Ice-Driven Degradation Styles in the Martian Mid-Latitudes: Constraints from Lobate Debris Aprons, Lineated Valley Fill, and Small Flow Lobes

Details Ice-Driven Degradation Styles in the Martian Mid-Latitudes: Constraints from Lobate Debris Aprons, Lineated Valley Fill, and Small Flow Lobes Ice-Driven Degradation Styles in the Martian Mid-Latitudes: Constraints from Lobate Debris Aprons, Lineated Valley Fill, and Small Flow Lobes

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1861c&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1861

Physics

8

Scientific paper

This investigation examines the geomorphic characteristics of lobate
debris aprons, lineated valley fill, and small flow lobes found on
crater rims and massifs in order to characterize emplacement styles for
ice-rich flows on Mars.

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