Lobate Debris Aprons Surrounding Mesa Clusters North of Ismeniae Fossae, Mars: Characteristics and Transition to Lineated Valley Fill

Details Lobate Debris Aprons Surrounding Mesa Clusters North of Ismeniae Fossae, Mars: Characteristics and Transition to Lineated Valley Fill Lobate Debris Aprons Surrounding Mesa Clusters North of Ismeniae Fossae, Mars: Characteristics and Transition to Lineated Valley Fill

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1186n&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1186

Physics

3

Scientific paper

Lobate debris aprons examined in new high resolution images show
evidence for origin in alcoves as debris-covered glaciers and merging to
form lineated valley fill. These deposits suggest periods of glaciation
in the Amazonian.

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