"Water Tracks" in the McMurdo Dry Valleys, Antarctica: A Permafrost-Based Hydrological System Supporting Complex Biological and Geochemical Processes in a Mars-Analog Environment

Details "Water Tracks" in the McMurdo Dry Valleys, Antarctica: A Permafrost-Based Hydrological System Supporting Complex Biological and Geochemical Processes in a Mars-Analog Environment "Water Tracks" in the McMurdo Dry Valleys, Antarctica: A Permafrost-Based Hydrological System Supporting Complex Biological and Geochemical Processes in a Mars-Analog Environment

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1210l&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1210

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Scientific paper

Water tracks are shallow subsurface water/brine conduits typical of
permafrost-dominated hydrological systems on Earth. They may represent a
major water transport pathway that has been active in association with
more recognizable fluvial processes throughout martian history.

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