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New Evidence Supporting an Ice-covered Lake in Gusev CraterThe morphology and setting of a groove in Gusev strongly supports the hypothesis of a lateral channel generated by meltwater flowing against an ice covered lake margin. The size of the groove and the slope of the bed independent of the topography of the crater are consistent with modest discharges. Additional information is contained in the original extended abstract.
Document ID
20020045685
Acquisition Source
Ames Research Center
Document Type
Conference Paper
Authors
Grin, E. A.
(NASA Ames Research Center Moffett Field, CA United States)
Fike, D.
(Scott Polar Research Inst. Cambridge, United Kingdom)
Cabrol, N. A.
(NASA Ames Research Center Moffett Field, CA United States)
Date Acquired
August 20, 2013
Publication Date
April 1, 2002
Publication Information
Publication: Lunar and Planetary Science XXXIII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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