Earth Observations taken by the Expedition 15 Crew

NASA Image and Video Library

2007-07-21

ISS015-E-18808 (21 July 2007) --- Ceuta on the northern African coastline is featured in this image photographed by an Expedition 15 crewmember on the International Space Station. The small Spanish enclave of Ceuta occupies a narrow isthmus of land on the African side of the Strait of Gibraltar. This view illustrates the sharp contrast in land cover between urban Ceuta (pink to white residential and industrial rooftops at center), the bay formed by seawalls to the north of the city, and the higher elevations of Monte Hacho forming the end of the isthmus. Green, vegetated slopes surround the Spanish fort atop the mountain, which commands a clear view of the Strait of Gibraltar to the northwest (not shown). Several small dots are visible near the coastline to the northwest and south of Ceuta -- these are small pleasure or fishing boats.

Metamorphic and tectonic evolution of Ceuta peninsula (Internal Rif): new interpretation in the framework of arc and back arc evolution

NASA Astrophysics Data System (ADS)

Homonnay, Emmanuelle; Lardeaux, Jean-Marc; Corsini, Michel; Cenki-Tok, Bénédicte; Bosch, Delphine; Munch, Philippe; Romagny, Adrien; Ouazzani-Touhami, Mohamed

2016-04-01

In the last twenty years, various geophysical investigations have established that the Western Mediterranean opened in a subduction context as a back arc domain. In the Alboran basin the dip of the subduction plane is eastwards or southeastwards depending of considered models. If the geological records of back-arc opening are well-known, the arc-related tectonic and petrologic evolutions are still poorly documented. In order to decipher these markers, we focalised structural, petrological and thermo-chronological studies on the Ceuta peninsula located in the Rif belt, on the western part of the Gibraltar arc to the North of Morocco. The present-day tectonic pile is constituted by: (1) the upper Ceuta unit, composed of High Pressure and High Temperature metapelites retromorphosed under Amphibolite-facies condition, with Ultra-High Pressure relicts, and pyrigarnite and spinel bearing peridotites boudins at its base, (2) the lower Monte Hacho unit, with orthogneisses metamorphosed under Amphibolite-facies conditions. Structural analysis indicates a polyphase tectonic evolution: (1) an earlier deformation phase only observed in the UHP metapelites and characterized by a steep S1 foliation plane, (2) a main deformation phase associated to a pervasive gently dipping S2 foliation plane bearing a L2 stretching lineation and synschistose folds whose axes are parallel to L2 and (3) a late deformation phase which developed S3 foliation plane and L3 stretching lineation coeval with development of narrow normal ductile shear zones. A zone of increasing deformation, several dozen meters wide, is identified as a major ductile shear zone involving the peridotitic lenses at the base of the metapelites of the Ceuta unit and overlaying this upper unit on top of the orthogneisses of the Monte Hacho lower unit. The attitude of mylonitic foliation and stretching and mineral lineations as well as the numerous shear sense indicators observed in the shear zone are consistent with a

Rapid engineering of endothelial cell-lined vascular-like structures in in situ crosslinkable hydrogels.

PubMed

Kageyama, Tatsuto; Kakegawa, Takahiro; Osaki, Tatsuya; Enomoto, Junko; Ito, Taichi; Nittami, Tadashi; Fukuda, Junji

2014-06-01

Fabrication of perfusable vascular networks in vitro is one of the most critical challenges in the advancement of tissue engineering. Because cells consume oxygen and nutrients during the fabrication process, a rapid fabrication approach is necessary to construct cell-dense vital tissues and organs, such as the liver. In this study, we propose a rapid molding process using an in situ crosslinkable hydrogel and electrochemical cell transfer for the fabrication of perfusable vascular structures. The in situ crosslinkable hydrogel was composed of hydrazide-modified gelatin (gelatin-ADH) and aldehyde-modified hyaluronic acid (HA-CHO). By simply mixing these two solutions, the gelation occurred in less than 20 s through the formation of a stable hydrazone bond. To rapidly transfer cells from a culture surface to the hydrogel, we utilized a zwitterionic oligopeptide, which forms a self-assembled molecular layer on a gold surface. Human umbilical vein endothelial cells adhering on a gold surface via the oligopeptide layer were transferred to the hydrogel within 5 min, along with electrochemical desorption of the oligopeptides. This approach was applicable to cylindrical needles 200-700 µm in diameter, resulting in the formation of perfusable microchannels where the internal surface was fully enveloped with the transferred endothelial cells. The entire fabrication process was completed within 10 min, including 20 s for the hydrogel crosslinking and 5 min for the electrochemical cell transfer. This rapid fabrication approach may provide a promising strategy to construct perfusable vasculatures in cell-dense tissue constructs and subsequently allow cells to organize complicated and fully vascularized tissues while preventing hypoxic cell injury.

Miocene crustal extension following thrust tectonic in the Lower Sebtides units (internal Rif, Ceuta Peninsula, Spain): Implication for the geodynamic evolution of the Alboran domain

NASA Astrophysics Data System (ADS)

Homonnay, Emmanuelle; Corsini, Michel; Lardeaux, Jean-Marc; Romagny, Adrien; Münch, Philippe; Bosch, Delphine; Cenki-Tok, Bénédicte; Ouazzani-Touhami, Mohamed

2018-01-01

In Western Mediterranean, the Rif belt in Morocco is part of the Gibraltar Arc built during the Tertiary in the framework of Eurasia-Africa convergence. The structural and metamorphic evolution of the internal units of this belt as well as their timing, crucial to constrain the geodynamic evolution of the Alboran Sea, is still largely debated. Our study on the Ceuta Peninsula (Northern Rif) provides new structural, petrological and geochronological data (U-Th-Pb, Ar-Ar), which allow to precise the tectono-metamorphic evolution of the Lower Sebtides metamorphic units with: (1) a syn-metamorphic thrusting event developed under granulite facies conditions (7-10 kbar and 780-820 °C). A major thrust zone, the Ceuta Shear Zone, drove the emplacement of metapelites and peridotitic lenses from the Ceuta Upper Unit over the orthogneisses of the Monte Hacho Lower Unit. This compressional event ended during the Upper Oligocene. (2) an extensional event developed at the boundary between amphibolite and greenschist facies conditions (400-550 °C and 1-3 kbar). During this event, the Ceuta Shear Zone has been reactivated as a normal fault. Normal ductile shear zones contributed to the final exhumation of the metamorphic units during the Early Miocene. We propose that the compressional event is related to the formation of an orogenic wedge located in the upper plate, in a backward position, of the subduction zone driving the geodynamic evolution of the Alboran domain. In this context, the episode of lithospheric thinning could be related to the opening of the Alboran basin in a back-arc position. Furthermore, unlike the previous models proposed for the Rif belt, the tectonic coupling between mantle peridotites and crustal metamorphic rocks occurred in Ceuta Peninsula at a depth of 20-30 km under high temperature conditions, before the extensional event, and thus cannot be related to the back-arc extension. 1, BSE image of monazite. 2, CL image of monazite showing a thin rim