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.
Morphology of Fresh Outflow Channel Deposits on Mars
2002-04-01
Aufsatz (Konferenz)
Keine Angabe
Englisch
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