Search Results - "Crumpler, L. S."

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    Erosion rates at the Mars Exploration Rover landing sites and long-term climate change on Mars by Golombek, M. P., Grant, J. A., Crumpler, L. S., Greeley, R., Arvidson, R. E., Bell III, J. F., Weitz, C. M., Sullivan, R., Christensen, P. R., Soderblom, L. A., Squyres, S. W.

    Published in Journal Of Geophysical Research (01-12-2006)
    “…Erosion rates derived from the Gusev cratered plains and the erosion of weak sulfates by saltating sand at Meridiani Planum are so slow that they argue that…”
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    Assessment of Mars Exploration Rover landing site predictions by Golombek, M. P, Arvidson, R. E, Bell, J. F, Christensen, P. R, Crisp, J. A, Crumpler, L. S, Ehlmann, B. L, Fergason, R. L, Grant, J. A, Greeley, R, Haldemann, A. F. C, Kass, D. M, Parker, T. J, Schofield, J. T, Squyres, S. W, Zurek, R. W

    Published in Nature (07-07-2005)
    “…Comprehensive analyses of remote sensing data during the three-year effort to select the Mars Exploration Rover landing sites at Gusev crater and at Meridiani…”
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    Crater gradation in Gusev crater and Meridiani Planum, Mars by Grant, J. A., Arvidson, R. E., Crumpler, L. S., Golombek, M. P., Hahn, B., Haldemann, A. F. C., Li, R., Soderblom, L. A., Squyres, S. W., Wright, S. P., Watters, W. A.

    Published in Journal of Geophysical Research - Planets (01-01-2006)
    “…The Mars Exploration Rovers investigated numerous craters in Gusev crater and Meridiani Planum during the first ∼400 sols of their missions. Craters vary in…”
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    Geology and MER target site characteristics along the southern rim of Isidis Planitia, Mars by Crumpler, L. S., Tanaka, K. L.

    Published in Journal of Geophysical Research - Planets (01-12-2003)
    “…The southern rim of the Isidis basin contains one of the highest densities of valley networks, several restricted paleolake basins, and the stratigraphically…”
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    The degradational history of Endeavour crater, Mars by Grant, J.A., Parker, T.J., Crumpler, L.S., Wilson, S.A., Golombek, M.P., Mittlefehldt, D.W.

    Published in Icarus (New York, N.Y. 1962) (01-12-2016)
    “…•Endeavour crater has a discontinuous 10–160m high rim, and is 200–500m deep.•Endeavour crater is mostly buried by 100–200m Burns Formation/Grasberg…”
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    Rock spectral classes observed by the Spirit Rover's Pancam on the Gusev Crater Plains and in the Columbia Hills by Farrand, W. H., Bell III, J. F., Johnson, J. R., Arvidson, R. E., Crumpler, L. S., Hurowitz, J. A., Schröder, C.

    Published in Journal of Geophysical Research - Planets (01-12-2008)
    “…This paper examines the ferrous and ferric iron mineralogy of rocks inferred from 246 visible/near‐infrared (430–1010 nm) multispectral observations made by…”
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    Relation of Major Volcanic Center Concentration on Venus to Global Tectonic Patterns by Crumpler, L. S., Head, James W., Aubele, Jayne C.

    “…Global analysis of NASA Magellan image data indicates that a major concentration of volcanic centers covering ∼40 percent of the surface of Venus occurs…”
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