by third parties to be used in any process modeling environment (PME) utilizing these standards. The <span class="hlt">CAPE</span>-OPEN middleware specifications were based upon both Microsoft's Compone...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=overlay&pg=7&id=EJ710154','ERIC'); return false;" href="http://eric.ed.gov/?q=overlay&pg=7&id=EJ710154"><span id="translatedtitle">Discourse, Differentiation, and Agency: Muslim Community Schools in Postapartheid <span class="hlt">Cape</span> Town</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Fataar, Aslam</p> <p>2005-01-01</p> <p>This article explores the establishment of schools set up by Muslim communities in <span class="hlt">Cape</span> Town, South Africa, after 1994. Twelve schools have been set up across the city: four primary schools, three high schools, four schools that have grades 1-12, and one school that has grades 1-3 and 8-10. They are registered with the Western <span class="hlt">Cape</span> Education…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-703.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-703.pdf"><span id="translatedtitle">33 CFR 80.703 - Little River Inlet, SC to <span class="hlt">Cape</span> Romain, SC.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Little River Inlet, SC to <span class="hlt">Cape</span> Romain, SC. 80.703 Section 80.703 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND... Inlet, SC to <span class="hlt">Cape</span> Romain, SC. (a) A line drawn from the westernmost extremity of the sand spit on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-723.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-723.pdf"><span id="translatedtitle">33 CFR 80.723 - Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false Amelia Island, FL to <span class="hlt">Cape</span>... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Seventh District § 80.723 Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL. (a) A line drawn from the southernmost extremity of Amelia Island to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-723.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-723.pdf"><span id="translatedtitle">33 CFR 80.723 - Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Amelia Island, FL to <span class="hlt">Cape</span>... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Seventh District § 80.723 Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL. (a) A line drawn from the southernmost extremity of Amelia Island to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-723.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-723.pdf"><span id="translatedtitle">33 CFR 80.723 - Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Amelia Island, FL to <span class="hlt">Cape</span>... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Seventh District § 80.723 Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL. (a) A line drawn from the southernmost extremity of Amelia Island to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-723.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-723.pdf"><span id="translatedtitle">33 CFR 80.723 - Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false Amelia Island, FL to <span class="hlt">Cape</span>... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Seventh District § 80.723 Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL. (a) A line drawn from the southernmost extremity of Amelia Island to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-723.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-723.pdf"><span id="translatedtitle">33 CFR 80.723 - Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false Amelia Island, FL to <span class="hlt">Cape</span>... SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Seventh District § 80.723 Amelia Island, FL to <span class="hlt">Cape</span> Canaveral, FL. (a) A line drawn from the southernmost extremity of Amelia Island to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=Primary+AND+election&pg=5&id=EJ739994','ERIC'); return false;" href="http://eric.ed.gov/?q=Primary+AND+election&pg=5&id=EJ739994"><span id="translatedtitle">A Survey of Music Education in the Primary Schools of South Africa's <span class="hlt">Cape</span> Peninsula</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Herbst, Anri; Wet, Jacques de; Rijsdijk, Susan</p> <p>2005-01-01</p> <p>We investigated the state of music education in government primary schools in the <span class="hlt">Cape</span> Peninsula (Western <span class="hlt">Cape</span> Province, South Africa) as perceived by the general class teacher. Since the first democratic elections in South Africa (1994), the entire primary and secondary school education system has changed drastically in terms of content, and…</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-120.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-120.pdf"><span id="translatedtitle">33 CFR 80.120 - <span class="hlt">Cape</span> Ann, MA to Marblehead Neck, MA.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false <span class="hlt">Cape</span> Ann, MA to Marblehead Neck, MA. 80.120 Section 80.120 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Atlantic Coast § 80.120 <span class="hlt">Cape</span> Ann, MA...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3715281','PMC'); return false;" href="http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3715281"><span id="translatedtitle">Reconstruction of major maternal and paternal lineages of the <span class="hlt">Cape</span> Muslim population</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Isaacs, Shafieka; Geduld-Ullah, Tasneem; Benjeddou, Mongi</p> <p>2013-01-01</p> <p>The earliest <span class="hlt">Cape</span> Muslims were brought to the <span class="hlt">Cape</span> (<span class="hlt">Cape</span> Town - South Africa) from Africa and Asia from 1652 to 1834. They were part of an involuntary migration of slaves, political prisoners and convicts, and they contributed to the ethnic diversity of the present <span class="hlt">Cape</span> Muslim population of South Africa. The history of the <span class="hlt">Cape</span> Muslims has been well documented and researched however no in-depth genetic studies have been undertaken. The aim of the present study was to determine the respective African, Asian and European contributions to the mtDNA (maternal) and Y-chromosomal (paternal) gene pool of the <span class="hlt">Cape</span> Muslim population, by analyzing DNA samples of 100 unrelated Muslim males born in the <span class="hlt">Cape</span> Metropolitan area. A panel of six mtDNA and eight Y-chromosome SNP markers were screened using polymerase chain reaction-restriction fragment length polymorphisms (PCR-RFLP). Overall admixture estimates for the maternal line indicated Asian (0.4168) and African mtDNA (0.4005) as the main contributors. The admixture estimates for the paternal line, however, showed a predominance of the Asian contribution (0.7852). The findings are in accordance with historical data on the origins of the early <span class="hlt">Cape</span> Muslims. PMID:23885197</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED136548.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED136548.pdf"><span id="translatedtitle"><span class="hlt">Cape</span> Barren English. Linguistic Communications: Working Papers of the Linguistic Society of Australia, No. 13.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Sutton, Peter</p> <p></p> <p><span class="hlt">Cape</span> Barren English is clearly the most aberrant dialect of English spoken in Australia. Descended from English sealers, whalers and ex-convicts and their Aboriginal wives, the inhabitants of <span class="hlt">Cape</span> Barren Island, Tasmania, have lived in relative isolation for the last 150 years or more. Their dialect is not a creolized pidgin; it has a number of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-115.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-115.pdf"><span id="translatedtitle">33 CFR 80.115 - Portland Head, ME to <span class="hlt">Cape</span> Ann, MA.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Portland Head, ME to <span class="hlt">Cape</span> Ann, MA... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Atlantic Coast § 80.115 Portland Head, ME to <span class="hlt">Cape</span> Ann... harbors, bays, and inlets on the east coast of Maine, New Hampshire, and Massachusetts from Portland...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-10-12/pdf/2012-24888.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-10-12/pdf/2012-24888.pdf"><span id="translatedtitle">77 FR 62257 - Draft Environmental Impact Statement for the Herring River Restoration Project, <span class="hlt">Cape</span> Cod National...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-10-12</p> <p>... National Park Service Draft Environmental Impact Statement for the Herring River Restoration Project, <span class="hlt">Cape</span>... Impact Statement (DEIS) for the Herring River Restoration Project in <span class="hlt">Cape</span> Cod National Seashore... Restoration Project will be available for public review online at the NPS's PEPC Web site (...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://eric.ed.gov/?q=smart+AND+cities&id=ED484726','ERIC'); return false;" href="http://eric.ed.gov/?q=smart+AND+cities&id=ED484726"><span id="translatedtitle">E-Powering the People: South Africa's Smart <span class="hlt">Cape</span> Access Project</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Valentine, Susan</p> <p>2004-01-01</p> <p>This document examines the launch of the Smart <span class="hlt">Cape</span> Access Project in <span class="hlt">Cape</span> Town, South Africa. In a city where more than 80 percent of the citizens do not have access to computers and fewer still can access the Internet, public officials set out to build a "smart city," where "informed people could connect to the world and to each other by the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1001397.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1001397.pdf"><span id="translatedtitle">Developing a Strategic Approach to Social Responsiveness at the University of <span class="hlt">Cape</span> Town, South Africa</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Favish, Judith; McMillan, Janice; Ngcelwane, Sonwabo V.</p> <p>2012-01-01</p> <p>Collaborative community-engaged scholarship has roots in many parts of the world, and engaged practitioners and researchers are increasingly finding each other and sharing resources globally. This article focuses on a "social responsiveness" initiative at the University of <span class="hlt">Cape</span> Town. Its story, told here by three University of <span class="hlt">Cape</span> Town…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-740.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-740.pdf"><span id="translatedtitle">33 CFR 80.740 - Long Key, FL to <span class="hlt">Cape</span> Sable, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false Long Key, FL to <span class="hlt">Cape</span> Sable, FL... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Gulf Coast § 80.740 Long Key, FL to <span class="hlt">Cape</span> Sable, FL. A line drawn from the microwave tower charted on Long Key at approximate position latitude 24°48.8′...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-740.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol1/pdf/CFR-2014-title33-vol1-sec80-740.pdf"><span id="translatedtitle">33 CFR 80.740 - Long Key, FL to <span class="hlt">Cape</span> Sable, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2014-07-01 2014-07-01 false Long Key, FL to <span class="hlt">Cape</span> Sable, FL... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Gulf Coast § 80.740 Long Key, FL to <span class="hlt">Cape</span> Sable, FL. A line drawn from the microwave tower charted on Long Key at approximate position latitude 24°48.8′...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-740.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-740.pdf"><span id="translatedtitle">33 CFR 80.740 - Long Key, FL to <span class="hlt">Cape</span> Sable, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Long Key, FL to <span class="hlt">Cape</span> Sable, FL... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Gulf Coast § 80.740 Long Key, FL to <span class="hlt">Cape</span> Sable, FL. A line drawn from the microwave tower charted on Long Key at approximate position latitude 24°48.8′...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-740.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec80-740.pdf"><span id="translatedtitle">33 CFR 80.740 - Long Key, FL to <span class="hlt">Cape</span> Sable, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Long Key, FL to <span class="hlt">Cape</span> Sable, FL... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Gulf Coast § 80.740 Long Key, FL to <span class="hlt">Cape</span> Sable, FL. A line drawn from the microwave tower charted on Long Key at approximate position latitude 24°48.8′...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-740.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec80-740.pdf"><span id="translatedtitle">33 CFR 80.740 - Long Key, FL to <span class="hlt">Cape</span> Sable, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2012-07-01 2012-07-01 false Long Key, FL to <span class="hlt">Cape</span> Sable, FL... INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Gulf Coast § 80.740 Long Key, FL to <span class="hlt">Cape</span> Sable, FL. A line drawn from the microwave tower charted on Long Key at approximate position latitude 24°48.8′...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-810.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-810.pdf"><span id="translatedtitle">33 CFR 80.810 - <span class="hlt">Cape</span> San Blas, FL to Perdido Bay, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false <span class="hlt">Cape</span> San Blas, FL to Perdido Bay, FL. 80.810 Section 80.810 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Eighth District § 80.810 <span class="hlt">Cape</span> San...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-805.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-805.pdf"><span id="translatedtitle">33 CFR 80.805 - Rock Island, FL to <span class="hlt">Cape</span> San Blas, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false Rock Island, FL to <span class="hlt">Cape</span> San Blas, FL. 80.805 Section 80.805 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND... to <span class="hlt">Cape</span> San Blas, FL. (a) A south-north line drawn from the Econfina River Light to the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-810.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol1/pdf/CFR-2011-title33-vol1-sec80-810.pdf"><span id="translatedtitle">33 CFR 80.810 - <span class="hlt">Cape</span> San Blas, FL to Perdido Bay, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2011-07-01 2011-07-01 false <span class="hlt">Cape</span> San Blas, FL to Perdido Bay, FL. 80.810 Section 80.810 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND SECURITY INTERNATIONAL NAVIGATION RULES COLREGS DEMARCATION LINES Eighth District § 80.810 <span class="hlt">Cape</span> San...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-805.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol1/pdf/CFR-2010-title33-vol1-sec80-805.pdf"><span id="translatedtitle">33 CFR 80.805 - Rock Island, FL to <span class="hlt">Cape</span> San Blas, FL.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... 33 Navigation and Navigable Waters 1 2010-07-01 2010-07-01 false Rock Island, FL to <span class="hlt">Cape</span> San Blas, FL. 80.805 Section 80.805 Navigation and Navigable Waters COAST GUARD, DEPARTMENT OF HOMELAND... to <span class="hlt">Cape</span> San Blas, FL. (a) A south-north line drawn from the Econfina River Light to the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-252.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-252.pdf"><span id="translatedtitle">33 CFR 167.252 - In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme. 167.252 Section 167.252 Navigation and Navigable Waters COAST... § 167.252 In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme. (a) A traffic...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec167-252.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec167-252.pdf"><span id="translatedtitle">33 CFR 167.252 - In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme. 167.252 Section 167.252 Navigation and Navigable Waters COAST... § 167.252 In the approaches to the <span class="hlt">Cape</span> Fear River: Traffic separation scheme. (a) A traffic...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec167-251.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec167-251.pdf"><span id="translatedtitle">33 CFR 167.251 - In the approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area. 167.251 Section 167.251 Navigation and Navigable Waters COAST GUARD... approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area. A precautionary area is established bounded by a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-251.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec167-251.pdf"><span id="translatedtitle">33 CFR 167.251 - In the approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false In the approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area. 167.251 Section 167.251 Navigation and Navigable Waters COAST GUARD... approaches to the <span class="hlt">Cape</span> Fear River: Precautionary area. A precautionary area is established bounded by a...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <center> <div class="footer-extlink text-muted"><small>Some links on this page may take you to non-federal websites. 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