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Snow and Ice Melt Flow Features on Devon Island, Nunavut, Arctic Canada as Possible Analogs for Recent Slope Flow Features on MarsBased on morphologic and contextual analogs from Devon Island, Arctic Canada, the recent martian slope flow features reported by Malin and Edgett are reinterpreted as being due not necessarily to groundwater seepage but possibly to snow or ice melt. Additional information is contained in the original extended abstract.
Document ID
20010044414
Document Type
Conference Paper
Authors
Lee, Pascal
(Search for Extraterrestrial Intelligence Inst. Moffett Field, CA United States)
Cockell, Charles S.
(British Antarctic Survey Cambridge, United Kingdom)
Marinova, Margarita M.
(Massachusetts Inst. of Tech. Cambridge, MA United States)
McKay, Christopher P.
(Arizona Univ. Tucson, AZ United States)
Rice, James W., Jr.
(NASA Ames Research Center Moffett Field, CA United States)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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