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Curiosity's Investigation at Vera Rubin Ridge

Authors :
Fraeman, A. A
Edgar, L. A
Grotzinger, J. P
Vasavada, A. R
Johnson, J. R
Wellington, D. F
Fox, V. K
Sun, V. Z
Hardgrove, C. J
Horgan, B. N
House, C. H
Johnson, S. S
Stack Morgan, K. M
Rampe, E. B
Thompson, L. M
Wiens, R. C
Williams, A. J
Publication Year :
2018
Publisher :
United States: NASA Center for Aerospace Information (CASI), 2018.

Abstract

The Curiosity rover is exploring Vera Rubin Ridge (VRR), a ~6.5 km long and ~200 m wide topographic feature trending northeast-southwest across Aeolis Mons (informally known as Mt. Sharp) (Fig 1). In orbital data, VRR is distinct from the underlying Murray formation due to its relative erosional resistance and greater exposure of bedrock. Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) orbital data show a hematite spectral signature over much of the ridge (Fig. 2). On the ground, Curiosity also observed hematite associated with the sedimentary rocks of the underlying Murray formation, although these detections are difficult to see with CRISM due to mixing with sand and dust.

Details

Language :
English
Database :
NASA Technical Reports
Publication Type :
Report
Accession number :
edsnas.20180004271
Document Type :
Report