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Subsurface map and seismic risk analysis of the Salt Lake Valley (OFR-152)Vendor: Utah Geological SurveyBy: H. Radkins, M. Murphy, and G. T. Schuster This report is divided into two sections: 1) a compilation and integration of existing geophysical data pertaining to the sub-surface structure of Salt Lake Basin, and 2) a suite of synthetic seismograms which attempt to...
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The Davis County flood warning and information system (OFR-151)Vendor: Utah Geological SurveyBy: M. Lowe, S. R. Williams, and S. W. Smith Extensive damage occurred in Davis County in 1983 and 1984 due to flooding and debris-flow events. As a result of these recent hazards events, Davis County has taken a number of steps to reduce...
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Water-related geologic problems of 1983 in southeastern Utah (OFR-149)Vendor: Utah Geological SurveyBy: F. D. Davis Most of southeastern Utah is in the Colorado Plateau physiographic province. Only the western parts of Wayne and Garfield counties are in the Southern High Plateaus Section of the Basin and Range-Colorado Plateau subprovince. The Colorado Plateau is characterized by...
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AAPG Highway Map--Utah geologic cross section (OFR-147)Vendor: Utah Geological SurveyAAPG Highway Map--Utah geologic cross section
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Geology of the Cannonville quadrangle, Kane and Garfield Counties, Utah (OFR-142)Vendor: Utah Geological SurveyBy: R. Hereford The Cannonville quadrangle is in Kane and Garfield Counties of south-central Utah. Cannonville is the principal community, although Tropic, on the northern boundary of the quadrangle, and Henrieville, 0.4 miles east of the quadrangle, contribute to the economic base of the...
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Maximum extent of potential flooding due to simultaneous failure of dams in Salt Lake County, Utah (OFR-127)Vendor: Utah Geological SurveyBy: W. F. Case The purpose of this study is to determine the probable maximum extent of flooding if all Salt Lake County dams failed simultaneously and all reservoirs drained completely, as may occur during a large earthquake. It is assumed that all major...
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National Science Teachers Association Great Salt Lake field trip (OFR-112)Vendor: Utah Geological SurveyBy: J. W. Gwynn This publication details a field trip led by J. W. Gwynn on September 24, 1987. The publication describes the geology, geography, mineralogy, hydrology, and history of the Great Salt Lake. Information about hazards related to the water level of the...
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Utah's geologic hazards: a review for realtors (OFR-109)Vendor: Utah Geological SurveyBy: G. E. Christenson and D. R. Mabey Geologic hazards are important in Utah. Ever year these hazards cause significant property damage and in some years the damage totals hundreds of millions of dollars. Government facilities, particularly transportation corridors and utilities, sustain the greatest...
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Argyle Canyon-Willow Creek tar sand deposit overburden map (Duchesne County) (OFR-101)Vendor: Utah Geological SurveyBy: B. T. Tripp This tar sand deposit overburden map shows the location of the tar sand beds, overburden contour lines, and special tar sand area boundaries. Other Information: Published: 1986 Plates: 1 pl. Scale: 1:50,000 Location: Duchesne County Media Type: Paper Map
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Argyle Canyon-Willow Creek tar sand deposit isopach map (Duchesne County) (OFR-100)Vendor: Utah Geological SurveyBy: B. T. Tripp This tar sand deposit isopach map shows the location of the tar sand beds, tar sand thickness measurement locations, tar sand isopach lines, and special tar sand area boundaries. Other Information: Published: 1986 Plates: 1 pl. Scale: 1:50,000 Location: Duchesne...
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Geology of Utah (OUT OF PRINT)Vendor: Utah Geological SurveyBy: W. L. Stokes This book is about understanding and appreciating Utah's geology. Over the last fifty years, William lee Stokes has been a steady contributor to the mapping and interpretation of Utah geology. This book is a late dividend of a long professional...
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The Great Salt Lake, Utah (MP J)Vendor: Utah Geological SurveyBy: W. L. Stokes Unlike most large lakes the Great Salt Lake is named for what it truly is – it is great and salty. It is also notable for other reasons. Viewed from space it is an unmistakable landmark in the midst of...
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Proceedings volume, Basin and Range Province Seismic-Hazards Summit (MP 98-2)Vendor: Utah Geological SurveyBy: W. R. Lund, editor The Western States Seismic Policy Council (WSSPC) and the Nevada Bureau of Mines and Geology (NBMG) hosted the Basin and Range Province (BRP) Seismic-Hazards Summit in Reno, Nevada, May 13-15, 1997, to review important technical issues in characterizing seismic...
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Site-specific strong ground motion estimates for the Salt Lake Valley (MP 93-9)Vendor: Utah Geological SurveyBy: I. G. Wong and W. J. Silva The high level of seismic hazard in Salt Lake Valley from potential large earthquakes on the Wasatch fault zone has long been recognized. Of obvious importance to hazard mitigation is the prediction of the near-field strong...
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Tectonic evolution of the Uinta Mountains: palinspastic restoration of a structural cross section along longitude 109?15', Utah (MP 93-8)Vendor: Utah Geological SurveyBy: D. S. Stone Major tectonic events important in the evolution of the Uinta Mountains were evaluated through palinspastic restoration of a north-south structural cross section drawn along longitude 1090 15' in northeastern Utah. The section crosses the Uinta Mountains from Red Wash field...
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Characterization of argillic alteration and K/Ar dating of illite at the Mercur gold mine, Utah: further evidence for a Mesozoic age of gold mineralization (MP 93-5)Vendor: Utah Geological SurveyBy: P. N. Wilson and W. T. ParryMineralogical and chemical analyses of argillic ally altered rocks sampled on transects of the Carrie Steele and Lulu Graben fault zones in the Mereur gold deposit, indicate that the argillic mineralogy and geochemistry are heterogeneous. Although previous...
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Damage potential index mapping for Salt Lake Valley, Utah (MP 93-4)Vendor: Utah Geological SurveyBy: S. M. Adan and K. M. RollinsThe fact that local soil conditions play a major role in determining the intensity of earthquake shaking has been recognized by seismologists and engineers for many years. Recently, a number of major earthquakes have provided excellent opportunities...
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Stratigraphic and lithologic analysis of the Claron Formation in southwestern Utah (MP 93-1)Vendor: Utah Geological SurveyBy: W. J. Taylor The Paleocene - Oligocene Claron Formation in the Basin and Range physiographic province of southwestern Utah is composed dominantly of sandstone and conglomerate interbedded with fresh-water sandy limestone. Stratigraphic sections, clast counts, and point counts from the Claron Formation in...
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New 40Ar/39Ar ages of intrusive rocks from the Henry and La Sal Mountains, Utah (MP 92-2)Vendor: Utah Geological SurveyBy: S. T. Nelson, M. T. Heizler, and J. P. Davidson Previously published Eocene and late-Oligocene K-Ar ages of intrusive rocks of the Henry and La Sal Mountains are bimodal whereas sphene and zircon fission-track ages are exclusively late Oligocene. The apparent discordance between...
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Petrology, sedimentology, and stratigraphic implications of the Rock Canyon Conglomerate, southwestern Utah (MP 91-7)Vendor: Utah Geological SurveyR. L. Nielson Deposition of the Rock Canyon Conglomerate in southwestern Utah and northwestern Arizona resulted from infilling of topography that was cut during the late Permian and early Triassic Periods. Three lithofacies are recognized in the Rock Canyon Conglomerate: 1) a chert pebble...
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