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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    Titel :

    Morphology of Fresh Outflow Channel Deposits on Mars


    Beteiligte:
    Rice, J. W., Jr. (Autor:in) / Parker, T. J. (Autor:in) / Russell, A. J. (Autor:in) / Knudsen, O. (Autor:in)


    Erscheinungsdatum :

    2002-04-01


    Medientyp :

    Aufsatz (Konferenz)


    Format :

    Keine Angabe


    Sprache :

    Englisch




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