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TheVeteran

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TheVeteran

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Wednesday, 05/05/2021 3:15:33 AM

Wednesday, May 05, 2021 3:15:33 AM

Post# of 1743
In the western part of the Paiute area, the Dewitt Thrust Fault places Ordovician Valmy Formation cherts and shales on top of Cambrian Harmony Formation quartz- and feldspathic-sandstones and shales, which are locally calcareous. Faults at Elder Creek dip steeply, strike north-northwest to north-northeast and show normal and oblique-slip offset. The Elder Creek Fault indicates normal, down-to-the- west movement.
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