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Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies Don’t miss the chance to

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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 geology of central Utah creates unparalleled educational opportunities

scenic routes

Because these reports have many large basic-data maps in addition to the liquefaction potential maps

Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies Don’t miss the chance toBy: 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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