Regional Mid-Latitude Late Amazonian Valley Glaciers on Mars: Origin of Lineated Valley Fill and Implications for Recent Climate Change

Details Regional Mid-Latitude Late Amazonian Valley Glaciers on Mars: Origin of Lineated Valley Fill and Implications for Recent Climate Change Regional Mid-Latitude Late Amazonian Valley Glaciers on Mars: Origin of Lineated Valley Fill and Implications for Recent Climate Change

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1208h&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1208

Physics

Scientific paper

Evidence is presented that lineated valley fill in the Deuteronilus
mid-latitude region of Mars originated from snow and ice accumulation
and glacial flow during periods of high obliquity in the Amazonian.

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