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The generation of martian floods by the melting of ground ice above dykes

โœ Scribed by Nimmo, Francis; McKenzie, Dan


Book ID
109565021
Publisher
Nature Publishing Group
Year
1999
Tongue
English
Weight
321 KB
Volume
397
Category
Article
ISSN
0028-0836

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โœ David G. Jankowski; Steven W. Squyres ๐Ÿ“‚ Article ๐Ÿ“… 1993 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 788 KB

"Terrain softening" is a distinct style of landform degradation observed on Mars. The morphology and distribution of softened terrain have led to the hypothesis that it is the result of quasiviscous relaxation of topology due to the creep deformation of subsurface ice. In order to test this hypothes