| ISS016 Earth Sciences and Image Analysis Photographic Highlights |
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| ISS016-E-31086 |
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| Cerro Culiacan, Mexico:This astronaut photograph highlights
Cerro (Spanish for “hill”) Culiacan, part of the 50,000 km2
Michoacán-Guanajuato volcanic field of west-central Mexico. The
volcanic field contains over 1,400 known vents, with cinder cones,
steep, cone-shaped hills, being the dominant landform. Cerro Culiacan
however, is a shield volcano, a more gently sloping mound formed by
basaltic lavas. Cerro Culiacan most likely formed during the
Pleistocene Epoch approximately 10,000 to 2 million years ago. Shield
volcanoes in the Michoacán-Guanajuato field tend to have steeper
slopes than similar volcanic structures elsewhere (namely Iceland;
this is perhaps due to slightly thicker or higher-viscosity lavas),
and the 1,100-meter high Cerro Culiacan is no exception. The permeable, highly fractured basalt of Culiacan is an important component of the local hydrology. Precipitation that falls on the slopes of the hill swiftly infiltrates the sediments of the valley floor, providing sufficient moisture to support agriculture (green and brown fields at image center) and, in turn, several small cities such as Jaral del Progreso and El Capulin de la Trinidad (light gray regions with street grids). Precipitation has also incised the slopes of Cerro Culiacan with a radial drainage pattern, extending outwards from the peak in all directions much like the spokes of a bicycle wheel. |
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This service is provided by the International Space Station program and the JSC Astromaterials Research & Exploration Science Directorate. Recommended Citation: Image Science and Analysis Laboratory, NASA-Johnson Space Center. "The Gateway to Astronaut Photography of Earth." . |
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