The Geologic History of Terby Crater: Evidence for Lacustrine Deposition and Dissection by Ice

Details The Geologic History of Terby Crater: Evidence for Lacustrine Deposition and Dissection by Ice The Geologic History of Terby Crater: Evidence for Lacustrine Deposition and Dissection by Ice

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1863w&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1863

Physics

3

Scientific paper

The landforms in Terby Crater were likely deposited in a lacustrine
environment when the circum-Hellas region may have been occupied by a
body of water up to 3.6 km deep. The interior deposits were then
subsequently dissected and modified by ice.

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