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THEMIS: Fault-edged blocks of Sacra Fossae →

HiRISE: Inverted channel on elevated terrain

Posted on August 2, 2018 by rburnham

tumblr_pcp7ozLy2k1rlz4gso1_1280An inverted channel on elevated terrain. Interesting fluvial processes that might help improve our understanding of the deposits in the Medusae Fossae Formation.

Beautiful Mars series. [More at links]

This entry was posted in Reports and tagged Beautiful Mars, eolian processes, fluvial channels, fluvial deposits, fluvial processes, High Resolution Imaging Science Experiment, HiRISE, inverted channels, inverted topography, Mars Reconnaissance Orbiter, Medusae Fossae Formation, MRO, NASA, University of Arizona, wind erosion, yardangs. Bookmark the permalink.
← MARCI weather report, July 23-29, 2018
THEMIS: Fault-edged blocks of Sacra Fossae →

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