A Progression of Induration in Transverse Aeolian Ridges: Evidence for Ancient Aeolian Bedforms and Extensive Reworking in the Medusae Fossae Formation

Details A Progression of Induration in Transverse Aeolian Ridges: Evidence for Ancient Aeolian Bedforms and Extensive Reworking in the Medusae Fossae Formation A Progression of Induration in Transverse Aeolian Ridges: Evidence for Ancient Aeolian Bedforms and Extensive Reworking in the Medusae Fossae Formation

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1628k&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1628

Physics

Scientific paper

Evidence of degraded bedforms in the Medusae Fossae Formation suggests
that the deposit may undergo a recycling process whereby depositional
features are indurated to the point where they may be eroded again,
forming more depositional features.

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