Eroded Beauty in the Sahara Desert

Taken by astronauts aboard the International Space Station, this detailed photograph shows dark surfaces in the hyper-arid eastern Sahara Desert in Sudan. These surfaces are flat-topped mesas that rise 70-140 meters (230-460 feet) above the surrounding lighter-toned landscape. The mesas are defined by vertical cliffs cut into by numerous small gullies, producing a heavily indented pattern. For scale, the smaller mesa measures 10 kilometers (6 miles) long.

The bed of a dry river winds across the middle of the image. A dotted pattern of trees and clumps of bushes follow the line of the riverbed, indicating that roots are reaching the subsurface water. (Click on the image to see a more detailed view.)

Analysis of the height of the mesas and the rock units exposed in the cliff faces allows geologists to interpret the evolution of the area's landscape. It is possible to conclude that the rock layer forming the two mesas was more extensive in the past, and that it has been stripped away by river and wind erosion to produce the younger, light-toned surface seen today.

Eroded desert landscapes with strongly contrasting darker and lighter-toned surfaces result from both physical and chemical weathering processes and are a common landscape pattern in this part of the Sahara Desert. Geologic maps indicate that the entire area is a single rock type known as the Nubian Sandstone, which is one of the largest fossil water aquifers in the world.

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This service is provided by the International Space Station program and the JSC Earth Science & Remote Sensing Unit, ARES Division, Exploration Integration Science Directorate.
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