Geomorphic Evidence for Former Lobate Debris Aprons at Low Latitudes on Mars: Indicators of the Martian Paleoclimate

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Scientific paper

We show geomorphic evidence for the former presence of lobate debris
aprons at low latitudes (<30°) on Mars. Since lobate debris
aprons are thought to contain ice, which is theoretically not stable at
these latitudes today, this observation has implicatio

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