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Mars is currently at the center of scientific debate regarding proposedancient river morphological landscapes on the planet. An increased curiosity inthe geomorphology of Mars and its water history, therefore, has led to aneffort to better understand how those landscapes formed. Many studies, however,consist of patchwork investigations that have not thoroughly examined proposedancient fluvial processes on Mars from an Earth analog perspective. The purposeof this investigation, therefore, is to compare known fluvial features onMoenkopi Plateau with proposed paleopotamologic features on Mars. The searchfor analogs along the Moenkopi Plateau was due to the similarities in fluvialerosion, influenced and modified by eolian activity, primarily from Permianthrough Jurassic age. By analyzing orbital imagery from two cameras onboardNASA Mars Reconnaissance Orbiter High Resolution Imaging Science Experiment andthe Context Camera and paralleling it with imagery obtained from the U.S.Geological Survey and an unmanned aircraft operating over the Moenkopi Plateau,this investigation identified similar fluvial morphology. We interpret,therefore, that the same fluvial processes occurred on both planets, therebyreinforcing the history of water on Mars.

Ancient River Morphological Features on Mars versus Arizona Moenkopi Plateau