Image Credit: NASA/JPL/ASU
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Context image credit: NASA/JPL/MOLA
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Toward the westernmost extent of the Medusae Fossae Formation, a 5000+ km long belt of eroding sediments, the interleaving of erosional surfaces produces dramatic textural variations. In the lower third of this image, the cross-hatched MFF layer is being stripped back from a surface that was already heavily eroded before the MFF layer was deposited. Also note the sinuous and, in places, dendritic ridges that are either linear dunes or inverted channels.
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