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

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

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1127h&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1127

Physics

10

Scientific paper

Analysis of the northern mid-latitudes (30°-50°N) reveals
widespread lobate debris aprons and lineated valley fill that form as
deposits of debris-covered glaciers and valley glaciers in the Amazonian
during high-obliquity conditions.

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