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Pancam multispectral imaging results from the Opportunity rover at Meridiani Planum

Authors :
Bell, III, J.F.
Squyres, S.W.
Arvidson, R.E.
Arneson, H.M.
Bass, D.
Calvin, W.
Farrand, W.H.
Goetz, W.
Golombek, M.
Greeley, R.
Grotzinger, J.
Guinness, E.
Hayes, A.G.
Hubbard, M.Y.H.
Herkenhoff, K.E.
Johnson, M.J.
Johnson, J.R.
Joseph, J.
Kinch, K.M.
Lemmon, M.T.
Li, R.
Madsen, M.B.
Maki, J.N.
Malin, M.
McCartney, E.
McLennan, S.
McSween, Jr., H.Y.
Ming, D.W.
Morris, R.V.
Dobrea, E.Z. Noe
Parker, T.J.
Proton, J.
Rice, Jr., J.W.
Seelos, F.
Soderblom, J.M.
Soderblom, L.A.
Sohl-Dickstein, J.N.
Sullivan, R.J.
Weitz, C.M.
Wolff, M.J.
Source :
Science. December 3, 2004, Vol. 306 Issue 5702, p1703, 7 p.
Publication Year :
2004

Abstract

Panoramic Camera (Pancam) images from Meridiani Planum reveal a low-albedo, generally flat, and relatively rock-free surface. Within and around impact craters and fractures, laminated outcrop rocks with higher albedo are observed. Fine-grained materials include dark sand, bright ferric iron-rich dust, angular rock clasts, and millimeter-size spheroidal granules that are eroding out of the laminated rocks. Spectra of sand, clasts, and one dark plains rock are consistent with mafic silicates such as pyroxene and olivine. Spectra of both the spherules and the laminated outcrop materials indicate the presence of crystalline ferric oxides or oxyhydroxides. Atmospheric observations show a steady decline in dust opacity during the mission. Astronomical observations captured solar transits by Phobos and Deimos and time-lapse observations of sunsets.<br />On 24 January 2004 UTC, the Mars Exploration Rover Opportunity landed on Mars within the classical low-albedo Noachian terrain of Meridiani Planum. The landing region was previously identified in orbital [...]

Details

Language :
English
ISSN :
00368075
Volume :
306
Issue :
5702
Database :
Gale General OneFile
Journal :
Science
Publication Type :
Academic Journal
Accession number :
edsgcl.126195014