Image Credit: NASA/JPL/ASU
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Context image credit: NASA/JPL/MOLA
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These fractures occur within the volcanic plains south of Elysium Mons. The discontinuation of the fractures - like the one below the main group - indicates that these features are not formed by downdrop of material along faults, but rather formed by the collapse of the ceiling of lava tubes. Small regions of mega-ripples (a dune form) can be seen at the base of the hills at the bottom of the image.
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