Geologic Hazards of the Magna Quadrangle, Salt Lake County, Utah PDF Download
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Author: Jessica J. Castleton Publisher: Utah Geological Survey ISBN: 155791849X Category : Hazardous geographic environments Languages : en Pages : 78
Book Description
This study contains 10 1:24,000 scale GIS based geologic hazard maps that include liquafaction, surface fault rupture, flood hazard, landslides, rock-fall, indoor radon potential, collapsible soils, expanisve soils, shallow bedrock and shallow groundwater potential. Also includes a 73 page accompanying report that describes the hazards and provides background information on data sources, the nature and distribution of hazards, and possible hazard reducation measures.
Author: Jessica J. Castleton Publisher: Utah Geological Survey ISBN: 155791849X Category : Hazardous geographic environments Languages : en Pages : 78
Book Description
This study contains 10 1:24,000 scale GIS based geologic hazard maps that include liquafaction, surface fault rupture, flood hazard, landslides, rock-fall, indoor radon potential, collapsible soils, expanisve soils, shallow bedrock and shallow groundwater potential. Also includes a 73 page accompanying report that describes the hazards and provides background information on data sources, the nature and distribution of hazards, and possible hazard reducation measures.
Author: Jessica J. Castleton Publisher: ISBN: 9781557918994 Category : Hazardous geographic environments Languages : en Pages :
Book Description
This study contains ten 1:24,000 scale GIS based geologic hazard maps that include shallow groundwater, liquefaction, surface fault rupture, flood hazards, landslides, rock-fall, collapsible soils, expansive soils, and shallow bedrock. The accompanying 24 page report describes the hazards and provides background information on data sources and the nature and distribution of hazards.
Author: Bill D. Black Publisher: Utah Geological Survey ISBN: 1557916330 Category : Geology Languages : en Pages : 75
Book Description
The petrographic database consists of 705 maceral analyses, reflectance measurements, and density and porosity determinations from Utah coal samples. These data were collected by the Utah Geological Survey from 1982 to 1995. Samples were collected from seven of Utah's 22 coal fields. Coal fields sampled are the Book Cliffs (182 samples), Wasatch Plateau (262 samples), Emery (41 samples), Sego (27 samples), Henry Mountains (173 samples), Kaiparowits Plateau (12 samples), and Coalville (four samples). The data are sorted by coal-field names; within each field the analyses are arranged alphabetically by coal-bed name to facilitate comparison. The aim of the database is to provide the industry with information on petrographic properties of Utah coals. In addition, it should help the coal operators and purchasers to determine the best uses for Utah coals.
Author: William R. Lund Publisher: Utah Geological Survey ISBN: 1557910936 Category : Engineering geology Languages : en Pages : 77
Book Description
Geologic 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 Range and the Oquirrh Mountains. The Wasatch Range is the easternmost expression of major Basin and Range extension in north-central Utah and is bounded on the west by the Wasatch fault zone (WFZ), a major zone of active normal faulting. During the late Pleistocene Epoch, the Salt Lake City region was dominated by a succession of inter-basin lakes. Lake Bonneville was the last and probably the largest of these lakes. By 11,000 yr BP, Lake Bonneville had receded to approximately the size of the present Great Salt Lake.
Author: Charles Gifford Oviatt Publisher: Utah Geological Survey ISBN: 1557918937 Category : Science Languages : en Pages : 24
Book Description
This 20-page report summarizes observations of sediments and shorelines of the Gilbert episode in the Bonneville basin of northwestern Utah. Lake Bonneville dropped to altitudes similar to those of modern Great Salt Lake by 13,000 years ago, remained low for about 1400 years, then rapidly rose about 50 ft (15 m) during the Gilbert episode (about 11,600 years ago). The Gilbert lake was probably less extensive than shown by previous mapping of the Gilbert shoreline. The lake reached altitudes of 4250-4255 ft (1295-1297 m), and its shoreline, which is not well defined anywhere in the basin, was probably not deformed by residual isostatic rebound associated with removal of the Lake Bonneville water load. Holocene Great Salt Lake has not risen as high as the Gilbert-episode lake.
Author: Jessica J. Castleton
Author: Jessica J. Castleton
Author: Jessica J. Castleton
Author: JESSICA J. CASTLETON
Author: 
Author: Bill D. Black
Author: William R. Lund
Author: Charles Gifford Oviatt
Author: Bruce N. Kaliser
Author: Geological Survey (U.S.)
Author: