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Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies scenic routes

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scenic routes

Don’t miss the chance to learn from experts in the field and discover why Utah is recognized as a top destination for geological studies and exploration

The advanced printing process enhances the map's details

Spanning the eastern reaches of the Uinta range

Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies scenic routesBy: T. J. Copfer and J. P. Evans The Stansbury Mountains consists of Paleozoic rocks folded into the north south trending Deseret anticline. Ordovician, Silurian, and Devonian rocks are absent in the central part of the range where basal Mississippian units rest unconformably on Cambrian beds. Paleozoic uplift, Mesozoic contraction, and Cenozoic extension have created a series of broad folds, large thrust faults, and a variety of normal faults within

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