Seasonally Active Dune Slipface Avalanches on Mars: Evidence for a Wind-Related Origin

Details Seasonally Active Dune Slipface Avalanches on Mars: Evidence for a Wind-Related Origin Seasonally Active Dune Slipface Avalanches on Mars: Evidence for a Wind-Related Origin

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1631h&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1631

Physics

Scientific paper

The origin of slipface avalanches on some martian dunes has been
previously attributed to spring CO_2 sublimation. However, we show that
the timing, morphology, and orientations of the features support an
aeolian origin in mid- to late summer.

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