Lineated Valley Fill Surface Textures, Nilosyrtis Mensae, Mars: Comparison with Analagous Glacier Surface Textures in the Antarctic Dry Valleys

Details Lineated Valley Fill Surface Textures, Nilosyrtis Mensae, Mars: Comparison with Analagous Glacier Surface Textures in the Antarctic Dry Valleys Lineated Valley Fill Surface Textures, Nilosyrtis Mensae, Mars: Comparison with Analagous Glacier Surface Textures in the Antarctic Dry Valleys

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1245l&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1245

Physics

1

Scientific paper

We compare the lobate LVF feature observed in Nilosyrtis Mensae with the
Mullins Valley debris-covered glacier, located in the Antarctic Dry
Valleys. Cold-based glaciers in the hyper-arid, cold environments of the
ADV are considered to be physical analogs for martian valley-glacial
processes.

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