A Reevaluation of Mass Movements Within the Valles Marineris Region of Mars Using MOLA and MOC Data

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Scientific paper

Our research indicates that forces initiating Martian slumps may be
higher in potential energy than those initiating Martian landslides. Our
comparison of Martian slides to submarine landslides suggests that fluid
or acoustic fluidization may be driving long runouts on Mars.

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