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Deltaic and shelf deposits in the Cretaceous Blackhawk Formation and Mancos Shale, Grand County, Utah (MP 91-6)Vendor: Utah Geological SurveyM. A. Chan Continuous, well-preserved clastic depositional units south of the Book Cliffs escarpment of east-central Utah offer exceptional exposures of ancient deltaic, shoreline, shelf and offshore rocks. A stratigraphic and sedimentologic context for these Cretaceous units is an important tool in exploration for...
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Petrology, age, geochemistry, and correlation of the Tertiary volcanic rocks of the Awapa Plateau, Garfield, Piute, and Wayne Counties, Utah (MP 91-5)Vendor: Utah Geological SurveyBy: S. R. Mattox Volcanic rocks of the eastern flank of the Marysvale volcanic field are exposed on the Awapa Plateau, one of the easternmost High Plateaus in the Utah Colorado Plateau - Basin and Range transition zone. Initial mapping by Williams and Hackman...
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Wood Ranch thermal anomaly, Iron County, Utah (MP 91-4)Vendor: Utah Geological SurveyBy: H. P. Ross, R. E. Blackett, and M. A. Shubat Isolated locations within the Escalante Valley of southwestern Utah exhibit higher than normal ground-water temperatures. The sources of geothermal fluid, which cause the elevated temperatures, are not well understood. Because of this uncertainty...
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Soils as a tool for applied Quaternary geology (MP 91-3)Vendor: Utah Geological SurveyBy: P. W. Birkeland, M. N. Machette, and K. M. Haller This manual provides a brief summary of materials discussed during a short course entitled Soils as a tool for applied Quaternary geology that was taught May 30-June 1, 1990. During the seminar, we...
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Characteristics of acid-sulfate alteration in the Marysvale-Pioche mineral belt: a guide to gold mineralization (MP 91-2)Vendor: Utah Geological SurveyBy: A. J. B. Thompson The zones of extensive acid-sulfate alteration in the Marysvale-Pioche mineral belt have been of interest to explorationists for many years, most recently for their precious metal potential. Based on recent field work, existing information and advances in the understanding...
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A guide to reducing losses from future earthquakes in Utah - Consensus document (MP 91-1)Vendor: Utah Geological SurveyBy: W. J. Arabasz, editor The purpose of this document, as originally conceived, was to motivate and guide actions that will reduce losses from future moderate-to-large (magnitude 5.5 to 7.5) earthquakes in Utah, with primary emphasis on Utah's densely populated Wasatch Front region. In...
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Stratigraphy and paleogeography of Late Cretaceous and Paleogene rocks of southwest Utah (MP 90-2)Vendor: Utah Geological SurveyP. M. Goldstrand This paper describes the stratigraphy of the Late Cretaceous and Paleogene nonmarine strata of southwestern Utah. Paleocurrent analysis, depositional system reconstructions, and provenance studies are used to reconstruct the paleogeography from early Campanian to middle Eocene. These data document three temporally...
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Multi-characteristic correlation of upper Cretaceous volcanic ash beds from southwestern Utah to central Colorado (MP 89-5)Vendor: Utah Geological SurveyBy: B. J. Kowallis, E. H. Christiansen, and A. Deino Precise correlation of volcanic ash beds, common over wide areas in continental and marine sedimentary sections, has wide application in stratigraphic, tectonic, and paleontologic studies. To establish a protocol for direct correlation of ash...
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Geologic resources of Box Elder County, Utah (MP 89-3)Vendor: Utah Geological SurveyBy: S. N. Eldredge, M. H. Bugden, and C. M. Wilkerson This brochure is a basic introduction to Box Elder County's geologic resources and the role they play in our economy and everyday lives. To recognize their existence and realize their importance, it is...
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An evaluation of the travel distance potential of debris flows (MP 89-2)Vendor: Utah Geological SurveyBy: S. H. Cannon Debris flows are characteristically able to travel long distances over gentle slopes, and they often damage whatever may be in their path. A weakness in current debris-flow hazard assessments is in the lack of information available on the potential extent...
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Evaluation of seismicity relevant to the proposed siting of a superconducting supercollider (SSC) in Tooele County, Utah (MP 89-1)Vendor: Utah Geological SurveyBy: W. J. Arabasz, J. C. Pechmann, and E. D. Brown This report presents (1) a characterization of seismicity within 160 km of two alternative sites proposed for a Superconducting Supercollider (SSC) facility in Tooele County, Utah; and (2) an evaluation of implications for...
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Gold prospecting in Utah from Stuvey Notes 15-3Vendor: Utah Geological SurveyBy: M. R. Smith This article was republished from the August 1981 edition of Survey Notes 15-1, highlighting the rich history of gold mining in Utah. It explores the various types of gold deposits, including placer deposits, and provides valuable information on staking a...
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Juke Box Trench-a Valuable Archive of Late Pleistocene and Holocene Statigraphy in the Bonneville Basin, Utah (MP 18-1)Vendor: Utah Geological SurveyBy: Charles G. Oviatt, Jeffrey S. Pigati, David B. Madsen, David E. Rhode, and Jordan BrightIn 2009, we enlarged a backhoe trench below the mouth of Juke Box Cave, near Wendover, Utah, at the western edge of the Great Salt Lake Desert in order...
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Hydrocarbon Reservoir Potential of the Mississippian Chainman Shale, Western Utah (MP 15-4)Vendor: Utah Geological SurveyBy: S. Robert Bereskin, John D. McLennan, Thomas C. Chidsey, Jr., and Peter J. NielsenThe Mississippian Chainman Shale represents a potential target for untapped oil and gas resources in western Utah and eastern Nevada. This study focuses on the lithologic, facies, petrographic, petrophysical, and...
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Geologic Map of Unconsolidated Deposits in the Hogup Bar Quadrangle, Box Elder County, Utah (MP 15-2dm)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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Paleoseismology of Utah, Volume 20 - Compilation of U.S. Bureau of Reclamation seismotectonic studies in Utah, 1982-1999 (MP 11-2)Vendor: Utah Geological SurveyBy: W. R. Lund, S. D. Bowman, and L. A. Piety, compilers This compilation of eight seismotectonic reports pertaining to seismic safety evaluations conducted during the 1980s and 1990s is the first such legacy document released in the Paleoseismology series. This Utah Geological Survey...
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Paleoseismology of Utah, Volume 19: Late Quaternary faulting in East Canyon Valley, Northern Utah (MP 10-5)Vendor: Utah Geological SurveyBy: L. A. Piety, L. W. Anderson, and D. A. Ostenaa East Canyon Valley, a 25-km-long by 5-km-wide back-valley, is on the eastern flank of the Wasatch Range about 25 km northeast of Salt Lake City and the Wasatch Front. Previous geologic mapping and...
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New insights into the structural geology of the Gilson and Northern Canyon Mountains, Central Utah (MP 07-4)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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Land subsidence in southwest Utah from 1993 to 1998 measured with Interferometric Synthetic Aperture Radar (InSAR) (MP 06-5)Vendor: Utah Geological SurveyBy: R. R. Forster The objective of this study is to measure land-surface subsidence in southwest Utah using Interferometric Synthetic Aperture Radar (InSAR). During the winter of 2004/2005 the Utah Geological Survey documented earth fissures near Beryl Junction in Iron County, Utah. The UGS...
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Landslide investigation of Timber Lakes Estates, Wasatch County, Utah: Landslide inventory and preliminary geotechnical-engineering slope stability analysis (MP 05-9)Vendor: Utah Geological SurveyBy: D. P. Neuffer and R. L. Bruhn We produced a comprehensive, detailed landslide map of Timber Lakes Estates in Wasatch County, Utah. Landslide deposits underlie about 13% of the total area of Timber Lakes (about 3,200 acres). We mapped twenty separate landslides scattered...
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