Temporary Ponding of Floodwater in Athabasca Vallis, Mars

Details Temporary Ponding of Floodwater in Athabasca Vallis, Mars Temporary Ponding of Floodwater in Athabasca Vallis, Mars

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1066b&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1066

Physics

1

Scientific paper

Examination of MOC and MOLA data from the Athabasca Vallis outflow
channel, Mars, shows similar elevations for two disparate paleo-flood
height indicators. This is best explained by temporary ponding of water
behind an impact crater in the channel.

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