Gully Surface and Shallow Subsurface Structure in the South Fork of Wright Valley, Antarctic Dry Valleys: Implications for Gully Activity on Mars

Details Gully Surface and Shallow Subsurface Structure in the South Fork of Wright Valley, Antarctic Dry Valleys: Implications for Gully Activity on Mars Gully Surface and Shallow Subsurface Structure in the South Fork of Wright Valley, Antarctic Dry Valleys: Implications for Gully Activity on Mars

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1728l&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

7

Scientific paper

Gully analogs (Antarctic Dry Valleys) show that top-down melting of
trapped windblown snow is a major water source; meltwater soaks into the
hyporheic zone and travels along the top of the ice table, providing
insight into the origin of Mars gullies.

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