Fluvial Discharge Rates of Martian Gullies: Slope Measurements from Stereo HiRISE Images and Numerical Modeling of Sediment Transport

Details Fluvial Discharge Rates of Martian Gullies: Slope Measurements from Stereo HiRISE Images and Numerical Modeling of Sediment Transport Fluvial Discharge Rates of Martian Gullies: Slope Measurements from Stereo HiRISE Images and Numerical Modeling of Sediment Transport

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1947p&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Physics

Scientific paper

Based on fluvial discharge and sediment transport theory from Kleinhans
[2005], groundwater is a plausible mechanism for forming gullies on Mars
if the supplying aquifer is permeable and ~10s of m thick. Our model
suggests gullies form rapidly (~h).

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