Rapid Growth of Mars-Analog Gullies in a Buried Ice Substrate: Gullies as a Disequilibrium Landform in Garwood Valley, Antarctica

Details Rapid Growth of Mars-Analog Gullies in a Buried Ice Substrate: Gullies as a Disequilibrium Landform in Garwood Valley, Antarctica Rapid Growth of Mars-Analog Gullies in a Buried Ice Substrate: Gullies as a Disequilibrium Landform in Garwood Valley, Antarctica

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1432l&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1432

Physics

Scientific paper

Gullies in Garwood Valley, Antarctica, form in buried ice that may be
highly analogous to martian gullies forming in the latitude-dependent
mantle. Ice melt and sublimation are the main drivers of alcove growth,
rather than sediment erosion.

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