Geologic Hazards
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Vendor: Utah Geological SurveyBy: H. H. Doelling, F. D. Davis, and C. J. Brandt Kane County, with its 4105 square miles, lies along the south-central margin of Utah and is found in the western part of the Colorado Plateaus physiographic province. It is famous for scenic beauty...
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Vendor: Utah Geological SurveyBy: B. D. Black, B. J. Solomon, and K. M. Harty Geologic hazards are naturally occurring geologic processes that present a risk to life and property. Tooele County is subject to many geologic hazards that need to be identified and considered prior to development....
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Vendor: Utah Geological SurveyBy: M. D. Hylland and M. Lowe The Farmington Siding landslide complex is in Davis County, Utah, about 25 kilometers north of Salt Lake City. The landslide complex covers approximately 19.5 square kilometers and is one of 13 late Pleistocene/Holocene features along the Wasatch...
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Vendor: Utah Geological SurveyBy: H. E. Gill and W. R. LundPark City began as a mining community in the late 1860s and mining continued actively in the area for more than 100 years. In the 1970s skiing surpassed mining as the major industry in the area. Due...
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Vendor: Utah Geological SurveyBy: C. G. Oviatt, J. F. Shroder, and R. E. Sewell The Colorado Plateau is a unique area for the study of Quaternary deposits and processes since it has been the site of continuous stream downcutting, cliff retreat, and landscape denudation during much of...
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Vendor: Utah Geological SurveyBy: W. R. Lund, T. R. Knudsen, G. S. Vice, and L. M. ShawThe St. George-Hurricane metropolitan area is one of the nation?s fastest growing regions. As land well suited for development becomes increasingly scarce, urbanization has moved into less favorable areas where geologic...
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Vendor: Utah Geological SurveyBy: G. N. McDonald and F. X. Ashland Contains a 41-page report and a 1:150,000-scale map defining seismic site conditions for the Wasatch Front urban corridor. This mapping, partially funded through the U.S. Geological Survey’s National Hazards Reduction Program, provides a basis for predicting...
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Vendor: Utah Geological SurveyBy: W. R. Lund, C. B. DuRoss, S. M. Kirby, G. N. McDonald, G. Hunt, and G. S. Vice Contains a 30-page report and 37-photo appendix of an investigation by the Utah Geological Survey of five recently discovered earth fissures in southwestern Utah. The...
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Vendor: Utah Geological SurveyBy: F. X. Ashland The majority of the 1998 Wasatch Front landslides were likely triggered following a cumulative rise in ground-water levels resulting from four or more successive years of above-normal precipitation. Triggering of landslide movement likely coincided with a transient ground-water-level rise associated...
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Vendor: Utah Geological SurveyBy: UGS Staff This map shows the location of faults in Davis 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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Vendor: Utah Geological SurveyBy: Mark MilliganEarthquake-triggered liquefaction can cause extensive damage and loss of life. While Utah has historically experienced liquefaction-producing earthquakes, it has thus far escaped significant damage. However, the densely populated Wasatch Front region has a 93% probability of one or more earthquakes capable of...
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Vendor: Utah Geological SurveyDuring the 1980s engineers and geologists with the Utah State University Department of Civil and Environmental Engineering, and Dames and Moore prepared a series of liquefaction potential maps for parts of Utah. Five separate reports cover the urbanized Wasatch Front counties and other valley...
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Vendor: Utah Geological SurveyBy: R. L. Owens and K. M. Rollins Soil collapse is usually associated with human activities such as irrigation, construction of canals, or disposal of wastewater that introduce water into a relatively dry environment. Although soil collapse is generally not life threatening, it can...
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Vendor: Utah Geological SurveyBy: B. N. Kaliser Twenty-four counties in Utah were surveyed in 1983-84 to compile this summary of known geological events related to the 1983 wet year. It is hoped that this summary and the one by Davis will provide a data base that is...
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Vendor: Utah Geological SurveyBy: B. N. Kaliser and J. E. Slossen Geologic consequences of the abnormally wet year of 1983 were unprecedented in number, magnitude, and geographic distribution in the l36-year history of Utah. That year was preceded by an extraordinarily wet 1982 so that antecedent moisture...
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Vendor: Utah Geological SurveyBy: M. W. Halling, J. R. Keaton, L. R. Anderson, and W. Kohler Maximum ground motion maps for the State of Utah were prepared for the Utah Department of Transportation to provide context for probabilistic ground motion maps. Deterministic procedures were used to prepare...
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Vendor: Utah Geological SurveyBy: A. H. Elliot and K. M. Harty Significant economic losses are associated with landslides, and Utah has numerous landslides and landslide-prone geologic units. Exposure to landslide hazards increases as development expands onto hillsides and other landslide-prone areas. To improve the understanding of landslides...
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Vendor: Utah Geological SurveyBy: G. E. Christenson, editor Ground shaking and slope failures were the dominant geologic effects associated with the September 2, 1992 St. George earthquake. Ground shaking caused damage to buildings in Hurricane, La Verkin, Washington, St. George, and other. A destructive landslide in the...
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Vendor: Utah Geological SurveyBy: G. E. Christenson The purpose of geologic hazards ordinances is to encourage prudent land uses in areas of geologic hazards for the protection of the health, safety, and property of the citizens of the city or county enacting the ordinance. Geologic hazards can...
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Vendor: Utah Geological SurveyBy: W. R. Lund, editorGeologic exposures in the Salt Lake City region record a long history of sedimentation and tectonic activity extending back to the Precambrian Era. Today, the city lies above a deep, sediment-filled basin flanked by two uplifted range blocks, the Wasatch...
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