
This terrain is unusual for the South Polar region of Mars, with a set of curved ridges of unknown origin. Small pits are present, often concentrated on the ridges, that may have resulted from sublimation of ice. https://photojournal.jpl.nasa.gov/catalog/PIA22803
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NASA ID
PIA22803
Date Created
October 29, 2018
Center
JPL
Media Type
image
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Medium
960px