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Vendor: Utah Geological AssociationEdited By: John S. MacLean, Robert F. Biek, and Jacqueline E. HuntoonContains 35 geological papers and 2 road guides describing the geology of Utah's Far South. The papers are arranged by topics: Geomorphology, Hydrogeology, Reservoir Properties, Statigraphy, Paleontology, Structural Geology & Volcanism, and Field...
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Vendor: Ground WaterBy: F. X. Ashland, C. E. Bishop, M. Lowe, and B. H. Mayes, editors Urbanization of parts of the Snyderville basin has been accompanied by an increasing demand to develop the area?s ground-water resources. Ground water is present in shallow unconsolidated deposits and fractured...
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Vendor: Utah Geological AssociationEdited by: S. M. Carney, D. E. Tabet, C. L. Johnson South-central Utah is famous for its superb outcrops of igneous, metamorphic, and sedimentary rocks. In particular, strata of this region range in age from Triassic to early and mid-Tertiary and were deÂposited in...
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Vendor: Utah Geological AssociationEdited by: L. E. Spangler Ground water in Utah is an important and current subject. Ground water as a resource is under increased pressure because of droughts, and because of continuing development in many parts of the state. Several artificial recharge projects are in...
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Vendor: Utah Geological AssociationEdited by: R. E. Blackett and J. N. MooreOver the past decade, southwestern Utah has undergone rapid urban growth; the populations of Iron and Washington Counties have nearly doubled. This rapid growth has created new emphasis on developing the economy of the region, while...
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Vendor: Utah Geological AssociationEdited by: G. E. CordyThis publication contains papers detailing ground-water and waste issues in the state of Utah. The following are the papers that can be found in this publication:Utah ground-water quality: status and design for protection, by R. P. Barnes and W. E....
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Vendor: Utah Geological SurveyBy: R. W. Fleming and G. L. Waanders Lower Cretaceous strata exposed in the foreland basin of central Utah were divided into two lithostratigraphic units, the Cedar Mountain and San Pitch Formations. Together these formations correlate with both the Cedar Mountain Formation exposed on...
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Vendor: Utah Geological SurveyBy: B. D. Black, B. J. Solomon, and K. M. Harty Geologic hazards are naturally occurring geologic processes that present a risk to life and property. Tooele County is subject to many geologic hazards that need to be identified and considered prior to development....
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Vendor: Utah Geological SurveyBy: M. D. Hylland and M. Lowe The Farmington Siding landslide complex is in Davis County, Utah, about 25 kilometers north of Salt Lake City. The landslide complex covers approximately 19.5 square kilometers and is one of 13 late Pleistocene/Holocene features along the Wasatch...
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Vendor: Utah Geological SurveyBy: B. J. Solomon Radon derived from the radioactive decay of uranium migrates in soil gas and, after penetrating foundation openings, can accumulate indoors in sufficient quantities to pose a health hazard. Geologic factors that influence radon emanation and migration, including uranium concentration, ground-water...
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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: H. E. Gill and W. R. LundPark City began as a mining community in the late 1860s and mining continued actively in the area for more than 100 years. In the 1970s skiing surpassed mining as the major industry in the area. Due...
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Vendor: Utah Geological SurveyBy: C. G. Oviatt, J. F. Shroder, and R. E. Sewell The Colorado Plateau is a unique area for the study of Quaternary deposits and processes since it has been the site of continuous stream downcutting, cliff retreat, and landscape denudation during much of...
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Vendor: Utah Geological SurveyBy: J. A. WhelanThe Rocky Range is a small, isolated mountain range northwest of Milford in Beaver County, Utah. The range was organized into a mining district in 1872 and has been a small but significant producer of copper and tungsten ores during periods...
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Vendor: Utah Geological SurveyBy: S. Heuscher The Henry Mountains coalfield is in central Wayne and Garfield Counties in a remote area of Utah with few paved roads. The coalfield lies in a structural basin called the Henry Mountains syncline. The syncline is bounded on the west by...
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Vendor: Utah Geological SurveyBy: D. E. Tabet, B. P. Hucka, J. C. Quick, and S. I. Wakefield This report describes the coal stratigraphy, quality, and resource found in the Blackhawk Formation within four quadrangles in Sevier County, Utah. These quadrangles cover most of the Salina Canyon coalfield...
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Vendor: Utah Geological SurveyBy: W. R. Lund, T. R. Knudsen, G. S. Vice, and L. M. ShawThe St. George-Hurricane metropolitan area is one of the nation?s fastest growing regions. As land well suited for development becomes increasingly scarce, urbanization has moved into less favorable areas where geologic...
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Vendor: Utah Geological SurveyBy: G. N. McDonald and F. X. Ashland Contains a 41-page report and a 1:150,000-scale map defining seismic site conditions for the Wasatch Front urban corridor. This mapping, partially funded through the U.S. Geological Survey’s National Hazards Reduction Program, provides a basis for predicting...
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Vendor: Utah Geological SurveyBy: S. M. Kirby Recent residential growth in unincorporated portions of San Juan County north and east of Blanding utilizes ground water derived primarily from sandstone of the undivided Dakota and Burro Canyon Formations for culinary water. The primary source of recharge to the...
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Vendor: Utah Geological SurveyBy: W. R. Lund, C. B. DuRoss, S. M. Kirby, G. N. McDonald, G. Hunt, and G. S. Vice Contains a 30-page report and 37-photo appendix of an investigation by the Utah Geological Survey of five recently discovered earth fissures in southwestern Utah. The...
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