Mars: Periglacial Morphology and Implications for Future Landing Sites

At the Mars Phoenix landing site and in much of the Martian northern plains, there is ice-cemented ground beneath a layer of dry permafrost. Unlike most permafrost on Earth, though, this ice is not liquid at any time of year. However, in past epochs at higher obliquity the surface conditions during...

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Bibliographic Details
Main Authors: Schurmeier, Lauren, Heldmann, Jennifer L., Stoker, Carol, Davila, Alfonso, Wilhelm, Mary Beth, Marinova, Margarita, McKay, Christopher
Format: Other/Unknown Material
Language:unknown
Published: 2015
Subjects:
Ice
Online Access:http://hdl.handle.net/2060/20150023012