Quaternary Studies and General Geology
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Vendor: Utah Geological SurveyBy: Daren T. Nelson and Paul W. JewellThe 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...
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Vendor: Utah Geological SurveyBy: S. Kwon and G. Mitra Chapter 1 describes the bedrock stratigraphy and structural aspects of the study area, located at the southern end of the Provo salient of the Sevier fold-thrust belt. Chapter 2 discusses the controversies on the structural geology and provides...
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Vendor: Utah Geological SurveyBy: Other Information: Published: Pages:
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Vendor: Utah Geological SurveyBy: Other Information: Published: Pages:
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Vendor: Utah Geological SurveyBy: K. L. Cook, V. Bankey, D. R. Mabey, M. DePangher The compilation and publication of this map was a cooperative effort by (1) the Utah Geological and Mineral Survey, (2) the United States Geological Survey, and (3) the Department of Geology and Geophysics,...
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Vendor: Utah Geological SurveyBy: W. R. Lund This report presents the results of the Utah Quaternary Fault Parameters Working Group (hereafter referred to as the Working Group) review and evaluation of Utah’s Quaternary fault paleoseismic-trenching data. The purpose of the review was to (1) critically evaluate the...
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Vendor: Utah Geological SurveyBy: M. A. Shubat and W. S. McIntoshThe Antelope Range mining district, located approximately 20 miles (32 km) west of Cedar City, Utah, contains many occurrences of epithermal, base and precious metals mineralized veins. Host rocks in the district range from limestone of the...
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