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

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], represents

Bibliographic Details
Main Author: Introduction The Phoenix L
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
permafrost
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867
http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf
Description
Summary: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], represents

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