The Nature of the Transition from Lobate Debris Aprons to Lineated Valley Fill: Mamers Valles, Northern Arabia Terra-Deuteronilus Mensae Region on Mars

Details The Nature of the Transition from Lobate Debris Aprons to Lineated Valley Fill: Mamers Valles, Northern Arabia Terra-Deuteronilus Mensae Region on Mars The Nature of the Transition from Lobate Debris Aprons to Lineated Valley Fill: Mamers Valles, Northern Arabia Terra-Deuteronilus Mensae Region on Mars

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1323k&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1323

Physics

8

Scientific paper

Mamers Valles lobate debris aprons (LDA) form in alcoves, meet and flow
laterally to become lineated valley fill (LVF) suggesting a related mode
of origin: individual debris-covered glaciers creating larger glacial
landsystems.

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