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(NASA Crew Earth Observations)

Photographing the Earth from the International Space Station

Astronaut Photography of Earth - Display Record


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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View ISS009-E-22625.JPG 134488639435 No No
View ISS009-E-22625.JPG 453029540451 Yes Yes Earth From Space collection
View ISS009-E-22625.JPG 15176531000835 No Yes NASA's Earth Observatory web site
View ISS009-E-22625.JPG 211412130322064 No No

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Electronic Image Data

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Mission: ISS009 Roll: E Frame: 22625 Mission ID on the Film or image: ISS009
Country or Geographic Name: CHILE
Center Point: Latitude: -34.0 Longitude: -70.0 (Negative numbers indicate south for latitude and west for longitude)

Stereo: (Yes indicates there is an adjacent picture of the same area)


Camera Tilt: 7
Camera Focal Length: 180mm
Camera: E4: Kodak DCS760C Electronic Still Camera
Film: 3060E : 3060 x 2036 pixel CCD, RGBG array.


Film Exposure:
Percentage of Cloud Cover: 10 (0-10)


GMT Date: 20040914 (YYYYMMDD) GMT Time: 181209 (HHMMSS)
Nadir Point Latitude: -33.6, Longitude: -70.0 (Negative numbers indicate south for latitude and west for longitude)

Nadir to Photo Center Direction: South
Sun Azimuth: 323 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 198 nautical miles (367 km)
Sun Elevation Angle: 47 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 1238


Maipo Volcano, Chile

The high peaks of the Andes form the backbone of South America and the political border between Chile and Argentina. Formed from the subduction of the Nazca Plate under the South American Plate, the south-central Andes also includes several major volcanoes. One of the most active border volcanoes is Volcan Maipo, located just southeast of Santiago, Chile. The volcano’s summit (5264m) rests in the large Diamante Caldera, and is defined by a radial drainage pattern highlighted by snow cover (center right of image). Lava flows from an 1826 eruption blocked drainage within the caldera, forming Lake Diamante. The lake is a popular tourist destination. Maipo’s last significant eruption was in 1908.

Imagery of the region from the International Space Station includes seasonal observations—this image shows the volcano near the southern hemisphere spring equinox. The lake, just east of Maipo’s peak, is still ice covered. However, the increasing temperatures of spring are suggested by a muddy-looking streak near the lower left corner. The streak appears to be a landslide or avalanche that flowed westward down a rugged slope, possibly triggered by instability in the snowpack due to snow melt.

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