Investigating Creep of Ground Ice as a Cause of Crater Relaxation in Martian High-Latitude Softened Terrain

Details Investigating Creep of Ground Ice as a Cause of Crater Relaxation in Martian High-Latitude Softened Terrain Investigating Creep of Ground Ice as a Cause of Crater Relaxation in Martian High-Latitude Softened Terrain

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.2044t&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.2044

Mathematics

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Scientific paper

We incorporated recent rheologic data for ice/dust mixtures into
finite-element models to investigate the conditions under which viscous
creep of martian ground ice can occur to create the modified craters
observed in the 'softened terrain' on Mars.

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