Mid-Latitude Glacial Modification of Moreux Crater (44°E, 42°N; 135 km): Evidence for Polythermal Glaciation Related to Impact-induced Enhanced Thermal Gradients

Details Mid-Latitude Glacial Modification of Moreux Crater (44°E, 42°N; 135 km): Evidence for Polythermal Glaciation Related to Impact-induced Enhanced Thermal Gradients Mid-Latitude Glacial Modification of Moreux Crater (44°E, 42°N; 135 km): Evidence for Polythermal Glaciation Related to Impact-induced Enhanced Thermal Gradients

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1425m&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1425

Physics

1

Scientific paper

Most northern mid-latitude glacial deposits are cold based. Wet-based
glacial features are observed in Moreux crater, interpreted as a local
thermal anomaly in the northern mid-latitude Amazonian cold polar desert
thermal environment.

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