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Superficial Deposits at Gusev Crater Along Spirit Rover TraversesThe Mars Exploration Rover Spirit has traversed a fairly flat, rock-strewn terrain whose surface is shaped primarily by impact events, although some of the landscape has been altered by eolian processes.Impacts ejected basaltic rocks that probably were part of locally formed lava flows from at least 10 meters depth.Some rocks have been textured and/or partially buried by windblown sediments less than 2 millimeters in diameter that concentrate within shallow, partially filled, circular impact depressions referred to as hollows.The terrain traversed during the 90-sol (martian solar day) nominal mission shows no evidence for an ancient lake in Gusev crater.
Document ID
20060009017
Acquisition Source
Johnson Space Center
Document Type
Reprint (Version printed in journal)
Authors
Grant, J. A.
(Smithsonian Institution Washington, DC, United States)
Arvidson, R.
(Washington Univ. Saint Louis, MO, United States)
Bell, J. F., III
(Cornell Univ. Ithaca, NY, United States)
Cabrol, N. A.
(NASA Ames Research Center Moffett Field, CA, United States)
Carr, M. H.
(Geological Survey Menlo Park, CA, United States)
Christensen, P.
(Arizona State Univ. Tempe, AZ, United States)
Crumpler, L.
(New Mexico Museum of Natural History and Science Albuquerque, NM, United States)
DesMarsais, D.
(NASA Ames Research Center Moffett Field, CA, United States)
Ehlmann, B. L.
(Washington Univ. Saint Louis, MO, United States)
Ming, Douglas W.
(NASA Johnson Space Center Houston, TX, United States)
Date Acquired
August 23, 2013
Publication Date
August 6, 2004
Publication Information
Publication: Science
Volume: 305
Subject Category
Geophysics
Funding Number(s)
WBS: WBS 390-30-AA
Distribution Limits
Public
Copyright
Other

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