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Science 3 December 2004:
Vol. 306. no. 5702, pp. 1730 - 1733
DOI: 10.1126/science.1104211

Reports

Localization and Physical Property Experiments Conducted by Opportunity at Meridiani Planum

R. E. Arvidson,1* R. C. Anderson,2 P. Bartlett,3 J. F. Bell, III,4 P. R. Christensen,5 P. Chu,3 K. Davis,3 B. L. Ehlmann,1 M. P. Golombek,2 S. Gorevan,3 E. A. Guinness,1 A. F. C. Haldemann,2 K. E. Herkenhoff,6 G. Landis,7 R. Li,8 R. Lindemann,2 D. W. Ming,9 T. Myrick,3 T. Parker,2 L. Richter,10 F. P. Seelos, IV,1 L. A. Soderblom,6 S. W. Squyres,4 R. J. Sullivan,4 J. Wilson3

The location of the Opportunity landing site was determined to better than 10-m absolute accuracy from analyses of radio tracking data. We determined Rover locations during traverses with an error as small as several centimeters using engineering telemetry and overlapping images. Topographic profiles generated from rover data show that the plains are very smooth from meter- to centimeter-length scales, consistent with analyses of orbital observations. Solar cell output decreased because of the deposition of airborne dust on the panels. The lack of dust-covered surfaces on Meridiani Planum indicates that high velocity winds must remove this material on a continuing basis. The low mechanical strength of the evaporitic rocks as determined from grinding experiments, and the abundance of coarse-grained surface particles argue for differential erosion of Meridiani Planum.

1 Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA.
2 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
3 Honeybee Robotics, 204 Elizabeth Street, New York, NY 10012, USA.
4 Department of Astronomy, Space Sciences Building, Cornell University, Ithaca, NY 14853, USA.
5 Department of Geological Sciences, Arizona State University, Tempe, AZ 85287, USA.
6 U.S. Geological Survey, Flagstaff, AZ 86001, USA.
7 NASA Glenn Research Center, Cleveland, OH 44135, USA.
8 Department of Civil and Environmental Engineering and Geodetic Science, The Ohio State University, Columbus, OH 43210, USA.
9 NASA Johnson Space Center, Houston, TX 77058, USA.
10 Deutsches Zentrum für Luft und Raumfahrt, Institut für Raumsimulation, Linder Höhe, Köln, D-51170, Germany.

* To whom correspondence should be addressed. E-mail: arvidson{at}wunder.wustl.edu

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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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In Situ Evidence for an Ancient Aqueous Environment at Meridiani Planum, Mars.
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Evidence from Opportunity's Microscopic Imager for Water on Meridiani Planum.
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Mineralogy at Meridiani Planum from the Mini-TES Experiment on the Opportunity Rover.
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