Shifting sands on Mars: insights from tropical intra-crater dunes

ABSTRACT Evidence for sand motion is found in repeated observations of sand dunes at three sites in the Martian tropics by the High Resolution Imaging Science Experiment on Mars Reconnaissance Orbiter. An eroding outcrop of layered sediments is identified as a possible source of the sand in Pasteur...

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Published in:Earth surface processes and landforms Vol. 38; no. 4; pp. 407 - 412
Main Authors: Geissler, Paul E., Stantzos, Nicholas W., Bridges, Nathan T., Bourke, Mary C., Silvestro, Simone, Fenton, Lori K.
Format: Journal Article
Language:English
Published: Chichester Blackwell Publishing Ltd 30-03-2013
Wiley
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Summary:ABSTRACT Evidence for sand motion is found in repeated observations of sand dunes at three sites in the Martian tropics by the High Resolution Imaging Science Experiment on Mars Reconnaissance Orbiter. An eroding outcrop of layered sediments is identified as a possible source of the sand in Pasteur crater. Ancient layered sediments in Becquerel crater are actively being carved into flutes and yardangs by the blowing sands. Dunes in an un‐named crater in Meridiani near the Mars Exploration Rover Opportunity landing site advanced as much as 50 cm over an interval of one Martian year. Copyright © 2012 John Wiley & Sons, Ltd.
Bibliography:istex:5CD39A128BF25774E87E8A897A1CF73C6E781B42
ark:/67375/WNG-XGTQTFBS-8
ArticleID:ESP3331
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0197-9337
1096-9837
DOI:10.1002/esp.3331