Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies Because these reports have many

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

The advanced printing process enhances the map's details

Strata generally dip northward toward the Uinta Basin

geophysical logs

scenic routes

Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) Butterflies Because these reports have manyBy: 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