Cold-based Glaciers in the Western Dry Valleys of Antarctica: Terrestrial Landforms and Martian Analogs

Details Cold-based Glaciers in the Western Dry Valleys of Antarctica: Terrestrial Landforms and Martian Analogs Cold-based Glaciers in the Western Dry Valleys of Antarctica: Terrestrial Landforms and Martian Analogs

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003mars.conf.3087h&link_type=abstract

Sixth International Conference on Mars, July 20-25 2003, Pasadena, California, abstract no.3087

Physics

1

Scientific paper

A lobate deposit on Western Arsia Mons is analogous to cold-based
glacier deposits in the Dry Valleys of Antarctica (ridged facies and
drop moraines; knobby facies and sublimation tills; smooth facies and
rock glaciers).

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