Volumetric Estimates of Amazonian Lobate Debris Aprons (LDA) in the Mid-Latitudes of Mars: Support for the Presence of Significant Water-Ice

Details Volumetric Estimates of Amazonian Lobate Debris Aprons (LDA) in the Mid-Latitudes of Mars: Support for the Presence of Significant Water-Ice Volumetric Estimates of Amazonian Lobate Debris Aprons (LDA) in the Mid-Latitudes of Mars: Support for the Presence of Significant Water-Ice

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1652o&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

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Lobate debris apron morphometric/morphologic analyses indicate that
models of origin as simple talus debris aprons and pore-ice assisted
debris flow are unlikely; our data support a debris-covered glacier
origin and significant volumes of subsurface ice.

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