Soil-like deposits observed by Sojourner, the Pathfinder rover

Journal of Geophysical Research E: Planets
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Abstract

Most of the soil-like materials at the Pathfinder landing site behave like moderately dense soils on Earth with friction angles near 34°-39° and are called cloddy deposits. Cloddy deposits appear to be poorly sorted with dust-sized to granule-sized mineral or rock grains; they may contain pebbles, small rock fragments, and clods. Thin deposits of porous, compressible drifts with friction angles near 26°-28° are also present. Drifts are fine grained. Cohesions of both types of deposits are small. There may be indurated soil-like deposits and/or coated or crusted rocks. Cloddy deposits may be fluvial sediments of the Ares-Tiu floods, but other origins, such as ejecta from nearby impact craters, should be considered. Drifts are probably dusts that settled from the Martian atmosphere. Remote-sensing signatures of the deposits inferred from rover observations are consistent with those observed from orbit and Earth.

Suggested Citation

Moore, H.J., Bickler, D.B., Crisp, J.A., Eisen, H.J., Gensler, J.A., Haldemann, A.F., Matijevic, J.R., Reid, L.K., Pavlics, F., 1999, Soil-like deposits observed by Sojourner, the Pathfinder rover: Journal of Geophysical Research E: Planets, v. 104, no. E4, p. 8729-8746, https://doi.org/10.1029/1998JE900005.

Publication type Article
Publication Subtype Journal Article
Title Soil-like deposits observed by Sojourner, the Pathfinder rover
Series title Journal of Geophysical Research E: Planets
DOI 10.1029/1998JE900005
Volume 104
Issue E4
Year Published 1999
Language English
Publisher American Geophysical Union
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Journal of Geophysical Research E: Planets
First page 8729
Last page 8746
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