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Topographic and Morphologic Evidence for Flooding of Ganymede's Resurfaced Terrains by Low-Viscosity Water-Ice LavasTopographic mapping in at least three distinct regions of Ganymede reveals that smooth terrains are flat and are topographically depressed. This and embayment relationships are consistent with volcanic resurfacing. Additional information is contained in the original extended abstract.
Document ID
Document Type
Conference Paper
McKinnon, W. B.
(Washington Univ. Saint Louis, MO United States)
Schenk, P. M.
(Lunar and Planetary Inst. Houston, TX United States)
Moore, J. M.
(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
Work of the US Gov. Public Use Permitted.

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IDRelationTitle20010044353Analytic PrimaryLunar and Planetary Science XXXII
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