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

Provisional geologic map of the Deseret Peak East quadrangle, Tooele County, Utah (OFR-450) ButterfliesBy: 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

geophysical logs

Spanning the eastern reaches of the Uinta range

The geology of central Utah creates unparalleled educational opportunities

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

Strata generally dip northward toward the Uinta Basin

It is the only journal kept by anyone on that expedition

Coal thickness measurements from outcrops were plotted on the maps only when they appeared to fully represent the complete coal section for each coal zone and not just scattered individual coalbeds

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

do what interests them

"This book is about Lake Powell