Equilibration Timescales for Ice Flow on Gemina Lingula Indicate Enhanced Flow at Low Temperatures

Details Equilibration Timescales for Ice Flow on Gemina Lingula Indicate Enhanced Flow at Low Temperatures Equilibration Timescales for Ice Flow on Gemina Lingula Indicate Enhanced Flow at Low Temperatures

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2272k&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2272

Computer Science

1

Scientific paper

With ice-flow enhancement comparable to that observed in Taylor Glacier,
Antarctica, equilibration timescales for flow in Gemina Lingula, North
Polar Layered Deposits are less than 5 million years, at basal
temperatures only modestly warmer than today.

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