Destabilization of Valles Marineris Wallslopes by Retreat of Ancient Glaciers

Details Destabilization of Valles Marineris Wallslopes by Retreat of Ancient Glaciers Destabilization of Valles Marineris Wallslopes by Retreat of Ancient Glaciers

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1713m&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1713

Physics

2

Scientific paper

Deep-seated gravitational spreading of most Valles Marineris
inter-chasma basement ridges strongly argues in favor of a minimum of 1
km of glacial infill, probably during the Hesperian.

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