|Home >>||Advanced Search >>|
The Gateway to Astronaut Photography of Earth
(NASA Crew Earth Observations)
Astronaut Photography of Earth - Display Record
Low-resolution Browse Image(Most browse images are not color adjusted.)
ImagesConditions for Use of Images >>
Image Transformation Tutorial >> Saving, Color Adjusting, and Printing Images >>
Images to View on Your Computer Now
Request the original image file.
Download a Keyhole Markup Language (KML) file for use in Google Earth.
Electronic Image DataCamera Files >> No sound file available.
IdentificationMission: ISS016 Roll: E Frame: 31086 Mission ID on the Film or image: ISS016
Country or Geographic Name: MEXICO
Features: CERRO CULIACAN, RADIAL DRAINAGE
Center Point Latitude: 20.3 Center Point Longitude: -100.9 (Negative numbers indicate south for latitude and west for longitude)
Stereo: (Yes indicates there is an adjacent picture of the same area)
ONC Map ID: JNC Map ID:
CameraCamera Tilt: 32
Camera Focal Length: 400mm
Camera: E4: Kodak DCS760C Electronic Still Camera
Film: 3060E : 3060 x 2036 pixel CCD, RGBG array.
Percentage of Cloud Cover: 10 (0-10)
NadirGMT Date: 20080303 (YYYYMMDD) GMT Time: 200012 (HHMMSS)
Nadir Point Latitude: 22.2, Longitude: -101.3 (Negative numbers indicate south for latitude and west for longitude)
Nadir to Photo Center Direction: South
Sun Azimuth: 210 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 183 nautical miles (339 km)
Sun Elevation Angle: 58 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 1190
CaptionsCerro Culiacan, Guanajuato, 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 1400 known vents, with cinder cones being the dominant landform. Cerro Culiacan however, is a shield volcano formed by basaltic lavas; it 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 higher-viscosity lavas), and the 1100-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 down into 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.
Download Packaged File.
This option downloads the following items, packaged into a single file, if they are available:
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." .