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Preguntas comunes acerca de Gran Lago Salado de Utah y de Antiguo Lago Boneville (Spanish version of Commonly asked questions about Utah's Great Salt Lake) (PI-86)Vendor: Utah Geological SurveyBy: J. W. Gwynn Translated into Spanish, this color pamphlet 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...
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Earthquake fault map of a portion of Tooele County, Utah (PI-84)Vendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Tooele Valley, between the Oquirrh Mountains and the Stansbury Mountains. Back side of map includes information on faults, effects of surface fault rupture, when and where surface rupture is likely to occur, and...
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Earthquake fault map of a portion of Cache County, Utah (PI-83)Vendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Cache Valley, between the Bear River Range to the east and the Cache County line to the west. Back side of map includes information on faults, effects of surface fault rupture, when and...
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Liquefaction susceptibility map for Tooele Valley, Tooele County, Utah (PI-80)Vendor: Utah Geological SurveyBy: UGS Staff The liquefaction-susceptibility categories of Tooele Valley are mapped based on local geology and subsurface soil and water conditions. In Tooele Valley, the most susceptible soils are along the shorelines of Great Salt Lake and Rush Lake. Answers are provided to questions...
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Great Salt Lake information sheet (PI-8)Vendor: Utah Geological SurveyBy: J. W. Gwynn This one page information sheet gives basic information concerning the Great Salt Lake. Information includes: low level on record, high level on record, freshwater sources, salt content, islands, and more. Other Information: Published: 1990 (updated 1998) Pages: 1 p. Location:...
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St. George dinosaur tracksite (PI-78)Vendor: Utah Geological SurveyBy: UGS Staff The St. George Dinosaur Trackside, a world-class dinosaur trackside, was discovered in February 200 about one mile east of downtown St. George in southwestern Utah. This two-sided handout gives information about the ancient environment, how the tracks were preserved, and how...
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Using geologic-hazards information to reduce risks and losses - a guide for local governments (PI-75)Vendor: Utah Geological SurveyBy: B. J. Solomon Many of the geologic processes that shaped Utah's landscape over the past few million years remain active today. When these natural processes endanger life and property we term them geologic hazards. Utah has experienced loss of life and property damage...
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Landslides: What they are, why they occur (PI-74)Vendor: Utah Geological SurveyBy: W. F. Case Landslides occur as gravitational forces exceed the strength of the material in a slope. Rock slides, debris slides, and slumps “slide†on a weak, fractured, slick, clayey, or water-saturated surface. This two-page sheet discusses why landslides occur, how risk can...
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Debris-flow hazards (PI-70)Vendor: Utah Geological SurveyBy: W. F. Case Color flyer with photos. It explains what debris-flows are, how they come to be, and the hazards associated with them in an easy-to-understand text. Other Information: Published: 2000 Pages: 2 p. Location: Utah Media Type: Paper Publication
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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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Brine properties, mineral extraction industries, and salt load of Great Salt Lake, Utah (PI-51)Vendor: Utah Geological SurveyBrine properties, mineral extraction industries, and salt load of Great Salt Lake, Utah
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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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Geothermal resources map of Utah (PI-4)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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