Northern Mid-Latitude Glaciation in the Amazonian Period of Mars: Global-Scale Debris-covered Glacier and Valley Glacier Deposits in the 30°-50°N Latitude Band

Details Northern Mid-Latitude Glaciation in the Amazonian Period of Mars: Global-Scale Debris-covered Glacier and Valley Glacier Deposits in the 30°-50°N Latitude Band Northern Mid-Latitude Glaciation in the Amazonian Period of Mars: Global-Scale Debris-covered Glacier and Valley Glacier Deposits in the 30°-50°N Latitude Band

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3117h&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3117

Physics

Scientific paper

Widespread Late Amazonian northern mid-latitude lineated valley fill and
lobate debris aprons are interpreted as integrated glacial valley
landsystem remnants that were active following the formation of tropical
mountain glaciers at high obliquity.

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