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The 2005 Sage Vista Lane Landslide, Cedar Hills, Utah County, Utah (PI-89)By: A. Elliott Homeowners in Cedar Hills first detected movement on the Sage Vista Lane landslide on April 28, 2005, and by the next day the landslide had moved against the lower back wall of a townhouse unit. This publication explains why the landslide...
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The 2001 Heather Drive Landslide, Layton, Davis County, Utah (PI-88)By: A. Elliott The August 2001 Heather Drive landslide in Layton damaged six houses, forcing homeowners to evaluate them. This publication discusses the event and aftermath, as well as the geological makeup of the area in an attempt to explain why the landslide occurred....
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Earthquake fault map of a portion of Tooele County, Utah (PI-84)By: 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)By: 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)By: 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)By: 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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Landslides: What they are, why they occur (PI-74)By: 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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Rock-fall hazards (PI-69)By: 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)By: 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)By: 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)By: 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)By: 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)By: 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)By: 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)By: 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)By: 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)By: 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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Radon-hazard potential in the Ogden Valley, Weber County, Utah (PI-36)By: 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)By: 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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Radon-hazard potential in the Provo-Orem area, Utah County, Utah (PI-21)By: 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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