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Rock-fall hazards (PI-69)Vendor: Utah Geological SurveyBy: W. F. Case Rock falls are a natural process of cliff and hillside erosion. They consist of large rock fragments from a cliff, or boulders from a slope that bounce, roll, and slide down a hillside and come to rest in a “runoutâ€...
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Earthquake hazards and safety in Utah (PI-6)Vendor: Utah Geological SurveyBy: UGS Staff This four-page publication outlines a brief history of earthquakes in Utah, discusses different hazards related to earthquake activity, and gives instructions on earthquake safety. Other Information: Published: 1990 Pages: 4 p. Location: Utah Media Type: Paper Publication
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Homeowner's guide to recognizing and reducing landslide damage on their property (PI-58)Vendor: Utah Geological SurveyBy: GES staff Landslides are common in Utah. Landslide hazards are greatest near or on steep slopes or along streams. Listed below are suggestions on how to recognize landslides and landslide-prone areas, and what to do to reduce the likelihood of landslides. And REMEMBER...
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Stability of the Pine Ridge landslide at Timber Lakes Estates, Wasatch County, Utah: implications for future development and land-use planning (PI-53)Vendor: Utah Geological SurveyBy: F. X. Ashland and M. D. Hylland This pamphlet provides a nontechnical summary of the results of the Utah Geological Survey’s preliminary slope-stability evaluation of the Pine Ridge landslide at the Timber Lakes Estates in Wasatch County, and discusses the implications for future...
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Radon-hazard potential in the central Sevier Valley, Sevier County, Utah (PI-47)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of central Sevier Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common in the south end of the valley and along the valley margins. This soil is derived...
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Radon-hazard potential in southeastern Cache Valley, Cache County, Utah (PI-46)Vendor: Utah Geological SurveyBy: B. J. Solomon and B. D. Black The radon-hazard potential of southeastern Cache Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is generally found along the mountain front. This soil is derived from local conglomerate...
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Radon-hazard potential in the lower Weber River area, Weber and Davis Counties, Utah (PI-45)Vendor: Utah Geological SurveyBy: B. D. BlackThe radon-hazard potential of lower Weber River area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is found in the Weber delta and along the mountain front. This soil is deltaic sediment deposited by...
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Radon-hazard potential in Tooele Valley, Tooele County, Utah (PI-44)Vendor: Utah Geological SurveyBy: B. D. Black The radon-hazard potential of Tooele Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is found locally along the valley margin. This soil is sediment deposited by Lake Bonneville, or alluvium locally derived...
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Radon-hazard potential in western Salt Lake Valley, Salt Lake County, Utah (PI-43)Vendor: Utah Geological SurveyBy: B. D. Black Color pamphlet that answers questions about the Great Salt Lake and Lake Bonneville such as when did Lake Bonneville exist and what kinds of animals lived around it, why is the Great Salt Lake salty, what islands are in the...
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Radon-hazard potential in the Ogden Valley, Weber County, Utah (PI-36)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of Ogden Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common west of Liberty. This soil is derived from metamorphic rock on the northwest valley margin. Answers are...
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Radon-hazard potential in the St. George area, Washington County, Utah (PI-35)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the St. George area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common south of St. George. This soil is derived from local shale outcrops and from granitic...
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Earthquake fault map of a portion of Salt Lake County, UtahVendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Salt Lake County. Back side of map includes information on faults, effects of surface fault rupture, when and where surface rupture is likely to occur, and what can be done to protect homes....
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Radon-hazard potential in the Provo-Orem area, Utah County, Utah (PI-21)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the Provo-Orem area is mapped based on geologic factors. Soil with potential for higher indoor-radon levels is common on the east bench and on alluvial fans along the Wasatch Range front. This soil is derived from...
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Radon-hazard potential in the Sandy-Draper area, Salt Lake County, Utah (PI-18)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the Sandy-Draper area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common on the east bench at the mouth of Little Cottonwood Canyon. This soil is derived from...
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Earthquake fault map of a portion of Utah County, Utah (PI-11)Vendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Utah County. Back side of map includes information on faults, effects of surface fault rupture, when and where surface rupture is likely to occur, and what can be done to protect homes. Other...
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Earthquake fault map of a portion of Weber County, Utah (PI-1)Vendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Weber County. Back side of map includes information on faults, effects of surface fault rupture, when and where surface rupture is likely to occur, and what can be done to protect homes. Other...
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Compilation of 1970s Woodward-Lundgren & Associates Wasatch fault investigation reports and low-sun-angle aerial photography, Wasatch Front and Cache Valley, Utah and Idaho (OFR-632)Vendor: Utah Geological SurveyBy: Steve D. Bowman, Adam I. Hiscock, and Corey D. Unger This nine DVD set contains a descriptive 8-page report and digital files created from the Wasatch fault investigation project performed for the Utah Geologic and Mineralogical Survey (now the Utah Geological Suvey) and...
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Preliminary Landslide Inventory Map of the 2012 Seeley Fire Area, Carbon and Emery Counties, Utah (OFR-612)Vendor: Utah Geological SurveyBy: Greg N. McDonald and Richard E. GiraudThis map presents a landslide inventory for the 2012 Seeley fire area, Carbon and Emery counties, Utah, at a scale of 1:24,000. The purposes of the map and accompanying geodatabase are to show and characterize landslides and...
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Evaluation of interferometric synthetic aperture radar (InSAR) techniques for measuring land subsidence and calculated subsidence rates for the Escalante Valley, Utah, 1998 to 2006 (OFR-589)Vendor: Utah Geological SurveyBy: R. R. Forster Previous studies have shown the Escalante Valley, Utah, is subsiding due to groundwater withdrawal. The magnitude and spatial pattern of this cm/yr.-scale subsidence is mapped with satellite data from a synthetic aperture radar (SAR) using interferometric SAR (InSAR) processing techniques....
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Snowmelt-induced ground-water fluctuations in selected northern Utah landslides ? preliminary results from the 2007-08 landslide water year (OFR-550)Vendor: Utah Geological SurveyBy: F. X. Ashland The relationship between ground-water levels and late winter/early spring snowmelt was evaluated at selected northern Utah landslides where ground-water observation wells had previously been installed. The period of investigation between September 2007 and August 2008 was characterized by generally wetter-than-normal...
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