The Spirit Rover's Athena Science Investigation at Gusev Crater, Mars
SPIRIT AT CUSEV CRATER RESEARCH ARTICLE The Spirit Rover's Athena Science Investigation at Gusev Crater, Mars S. W. Squyres,^* R. E. Arvidson,^ J. F. Bell III/ J. Bruckner,' N. A. Cabrol,'* W. Calvîn,= M. H. Carr,® P. R. Christensen/ B. C. Clark,® L Crumpler,® D. J. Des Marais,^" C. d'Uston,''^ T. Economou,^^ J. Farmer,^ W. Farrand," W. Folkner,^^ M. Colombek,^'* S. Corevan," J. A. Crant,^^ R. Creeley,'^ J. Crotzinger,^'^ L Haskin,^ K. E. Herkenhoff,^® S. Hvîid," J. Johnson,^® C. Klîngelhofer,^" A. Knoll,^^ C. Landis,^^ M. Lemmon,^' R. Li,^* M. B. Madsen,2= 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,' M. Sims,^° M. Smitli,'^ P. Smith,'^ L A. Soderblom,^® R. Sullivan,^ H. Wanke,' T. Wdowiak," M. Wolff,'^ A. Yen^'* The Mars Exploration Rover Spirit and its Atliena science payload liave been used to sediment carried by the water that cut investigate a landing site in Gusev crater. Gusev is hypothesized to be the site of a Ma'adim before it overflowed and exited former lake, but no clear evidence for lacustrine sedimentation has been found to through a gap in the northern rim of the date. Instead, the dominant lithology is basalt, and the dominant geologic processes are impact events and eolian transport. I^jany rocks exhibit coatings and other characteristics that may be evidence for minor aqueous alteration. Any lacustrine ^Department of Astronomy, Cornell University, Ithaca, NY 14853, USA. ^Department of Earth and sediments that may exist at this location within Gusev apparently have been buried Planetary Sciences, Washington University, St.
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