Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/16849
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Overview of the Spirit Mars Exploration Rover Mission to Gusev Crater: Landing site to Backstay Rock in the Columbia Hills
Authors: Arvidson, Raymond E
Squyres, Steven W
Anderson, Robert C
Bell, III James F
Blaney, Diana
Brueckner, Johannes
Cabrol, Nathalie A
Calvin, Wendy M
Carr, Michael H
Christensen, Philip R
Clark, Benton C
Crumpler, Larry S
DesMarais, David J
d'Uston, Claude
Schröder, Christian
Contact Email: christian.schroeder@stir.ac.uk
Keywords: Gusev crater
Mars Exploration Rovers
Spirit rover
Issue Date: Feb-2006
Publisher: Wiley-Blackwell for the American Geophysical Union
Citation: Arvidson RE, Squyres SW, Anderson RC, Bell III JF, Blaney D, Brueckner J, Cabrol NA, Calvin WM, Carr MH, Christensen PR, Clark BC, Crumpler LS, DesMarais DJ, d'Uston C & Schröder C (2006) Overview of the Spirit Mars Exploration Rover Mission to Gusev Crater: Landing site to Backstay Rock in the Columbia Hills, Journal of Geophysical Research: Planets, 111 (E2), Art. No.: S01.
Abstract: Spirit landed on the floor of Gusev Crater and conducted initial operations on soil-covered, rock-strewn cratered plains underlain by olivine-bearing basalts. Plains surface rocks are covered by wind-blown dust and show evidence for surface enrichment of soluble species as vein and void-filling materials and coatings. The surface enrichment is the result of a minor amount of transport and deposition by aqueous processes. Layered granular deposits were discovered in the Columbia Hills, with outcrops that tend to dip conformably with the topography. The granular rocks are interpreted to be volcanic ash and/or impact ejecta deposits that have been modified by aqueous fluids during and/or after emplacement. Soils consist of basaltic deposits that are weakly cohesive, relatively poorly sorted, and covered by a veneer of wind-blown dust. The soils have been homogenized by wind transport over at least the several kilometer length scale traversed by the rover. Mobilization of soluble species has occurred within at least two soil deposits examined. The presence of monolayers of coarse sand on wind-blown bedforms, together with even spacing of granule-sized surface clasts, suggests that some of the soil surfaces encountered by Spirit have not been modified by wind for some time. On the other hand, dust deposits on the surface and rover deck have changed during the course of the mission. Detection of dust devils, monitoring of the dust opacity and lower boundary layer, and coordinated experiments with orbiters provided new insights into atmosphere-surface dynamics.
Type: Journal Article
URI: http://hdl.handle.net/1893/16849
DOI Link: http://dx.doi.org/10.1029/2005JE002499
Rights: The publisher does not allow this work to be made publicly available in this Repository. Please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study.
Notes: Additional co-authors: T. Economou, J. Farmer, W. H. Farrand, W. Folkner, M. Golombek, S. Gorevan, J. A. Grant, R. Greeley, J. Grotzinger, E. Guinness, B. C. Hahn, L. Haskin, K. E. Herkenhoff, J. A. Hurowitz, S. Hviid, J. R. Johnson, G. Klingelhöfer, A. H. Knoll, G. Landis, C. Leff, M. Lemmon, R. Li, M. B. Madsen, M. C. Malin, S. M. McLennan, H. Y. McSween, D. W. Ming, J. Moersch, R. V. Morris, T. Parker, J. W. Rice Jr., L. Richter, R. Rieder, D. S. Rodionov, M. Sims, M. Smith, P. Smith, L. A. Soderblom, R. Sullivan, S. D. Thompson, N. J. Tosca, A. Wang, H. Wnke, J. Ward, T. Wdowiak, M. Wolff, A. Yen
Affiliation: Washington University In Saint Louis
Cornell University
California Institute of Technology
Cornell University
California Institute of Technology
Max Planck Institute of Chemistry
National Aeronautics and Space Administration (NASA)
University of Nevada, Reno
U.S. Geological Survey
Arizona State University
Lockheed Martin Corporation
New Mexico Museum of Natural History and Science
National Aeronautics and Space Administration (NASA)
Centre d’Etude Spatiale des Rayonnements (CESR)
Biological and Environmental Sciences

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