What is it about?
The Antarctic McMurdo Dry Valleys are very similar in many ways (hyperarid, hypothermal) to the current surface of Mars. Here we explore these climatic and geological environments and provide a framework for the interpretation of a "cold and icy" Early Mars climate scenario.
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This page is a summary of: The climate history of early Mars: insights from the Antarctic McMurdo Dry Valleys hydrologic system, Antarctic Science, November 2014, Cambridge University Press,
DOI: 10.1017/s0954102014000686.
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