Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (I): Evidence for the Presence of Subsurface Ice

Details Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (I): Evidence for the Presence of Subsurface Ice Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (I): Evidence for the Presence of Subsurface Ice

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1273k&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

3

Scientific paper

Experimental impacts into ice form "ring-mold craters" (RMC) due to
spallation, in contrast to those in icy regolith and regolith; the
presence of RMC on lineated valley fill and lobate debris aprons suggest
the presence of an ice substrate there.

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