Measurement of Bedding Geometry of Upper Aeolis Mons, Gale Crater, Mars
Abstract:
We present initial results of an investigation using a HiRISE Digital Terrain Model (DTM) based on the HiRISE stereo pair PSP_001620_1750 and PSP_001422_1750 test the hypothesis that the upper formation of Aeolis Mons represents aeolian cross-bedding. By tracing the intersection of the beds with a plane, we will determine whether the observed patterns might be explained by the interaction of planar beds and complex erosion or if the observed structures require cross-bedded deposits. These measurements are ongoing. If the complex bedding patterns observed in the upper formation are confirmed to be cross-beds, we will present measurements of the bedding orientation and use computer models to interpret the depositional conditions for the upper formation of Aeolis Mons.
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