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Photographing the Earth from the International Space Station

Astronaut Photography of Earth - Display Record

ISS025-E-5538

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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View ISS025-E-5538.JPG 69313640437 No No
View ISS025-E-5538.JPG 270289540359 Yes Yes NASA's Earth Observatory web site
View ISS025-E-5538.JPG 8552771000664 No Yes NASA's Earth Observatory web site
View ISS025-E-5538.JPG 115756042882929 No No

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Electronic Image Data

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Identification

Mission: ISS025 Roll: E Frame: 5538 Mission ID on the Film or image: ISS025
Country or Geographic Name: ZIMBABWE
Features: GREAT DYKE OF ZIMBABWE, FAULTS
Center Point: Latitude: -20.5 Longitude: 29.8 (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:

Camera

Camera Tilt: 44
Camera Focal Length: 180mm
Camera: N2: Nikon D2Xs
Film: 4288E : 4288 x 2848 pixel CMOS sensor, RGBG imager color filter.

Quality

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

Nadir

GMT Date: 20100930 (YYYYMMDD) GMT Time: 135003 (HHMMSS)
Nadir Point Latitude: -17.5, Longitude: 29.0 (Negative numbers indicate south for latitude and west for longitude)

Nadir to Photo Center Direction: South
Sun Azimuth: 277 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 195 nautical miles (361 km)
Sun Elevation Angle: 30 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 4

Captions

Great Dyke of Zimbabwe, Africa

The Great Dyke of Zimbabwe is a layered mafic intrusion of igneous, metal-bearing rock that has been dated to approximately 2.5 billion years old. The dyke (or dike in American English) intrudes through the even older rocks of African craton, the core of oldest rocks forming the continent of Africa. In cross section, the Great Dyke looks somewhat triangular or keel-shaped, suggesting to geologists that it rose along deep faults associated with extension of the African crust.

This geological feature extends more than 550 kilometers (342 miles) northeast to southwest across the center of Zimbabwe, varying from 3 to 12 kilometers (2-8 miles) in width. The southern end of the dyke is captured in this astronaut photograph.

Layered mafic intrusions are usually associated with economically important metals such as chromium, nickel, copper, platinum, titanium, iron, vanadium, and tin. Chromium, in the form of the mineral chromite, and platinum are particularly abundant in the Great Dyke and actively mined. Younger faults have offset sections of the Dyke along its length; two of the most obvious faults in the image are indicated, with arrows showing the relative directions of offset.

While the Great Dyke and its metal ores are products of geologic processes from the deep past, more recent events have also left their mark on the landscape. Two large burn scars from fires are visible at image top center.

An older, more detailed view of the Great Dyke can be found in an astronaut photograph available here.



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