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MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE

By Introduction The Phoenix L

Abstract

high northern latitudes of Mars and verified the presence of shallow subsurface water ice. This subsurface ice, discovered by the Gamma Ray and Neutron Spectrometer Suite poleward of about 55 ◦ latitude on both hemispheres [1, 2, 3], represent

Year: 2011
OAI identifier: oai:CiteSeerX.psu:10.1.1.192.6867
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