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Overview of the Mars Pathfinder Mission and Assessment of Landing Site Predictions

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dc.contributor.author Golombek, M. P. en_US
dc.contributor.author Cook, R. A. en_US
dc.contributor.author Economou, T. en_US
dc.contributor.author Folkner, W. M. en_US
dc.contributor.author Haldemann, A. F. C. en_US
dc.contributor.author Kellemeyn, P. H. en_US
dc.contributor.author Knudsen, J. M. en_US
dc.contributor.author Manning, R. M. en_US
dc.contributor.author Moore, H. J. en_US
dc.contributor.author Parker, T. J. en_US
dc.contributor.author Rieder, R. en_US
dc.contributor.author Schofield, J. T. en_US
dc.contributor.author Smith, P. H. en_US
dc.contributor.author Vaughan, R. M. en_US
dc.date.accessioned 2004-09-27T17:16:06Z
dc.date.available 2004-09-27T17:16:06Z
dc.date.issued 1997-10 en_US
dc.identifier.citation USA en_US
dc.identifier.clearanceno 97-1349 en_US
dc.identifier.uri http://hdl.handle.net/2014/22815
dc.description.abstract Data retuned by Mars Pathfinder indicates some rocks may be high in silica implying deferentiated parent materials. Rounded pebbles and cobbles and a possible conglomerate suggest fluvial processes that imply liquid water in equilibrium with the atmosphere and thus a warmer and weter past. en_US
dc.format.extent 1000968 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Mars Pathfinder en_US
dc.title Overview of the Mars Pathfinder Mission and Assessment of Landing Site Predictions en_US


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