MARS GEOMORPHOLOGY AS AFFECTED BY AQUEOUS PROCESSES OVER THE HISTORY OF MARS

At 2:30 today in the Waterway Ballroom 4 at LPSC 2014 you can hear Mt. Sharp was formed in two phases of deposition and erosion, separated by a significant time gap. Location and morphology were influenced by a peak ring.   Follow on sessions at 2:45  will talk about Curiosity’s canyon path includes a gully, debris deposits, and fan/deltas that are bordered by a sloping bedform-capped plain and crossed by lake shorelines.

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