Phoenix Landing Site Geomorphology: Surface Stability and Implications for the Martian Latitude-dependent Mantle

Details Phoenix Landing Site Geomorphology: Surface Stability and Implications for the Martian Latitude-dependent Mantle Phoenix Landing Site Geomorphology: Surface Stability and Implications for the Martian Latitude-dependent Mantle

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1625l&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

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Geomorphological observations of the Phoenix landing site suggest a
history for local permafrost recently dominated by excess ice removal
through sublimation, ongoing thermal contraction cracking, and limited
cryoturbation by wet or dry processes.

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