Linear Lobate Debris Aprons, Piedmont-like Lobes, and Crater Fill in the Acheron Fossae Graben Region, Mars: Evidence for Debris-covered Glacier Formation and Flow

Details Linear Lobate Debris Aprons, Piedmont-like Lobes, and Crater Fill in the Acheron Fossae Graben Region, Mars: Evidence for Debris-covered Glacier Formation and Flow Linear Lobate Debris Aprons, Piedmont-like Lobes, and Crater Fill in the Acheron Fossae Graben Region, Mars: Evidence for Debris-covered Glacier Formation and Flow

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1321d&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1321

Physics

1

Scientific paper

The graben of Acheron Fossae contain linear lobate debris aprons (LDA)
where slopes are low and lineated valley fill (LVF) and piedmont-like
lobes on steeper slopes; post-graben craters host LDAs on pole-facing
slopes.

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