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Faulting

Faulting
The deep trough slashing diagonally across the center of this image resulted from faulting and down-dropping of the land. Boulders the size of small buildings can be seen on the slopes of this depression, which is sunlit from the left. Dark streaks on the trough's slopes are the paths of small landslides. This trough and the shallower one in the lower part of the image cut across lava flows, suggesting that the trenches formed after the lava had cooled and hardened. Short, parallel ridges in the valley floors are probably dunes.


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