Geomorphological Evidence for Shallow Ice in the Southern Hemisphere of Mars
The localized loss of near-surface excess ice on Mars by sublimation (and perhaps melting) can produce thermokarstic collapse features such as expanded craters and scalloped depressions, which can be indicators of the preservation of shallow ice. We demonstrate this by identifying High Resolution Im...
| Main Authors: | , |
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| Language: | en |
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AMER GEOPHYSICAL UNION
2018
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| Online Access: | http://hdl.handle.net/10150/627126 http://arizona.openrepository.com/arizona/handle/10150/627126 |