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Recent aeolian erosion and deposition in the north polar plateau of Mars


J.A.P. Rodriguez1,2, Kenneth L. Tanaka3, Yves Langevin4, Mary Bourke2,5, Jeffrey Kargel6, Phil Christensen7, and Sho Sasaki1

1National Astronomical Observatory, Mizusawa, Japan
2Planetary Science Institute, Tucson, Arizona, USA, alexis@psi.edu
3Astrogeology Team, U.S. Geological Survey, Flagstaff, Arizona, USA
4Institut d'Astrophysique Spatiale, CNRS / Univ. Paris Sud, France
5Oxford University Center for the Environment, University of Oxford, United Kingdom
6Department of Hydrology and Water Resources, University of Arizona, USA
7Department of Geological Science, Arizona State University, Arizona, USA

Citation: Mars 3, 29-41, 2007; doi:10.1555/mars.2007.0003

History: Submitted: December 8, 2006; Reviewed: March 13, 2007; Resubmitted: August 24, 2007; Accepted: October 3, 2007; Published: December 3, 2007

Summary: We have identified extensive dark regions in the north polar plateau of Mars, which are largely free of surface water-ice. We propose that represent zones of recent sedimentary accumulation.

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Last Updated: July 11, 2008
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