We interpret the channel surface of Athabasca and Marte Valles to be fresh former ice-rich fluvial (hyperconcentrated) deposits rather than volcanic flows. Simply stated, this is what a fresh outflow channel deposit would look like. Additional information is contained in the original extended abstract.


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    Title :

    Morphology of Fresh Outflow Channel Deposits on Mars


    Contributors:


    Publication date :

    2002-04-01


    Type of media :

    Conference paper


    Type of material :

    No indication


    Language :

    English




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