Origin of Aeolis Mensae, Mars, Fretted Terrain in a Thick Sedimentary Deposit

Details Origin of Aeolis Mensae, Mars, Fretted Terrain in a Thick Sedimentary Deposit Origin of Aeolis Mensae, Mars, Fretted Terrain in a Thick Sedimentary Deposit

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003mars.conf.3092i&link_type=abstract

Sixth International Conference on Mars, July 20-25 2003, Pasadena, California, abstract no.3092

Physics

Scientific paper

The boulder-free slopes, lack of surface flow paths, abrupt steepening
of valley longitudinal profiles, and layered stratigraphy suggest that
Aeolis Mensae fretted terrain formed primarily by aeolian erosion and
mass wasting of a sedimentary deposit.

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