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Wrinkle ridges in the floor material of Kasei Valles, Mars: Nature and originWrinkle ridges on Mars occur almost exclusively in smooth plains material referred to as ridged plains. One of the largest contiguous units of ridged plains occurs on Lunae Planum on the eastern flank of the Tharsis rise. The eastern, western, and northern margins of the ridged plains of Lunae Planum suffered extensive erosion in early Amazonian channel-forming events. The most dramatic example of erosion in early Amazonian plains is in Kasei Valles. The nature an origin of the wrinkle ridges in the floor material of Kasei Valles are discussed.
Document ID
19920001737
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Watters, Thomas R.
(National Air and Space Museum Washington, DC, United States)
Craddock, Robert A.
(National Air and Space Museum Washington, DC, United States)
Date Acquired
September 6, 2013
Publication Date
June 1, 1991
Publication Information
Publication: NASA, Washington, Reports of Planetary Geology and Geophysics Program, 1990
Subject Category
Lunar And Planetary Exploration
Meeting Information
Meeting: Lunar and Planetary Science Conference
Location: Houston, TX
Country: United States
Start Date: March 18, 1991
End Date: March 22, 1991
Accession Number
92N10955
Funding Number(s)
CONTRACT_GRANT: NAGW-1172
CONTRACT_GRANT: NAGW-1780
CONTRACT_GRANT: NAGW-940
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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