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Gigapans

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  1. These are synorogenic conglomerates deposited during the peak of Late Cretaceous Sevier Orogeny thrusting in the Utah-Wyoming Thrust Belt.

  2. Sevier age thrust fault at Ketobe Knob on the south side of Cedar Mountain in the San Rafael Swell, southeast of Cleveland, Utah. This is the iconic outcrop of the second major structure/geologic mapping project of the Fort Hays State University Geology Summer Field Camp. For more information about our field camp see...

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