Martian terrain. This image shows a classic example of Martian sedimentary rock in Danielson Crater. The many layers of rock are regularly spaced, forming steps; this implies a series of strong cap layers alternating with weaker layers. At small scale, much of the rock is heavily fractured. Because the fractured pieces neatly fit together, this occurred after the deposit turned to rock. MARS Enhanced colour image ( less than 1 km (under a mile) top to bottom) Ê An optimised and enhanced version of NASA imagery. Credit: NASA/JPL/UArizona

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Size: 10240px × 4310px
Location: Mars
Photo credit: © NASA / digitaleye / Alamy / Afripics
License: Licensed
Model Released: No

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