|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 only apply to electronic still cameras.
No sound file available.
IdentificationMission: STS108 Roll: 711 Frame: 25 Mission ID on the Film or image: STS108
Country or Geographic Name: MOROCCO
Features: ANTI ATLAS MOUNTAINS
Center Point: Latitude: 29.0 Longitude: -9.0 (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: 46
Camera Focal Length: 110mm
Camera: HB: Hasselblad
Film: 5069 : Kodak Elite 100S, E6 Reversal, Replaces Lumiere, Warmer in tone vs. Lumiere.
Percentage of Cloud Cover: 10 (0-10)
GMT Date: 20011215 (YYYYMMDD) GMT Time: 133559 (HHMMSS)
Nadir Point Latitude: 25.6, Longitude: -10.1 (Negative numbers indicate south for latitude and west for longitude)
Nadir to Photo Center Direction: North
Sun Azimuth: 198 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 207 nautical miles (383 km)
Sun Elevation Angle: 39 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 152
CaptionsThe Anti-Atlas Mountains of northern Africa and the nearby Atlas mountains were created by the prolonged collision of the African and Eurasian tectonic plates, beginning about 80 million years ago. Massive sandstone and limestone layers have been crumpled and uplifted more than 4,000 meters in the High Atlas and to lower elevations in the Anti-Atlas. Between more continuous major fold structures, such as the Jbel Ouarkziz in the southwestern Anti-Atlas, tighter secondary folds (arrow) have developed.
Earlier, the supercontinent of Pangea rifted apart to form precursors to the Mediterranean and the Atlantic Ocean (Beauchamp and others, 1996). In those seas sands, clays, limey sediments, and evaporite layers (gypsum, rock salt) were deposited. Later, during the mountain-building plate collision, the gypsum layers flowed under the pressure and provided a slippery surface on which overlying rigid rocks could glide (Burkhard, 2001). The broad, open style of folds seen in this view is common where evaporites are involved in the deformation. Other examples can be found in the Southern Zagros of Iran and the Sierra Madre Oriental of Mexico.
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: Earth Science and Remote Sensing Unit, NASA-Johnson Space Center. "The Gateway to Astronaut Photography of Earth." .