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Pumpkin Buttes

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Geology

The buttes are erosional remnants of Tertiary-aged sediment that once filled the entire Powder River Basin. Roughly 50 million years ago, the basin was a lush, subtropical environment filled with swamps and rivers. Rivers and creeks flowing from the Big Horn Mountains to the west deposited silt and sand in thick layers. During the Oligocene epoch, massive volcanic eruptions in the western U.S. (including the Absaroka Range) blanketed the area in thick volcanic ash. Over time, the vast majority of these sediments were washed away by wind and water. The Pumpkin Buttes remain because they are capped by a 30-to-50-foot layer of the White River Formation. This capstone is made of tougher, coarse-grained sandstone and volcanic tuff that protected the softer underlying Wasatch Formation from eroding away.

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