Mars exploration rover geologic traverse by the spirit rover in the plains of Gusev crater, Mars

L.S. Crumpler; S. W. Squyres; R. E. Arvidson; J.F. Bell; D. Blaney; N.A. Cabrol; P. R. Christensen; D.J. DesMarais; J.D. Farmer; R. Fergason; M.P. Golombek; F.D. Grant; J. A. Grant; R. Greeley; B. Hahn; Kenneth E. Herkenhoff; J.A. Hurowitz; A.T. Knudson; G. A. Landis; R. Li; J. Maki; H.Y. McSween; D. W. Ming; J.E. Moersch; M.C. Payne; J.W. Rice; L. Richter; S. W. Ruff; M. Sims; S.D. Thompson; N. Tosca; A. Wang; P. Whelley; S.P. Wright; M.B. Wyatt

doi:10.1130/G21673.1

Mars exploration rover geologic traverse by the spirit rover in the plains of Gusev crater, Mars

Geology

By: L.S. Crumpler, S. W. Squyres, R. E. Arvidson, J.F. Bell, D. Blaney, N.A. Cabrol, P. R. Christensen, D.J. DesMarais, J.D. Farmer, R. Fergason, M.P. Golombek, F.D. Grant, J. A. Grant, R. Greeley, B. Hahn, Kenneth E. Herkenhoff, J.A. Hurowitz, A.T. Knudson, G. A. Landis, R. Li, J. Maki, H.Y. McSween, D. W. Ming, J.E. Moersch, M.C. Payne, J.W. Rice, L. Richter, S. W. Ruff, M. Sims, S.D. Thompson, N. Tosca, A. Wang, P. Whelley, S.P. Wright, and M.B. Wyatt

https://doi.org/10.1130/G21673.1

Links

More information: Publisher Index Page (via DOI)
Download citation as: RIS | Dublin Core

Abstract

The Spirit rover completed a 2.5 km traverse across gently sloping plains on the floor of Gusev crater from its location on the outer rim of Bonneville crater to the lower slopes of the Columbia Hills, Mars. Using the Athena suite of instruments in a transect approach, a systematic series of overlapping panoramic mosaics, remote sensing observations, surface analyses, and trenching operations documented the lateral variations in landforms, geologic materials, and chemistry of the surface throughout the traverse, demonstrating the ability to apply the techniques of field geology by remote rover operations. Textures and shapes of rocks within the plains are consistent with derivation from impact excavation and mixing of the upper few meters of basaltic lavas. The contact between surrounding plains and crater ejecta is generally abrupt and marked by increases in clast abundance and decimeter-scale steps in relief. Basaltic materials of the plains overlie less indurated and more altered rock types at a time-stratigraphic contact between the plains and Columbia Hills that occurs over a distance of one to two meters. This implies that regional geologic contacts are well preserved and that Earth-like field geologic mapping will be possible on Mars despite eons of overturn by small impacts.

Additional publication details
Publication type	Article
Publication Subtype	Journal Article
Title	Mars exploration rover geologic traverse by the spirit rover in the plains of Gusev crater, Mars
Series title	Geology
DOI	10.1130/G21673.1
Volume	33
Issue	10
Year Published	2005
Language	English
Publisher	The Geological Society of America
Contributing office(s)	Astrogeology Science Center
Description	4 p.
Larger Work Type	Article
Larger Work Subtype	Journal Article
Larger Work Title	Geology
First page	809
Last page	812
Other Geospatial	Gusev Crater; Mars
Google Analytic Metrics	Metrics page