Cryogenic Evaporite Formation at the Lewis Cliff, Antarctica: A Mars Analog Study

Details Cryogenic Evaporite Formation at the Lewis Cliff, Antarctica: A Mars Analog Study Cryogenic Evaporite Formation at the Lewis Cliff, Antarctica: A Mars Analog Study

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1044h&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1044

Physics

1

Scientific paper

Large layered evaporite deposits near the Lewis Cliff Ice Tongue in
Antarctica appear to have formed through periodic short-term cycling of
very small volumes of water. These cryogenic, low water/rock ratio
processes offer possible analogs for Martian evaporite formation events.

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