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Spirit Mars Rover Mission: Overview and selected results from the northern Home Plate Winter Haven to the side of Scamander crater


Arvidson, RE and Bell III, JF and Bellutta, PH and Cabrol, NA and Catalano, JG and Cohen, J and Crumpler, LS and Des Marais, DJ and Estlin, TA and Farrand, WH and Gellert, R and Grant, JA and Greenberger, RN and Guinness, EA and Herkenhoff, KE and Herman, JA and Iagnemma, KD and Johnsn, JR and Klingelhofer, G and Li, R and Lichtenberg, KA and Maxwell, SA and Ming, DW and Morris, RV and Rice, MS and Ruff, SW and Shaw, A and Siebach, KL and de Souza, PA and Stroupe, AW and Squyres, SW and Sullivan, RJ and Talley, KP and Townsend, JA and Wang, A and Wright, JR and Yen, AS, Spirit Mars Rover Mission: Overview and selected results from the northern Home Plate Winter Haven to the side of Scamander crater, Journal of Geophysical Research-Space Physics, 115, (09/10) pp. EJJ. ISSN 0148-0227 (2010) [Refereed Article]

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Copyright Statement

Copyright 2010 American Geophysical Union

DOI: doi:10.1029/2010JE003633


This paper summarizes Spirit Rover operations in the Columbia Hills, Gusev crater, from sol 1410 (start of the third winter campaign) to sol 2169 (when extrication attempts from Troy stopped to winterize the vehicle) and provides an overview of key scientific results. The third winter campaign took advantage of parking on the northern slope of Home Plate to tilt the vehicle to track the sun and thus survive the winter season. With the onset of the spring season, Spirit began circumnavigating Home Plate on the way to volcanic constructs located to the south. Silica‐rich nodular rocks were discovered in the valley to the north of Home Plate. The inoperative right front wheel drive actuator made climbing soil‐covered slopes problematical and led to high slip conditions and extensive excavation of subsurface soils. This situation led to embedding of Spirit on the side of a shallow, 8 m wide crater in Troy, located in the valley to the west of Home Plate. Examination of the materials exposed during embedding showed that Spirit broke through a thin sulfate‐rich soil crust and became embedded in an underlying mix of sulfate and basaltic sands. The nature of the crust is consistent with dissolution and precipitation in the presence of soil water within a few centimeters of the surface. The observation that sulfate‐rich deposits in Troy and elsewhere in the Columbia Hills are just beneath the surface implies that these processes have operated on a continuing basis on Mars as landforms have been shaped by erosion and deposition.

Item Details

Item Type:Refereed Article
Research Division:Earth Sciences
Research Group:Geochemistry
Research Field:Exploration geochemistry
Objective Division:Expanding Knowledge
Objective Group:Expanding knowledge
Objective Field:Expanding knowledge in the earth sciences
UTAS Author:de Souza, PA (Professor Paulo de Souza Junior)
ID Code:77625
Year Published:2010
Web of Science® Times Cited:92
Deposited By:Information and Communication Technology
Deposited On:2012-05-14
Last Modified:2012-07-03

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