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ReportsSurficial Deposits at Gusev Crater Along Spirit Rover Traverses
The 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.
1 Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, USA.
2 Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA. 3 Department of Astronomy, Space Sciences Building, Cornell University, Ithaca, NY 14853, USA. 4 NASA Ames/SETI Institute, Space Science Division, MS 245-3, Moffett Field, CA 94035, USA. 5 U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA. 6 Department of Geological Sciences, Arizona State University, Tempe, AZ 85287, USA. 7 New Mexico Museum of Natural History and Science, 1801 Mountain Road NW, Albuquerque, NM 87104, USA. 8 NASA Ames Research Center, Moffett Field, CA 94035, USA. 9 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. 10 U.S. Geological Survey, Flagstaff, AZ 86001, USA. 11 Department of Civil and Environmental Engineering and Geodetic Science, Ohio State University, Columbus, OH 43210, USA. 12 Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996, USA. 13 NASA Johnson Space Center, Houston, TX 77058, USA. 14 DLR Institute of Space Simulation, Linder Hoehe, D-51170, Cologne, Germany. 15 NASA Headquarters, 300 E Street S.W., Washington, DC 20560, USA. * To whom correspondence should be addressed. E-mail: grantj{at}nasm.si.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)