By: Daren T. Nelson and Paul W. Jewell
The Hogup Bar quadrangle is located southeast of Park Valley, Utah, and west of the northwest arm of Great Salt Lake. Late Pleistocene Lake Bonneville sediments and related shorelines dominate the landscape, and record the transgression and regression of Lake Bonneville. Surficial deposits overlie Tertiary basalt and Permian-Pennsylvanian sedimentary bedrock.
Also included are one plate - a geologic map at 1:24,000 scale - and a 12-page booklet. The latest version of Adobe Reader is required to view the PDF files and can be downloaded from www.adobe.com. Specialized GIS software is required to use the GIS files.
Includes GIS data