HR: 08:31h
AN: P31A-01 [Abstracts]
TI: Recent Results from the Mars Exploration Rover Spirit Mission
AU: * Squyres, S W
EM: squyres@astro.cornell.edu
AF: Cornell University, Dept. of Astronomy, Ithaca, NY 14853 United States
AB:
Since arriving at the Columbia Hills, the Spirit rover's primary area of geologic investigation has been the West Spur of
Husband Hill. Pancam images of West Spur rocks show morphology ranging from massive to finely layered. Microscopic Imager
images show the rocks to be clastic in nature, with a substantial range in grain sizes. Grains vary from rounded to angular.
Mini-TES data show little variability from one rock to the next, and the best fit to the IR spectral signature of the rocks
is dominated by basaltic glass. The chemistry revealed by the APXS is broadly basaltic in nature, but substantially enhanced
in P, S, Cl, and Br relative to plains rocks. Moessbauer data show that olivine is absent in West Spur rocks, and pyroxene
signatures are weak. Fe oxides and oxyhydroxides are present. We interpret the rocks of the West Spur to be aqueously altered basaltic materials of volcaniclastic or impact origin.
Since leaving the West Spur, Spirit has explored toward the northeast, higher onto Husband Hill. Loose rocks ("float") on
the north flank of the hill are dominated by another poorly sorted clastic lithology that contains olivine and that has
strikingly high abundances of Ti and P. Only a few bedrock outcrops have been identified on the main body of Husband Hill.
All of these examined to date consist of a coarse-grained clastic rock dominated by basaltic chemistry and cemented by
sulfate salts. Grain sizes range up to several mm, and sub-cm layering is present. Moessbauer data show pyroxene, olivine,
and a high abundance of magnetite in the basaltic component. APXS data are consistent with the rock being up to 20 percent
magnesium sulfate salts by mass, and microscopic images show a high degree of cementation by these salts.
DE: 6055 Surfaces and interiors
SC: Planetary Sciences [P]
MN: 2005 Joint Assembly