Search Results - "GOLOMBEK, M. P"

Present‐Day Mars' Seismicity Predicted From 3‐D Thermal Evolution Models of Interior Dynamics by Plesa, A.‐C., Knapmeyer, M., Golombek, M. P., Breuer, D., Grott, M., Kawamura, T., Lognonné, P., Tosi, N., Weber, R. C.

“…The Interior Exploration using Seismic Investigations, Geodesy and Heat Transport mission, to be launched in 2018, will perform a comprehensive geophysical…”
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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.

“…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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Two Years at Meridiani Planum: Results from the Opportunity Rover by Squyres, S. W., Knoll, A. H., Arvidson, R. E., Clark, B. C., Grotzinger, J. P., Jolliff, B. L., McLennan, S. M., Tosca, N., Bell, J. F., Calvin, W. M., Farrand, W. H., Glotch, T. D., Golombek, M. P., Herkenhoff, K. E., Johnson, J. R., Klingelhöfer, G., McSween, H. Y., Yen, A. S.

“…The Mars Exploration Rover Opportunity has spent more than 2 years exploring Meridiani Planum, traveling ~8 kilometers and detecting features that reveal…”
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Small crater modification on Meridiani Planum and implications for erosion rates and climate change on Mars by Golombek, M. P., Warner, N. H., Ganti, V., Lamb, M. P., Parker, T. J., Fergason, R. L., Sullivan, R.

“…A morphometric and morphologic catalog of ~100 small craters imaged by the Opportunity rover over the 33.5 km traverse between Eagle and Endeavour craters on…”
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Rock Size‐Frequency Distributions at the InSight Landing Site, Mars by Golombek, M. P., Trussell, A., Williams, N., Charalambous, C., Abarca, H., Warner, N. H., Deahn, M., Trautman, M., Crocco, R., Grant, J. A., Hauber, E., Deen, R.

“…Rocks around the InSight lander were measured in lander orthoimages of the near field (<10 m), in panoramas of the far field (<40 m), and in a high‐resolution…”
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Localization and Physical Properties Experiments Conducted by Spirit at Gusev Crater by Arvidson, R. E., Anderson, R. C., Bartlett, P., Bell, J. F., Blaney, D., Christensen, P. R., Chu, P., Crumpler, L., Davis, K., Ehlmann, B. L., Fergason, R., Golombek, M. P., Gorevan, S., Grant, J. A., Greeley, R., Guinness, E. A., Haldemann, A. F. C., Herkenhoff, K., Johnson, J., Landis, G., Li, R., Lindemann, R., McSween, H., Ming, D. W., Myrick, T., Richter, L., Seelos, F. P., Squyres, S. W., Sullivan, R. J., Wang, A., Wilson, J.

“…The precise location and relative elevation of Spirit during its traverses from the Columbia Memorial station to Bonneville crater were determined with…”
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An Impact Crater Origin for the InSight Landing Site at Homestead Hollow, Mars: Implications for Near Surface Stratigraphy, Surface Processes, and Erosion Rates by Banks, Maria Elaine, Warner, N H, Grant, J A, Wilson, S A, Golombek, Matthew P, DeMott, A, Charalambous, C, Hauber, E, Ansan, V, Weitz, C, Pike, T, Williams, N, Banks, M E, Calef, F, Baker, M, Kopp, M, Deahn, M, Lethcoe, H, Berger, L

“…The InSight mission to Mars landed within Homestead hollow on an Early Amazonian lavaplain. The hollow is a 27‐m‐diameter, 0.3‐m‐deep quasi‐circular depression…”
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Finding SEIS North on Mars: Comparisons Between SEIS Sundial, Inertial and Imaging Measurements and Consequences for Seismic Analysis by Savoie, D., Richard, A., Goutaudier, M., Lognonné, P., Hurst, K. J., Maki, J. N., Golombek, M. P., van Driel, M., Clinton, J., Stutzmann, E., Mimoun, D., Banerdt, W. B., Williams, N. R.

“…In this paper, we present the results obtained in the determination of the true north direction on Mars by using a gnomon on the InSight mission and compare…”
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Geology of the Gusev cratered plains from the Spirit rover transverse by Golombek, M. P., Crumpler, L. S., Grant, J. A., Greeley, R., Cabrol, N. A., Parker, T. J., Rice Jr, J. W., Ward, J. G., Arvidson, R. E., Moersch, J. E., Fergason, R. L., Christensen, P. R., Castaño, A., Castaño, R., Haldemann, A. F. C., Li, R., Bell III, J. F., Squyres, S. W.

“…The cratered plains of Gusev traversed by Spirit are generally low‐relief rocky plains dominated by impact and eolian processes. Ubiquitous shallow,…”
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Size-frequency distributions of rocks on the northern plains of Mars with special reference to Phoenix landing surfaces by Golombek, M. P., Huertas, A., Marlow, J., McGrane, B., Klein, C., Martinez, M., Arvidson, R. E., Heet, T., Barry, L., Seelos, K., Adams, D., Li, W., Matijevic, J. R., Parker, T., Sizemore, H. G., Mellon, M., McEwen, A. S., Tamppari, L. K., Cheng, Y.

“…The size‐frequency distributions of rocks >1.5 m diameter fully resolvable in High Resolution Imaging Science Experiment (HiRISE) images of the northern plains…”
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Rock size-frequency distributions on Mars and implications for Mars Exploration Rover landing safety and operations by Golombek, M. P., Haldemann, A. F. C., Forsberg-Taylor, N. K., DiMaggio, E. N., Schroeder, R. D., Jakosky, B. M., Mellon, M. T., Matijevic, J. R.

“…The cumulative fractional area covered by rocks versus diameter measured at the Pathfinder site was predicted by a rock distribution model that follows simple…”
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Erosion rates on Mars and implications for climate change: Constraints from the Pathfinder landing site by Golombek, M. P., Bridges, N. T.

“…The observation that the Mars Pathfinder landing site looks very similar to its appearance after it was deposited by catastrophic floods around 1.8–3.5 Ga…”
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Localization and Physical Property Experiments Conducted by Opportunity at Meridiani Planum by Arvidson, R. E., Anderson, R. C., Bartlett, P., Bell, J. F., Christensen, P. R., Chu, P., Davis, K., Ehlmann, B. L., Golombek, M. P., Gorevan, S., Guinness, E. A., Haldemann, A. F. C., Herkenhoff, K. E., Landis, G., Li, R., Lindemann, R., Ming, D. W., Myrick, T., Parker, T., Richter, L., Seelos, F. P., Soderblom, L. A., Squyres, S. W., Sullivan, R. J., Wilson, J.

“…The location of the Opportunity landing site was determined to better than 10-m absolute accuracy from analyses of radio tracking data. We determined Rover…”
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Distribution of rocks on the Gusev Plains and on Husband Hill, Mars by Grant, J. A., Wilson, S. A., Ruff, S. W., Golombek, M. P., Koestler, D. L.

“…The population of rocks larger than 15 cm in diameter was measured at 36 locations imaged by the Spirit rover over ∼ 4 km of the traverse across the Gusev…”
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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

“…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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Mineralogic and compositional properties of Martian soil and dust: Results from Mars Pathfinder by Bell, J. F., McSween, H. Y., Crisp, J. A., Morris, R. V., Murchie, S. L., Bridges, N. T., Johnson, J. R., Britt, D. T., Golombek, M. P., Moore, H. J., Ghosh, A., Bishop, J. L., Anderson, R. C., Brückner, J., Economou, T., Greenwood, J. P., Gunnlaugsson, H. P., Hargraves, R. M., Hviid, S., Knudsen, J. M., Madsen, M. B., Reid, R., Rieder, R., Soderblom, L.

“…Mars Pathfinder obtained multispectral, elemental, magnetic, and physical measurements of soil and dust at the Sagan Memorial Station during the course of its…”
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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.

“…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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Wind-Related Processes Detected by the Spirit Rover at Gusev Crater, Mars by Greeley, R., Squyres, S. W., Arvidson, R. E., Bartlett, P., Bell, J. F., Blaney, D., Cabrol, N. A., Farmer, J., Farrand, B., Golombek, M. P., Gorevan, S. P., Grant, J. A., Haldemann, A. F. C., Herkenhoff, K. E., Johnson, J., Landis, G., Madsen, M. B., McLennan, S. M., Moersch, J., Rice, J. W., Richter, L., Ruff, S., Sullivan, R. J., Thompson, S. D., Wang, A., Weitz, C. M., Whelley, P., Athena Science Team

“…Wind-abraded rocks, ripples, drifts, and other deposits of windblown sediments are seen at the Columbia Memorial Station where the Spirit rover landed…”
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Veneers, rinds, and fracture fills: Relatively late alteration of sedimentary rocks at Meridiani Planum, Mars by Knoll, Andrew H., Jolliff, Brad L., Farrand, William H., Bell III, James F., Clark, Benton C., Gellert, Ralf, Golombek, M. P., Grotzinger, John P., Herkenhoff, Kenneth E., Johnson, Jeffrey R., McLennan, Scott M., Morris, Richard, Squyres, Steven W., Sullivan, Robert, Tosca, Nicholas J., Yen, Albert, Learner, Zoe

“…Veneers and thicker rinds that coat outcrop surfaces and partially cemented fracture fills formed perpendicular to bedding document relatively late stage…”
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Near Surface Stratigraphy and Regolith Production in Southwestern Elysium Planitia, Mars: Implications for Hesperian-Amazonian Terrains and the InSight Lander Mission by Warner, N. H., Golombek, M. P., Sweeney, J., Fergason, R., Kirk, R., Schwartz, C.

“…The presence of rocks in the ejecta of craters at the InSight landing site in southwestern Elysium Planitia indicates a strong, rock-producing unit at depth. A…”
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