Possible Evidences of Ice Dynamics in the Putative Glaciers at the Lower NW Flank of Hecates Tholus Volcano, Mars

Details Possible Evidences of Ice Dynamics in the Putative Glaciers at the Lower NW Flank of Hecates Tholus Volcano, Mars Possible Evidences of Ice Dynamics in the Putative Glaciers at the Lower NW Flank of Hecates Tholus Volcano, Mars

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1031c&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1031

Physics

Scientific paper

Glacial forms, like crevasses and bergschrunds give evidence of recent
glacial flow in the northwest flank of Hecates Tholus. We show several
working hypothesis on the origin of these forms and its relation with
slope gravitational processes and deglaciation.

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