Large Hesperian Proglacial Lake in Schmidt Valley, Mars: Evidence for Marginal Pitted Sandar Deposits

Details Large Hesperian Proglacial Lake in Schmidt Valley, Mars: Evidence for Marginal Pitted Sandar Deposits Large Hesperian Proglacial Lake in Schmidt Valley, Mars: Evidence for Marginal Pitted Sandar Deposits

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1185d&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1185

Physics

2

Scientific paper

We provide evidence that the depressions and valleys found in the plain
that separates Cavi Angusti from Schmidt Valley at the South Pole of
Mars are indicative of a glacier/lake contact environment, yielding a
marginal pitted sandur.

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