Ponding in Central Valles Marineris Due to Late-Stage Martian Outflow Channel Activity

Details Ponding in Central Valles Marineris Due to Late-Stage Martian Outflow Channel Activity Ponding in Central Valles Marineris Due to Late-Stage Martian Outflow Channel Activity

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1806h&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

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Scientific paper

Possible shoreline features in central Valles Marineris are consistently
close to the maximum regional ponding elevation and, with other
evidence, indicate the past presence of a lake which overflowed eastward
into channels and chaotic terrain.

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