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Vendor: Utah Geological SurveyCompiled by: R. E. Blackett Map showing warm and hot springs located in Utah. Spring temperatures range from 68 to over 122 degrees Fahrenheit. Other data for each spring includes location (using spring numbering system), flow rate, pH, and total dissolved solids (TDS). Other...
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Vendor: UGAThe UGS presents this Geofluids of Utah guidebook, which has papers highlighting key fields in the study of geofluids. This guidebook features four broad subjects in the realm of geofluids: (1) potable water, (2) geothermal energy, (3) biomarkers and hydrocarbons, and (4) evaporites, diagenesis,...
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Vendor: Utah Geological SurveyBy: R. E. Blackett and M. A. Shubat Past exploration in low- and moderate-temperature systems of the Great Basin shows that the relatively small area associated with fluid upflow and elevated temperatures is often difficult to detect by drilling widely spaced temperature-gradient holes or...
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Vendor: Utah Geological SurveyBy: R. E. Blackett In cooperation with geothermal greenhouse operators at the Newcastle geothermal area, the Utah Geological Survey continues to monitor temperature changes within the geothermal field over time. This report presents temperature-depth data collected from six monitoring wells since a previous study...
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Vendor: Utah Geological SurveyBy: R. E. Blackett As part of a U.S. Department of Energy-sponsored program to assist locating a production well to supply a proposed, small-scale geothermal power plant, two exploratory (thermal-gradient) boreholes were drilled in the fall of 2001 on private lands belonging to Milgro...
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Vendor: Utah Geological SurveyBy: W. Anderson and R. L. Bruhn The Sevier geothermal anomaly of southwestern Utah encompasses a broad region of enhanced heat flow with seven known high-temperature geothermal resource areas or "KGRA". The anomaly also encompasses the transition between the Colorado Plateau and the eastern...
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Vendor: Utah Geological SurveyBy: M. R. SmithUtah has valuable and abundant natural energy resources which include oil and natural gas, coal, uranium, gilsonite, geothermal hot water and steam, oil shale, tar sand, and methane. The locations of important energy resources are shown on the brochure map. At...
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Vendor: Utah Geological SurveyBy: R. E. Blackett, H. P. Ross, and C. B. Forster Discovered in 1975 by local farmers, the Newcastle geothermal resource has developed slowly. Pumping of geothermal water from the unconfined aquifer for space heating, mainly for commercial greenhouses, began in the early 1980s,...
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Vendor: Utah Geological SurveyBy: compiled by K.E. Budding and M. H. Bugden A bibliography of Utah geothermal references through 1984. These references which directly pertain to a geothermal resources are annotated. The annotations are intended to inform the reader of the information contained in the article, not...
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Vendor: Utah Geological SurveyBy: R. H. Klauk and C. Gourley The Escalante Valley is a typical Basin and Range valley encompassing an area of 800 mi2 in Iron County and parts of Beaver and Washington Counties in southwestern Utah. Cedar City, the major metropolitan center in this...
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Vendor: Utah Geological SurveyBy: J. Wallace and M. Lowe Nitrate can be used to identify potential deleterious effects of development using septic tank soil-absorption systems. We use a mass-balance approach to provide a valley-wide assessment of the potential impact of nitrate from septic tank soil-absorption systems on...
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Vendor: Utah Geological SurveyBy: R. H. Klauk The Utah Geological and Mineral Survey (UGMS) has been conducting research to identify low-temperature geothermal resources. This report, which is part of an area-wide geothermal research program along the Wasatch Front, is the culmination of the study conducted in the...
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Vendor: Utah Geological SurveyBy: UGS Staff This simplified map shows the location of geothermal areas throughout the state of Utah. Known geothermal areas are shown in dark green, while areas that are favorable for discovery are also identified. This map is perfect for anyone looking to get...
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Vendor: Utah Geological SurveyBy: Peter D. Rowley, Edward F. Rutledge, David J. Maxwell, Gary L. Dixon, and Chester A. WallaceThis 27-page report analyzes new detailed (1:12,000 scale) geologic mapping of a 14 square mile area centered by the high-temperature (350¡F) Sulphurdale heat source, which at the surface...
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Vendor: Utah Geological SurveyBy:Brennan Young, Katherine, Shervais, Moises Ponce-Zepeda, Sari Rosove, James EvansContains a 29-page report conducted by undergraduate researchers at Utah State University during 2010 and 2011 under the direction of Dr. James P. Evans. It includes data collected from hot springs in northern Utah and...
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Vendor: Utah Geological SurveyBy: Mike Lowe Contains a 9-page report describing the potential causes of subsidence in sedimentary basins and providing recommendations for avoiding or minimizing subsidence. Land subsidence can be caused by a variety of processes, but most land subsidence in the United States is associated...
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Vendor: Utah Geological SurveyBy: R. E. Blackett and S. I. Wakefield, compilers Many researchers have studied geothermal resources in Utah over the past few decades, largely the result of federal and state cooperative projects. Because no summary from these efforts had been compiled since the publication of...
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Vendor: Utah Geological SurveyBy: C. Eisinger The Cedar Valley drainage basin encompasses more than 580 square miles (1,502 km2) in southwestern Utah. Located in the transition zone between the Basin and Range and Colorado Plateau physiographic provinces, the drainage basin includes Cedar Valley, the Hurricane Cliffs, and...
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Vendor: Utah Geological SurveyBy: R. E. Blackett, M. A. Shubat, D. S. Chapman, C. B. Forster, C. M. Schlinger, and C. E. Bishop Geological, geophysical and geochemical studies contributed to a conceptual hydrologic model of the ''blind'' (no surface expression), moderate-temperature Newcastle geothermal system, located in the...
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Vendor: Utah Geological SurveyBy: P. N. Wilson and W. T. Parry Alteration of the Manning Canyon and Long Trail Shales in the southern Oquirrh Mountains has resulted in (1) oxidation of organic matter and pyrite; (2) replacement by phyllosilicates; (3) silicification; (4) porphyroblast growth; (5) fossil replacement...
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