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Geology of the Cordilleran Hingeline

Geology of the Cordilleran Hingeline
Author: Rocky Mountain Association of Geologists
Publisher:
Total Pages: 440
Release: 1976
Genre: Science
ISBN:

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The Geology of the Kamas-Coalville Region, Summit County, Utah, and Its Relation to Ground-water Conditions

The Geology of the Kamas-Coalville Region, Summit County, Utah, and Its Relation to Ground-water Conditions
Author: Hugh A. Hurlow
Publisher: Utah Geological Survey
Total Pages: 60
Release: 2002
Genre: Geology
ISBN: 155791656X

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The Kamas-Coalville region is in the Middle Rocky Mountains physiographic province, about 30 miles east of the Wasatch Front urban area. Rapid population growth and increased water use are the impetus for a collaborative study of water resources in the Kamas-Coalville region, which includes geologic and hydrologic components. This study describes the geologic framework of the Kamas-Coalville region, emphasizing geologic features that most strongly influence ground-water occurrence, flow, and development. The main topics include: (1) the stratigraphy and structural geology of bedrock, (2) the nature and geometry of unconsolidated deposits in Kamas Valley, (3) the hydrostratigraphy of the study area, and (4) the structure of bedrock units below Kamas Valley. 55 pages + 15 plates


The Geology of Kane County, Utah

The Geology of Kane County, Utah
Author: Hellmut H. Doelling
Publisher: Utah Geological Survey
Total Pages: 204
Release: 1989-01-25
Genre: Faults (Geology)
ISBN: 155791091X

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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 displayed in its colorful rock formations and other geologic features such as faults, folds, arches, monoclines, joints, cross beds, cliffs, lava fields, and canyons. Kane County contains parts of Bryce and Zion National Parks, the Glen Canyon Recreation Area, and it is home to the Coral Pink Sand Dunes and Kodachrome Basin State Parks. The county area has had an interesting geologic history and important fossil finds have added much to our knowledge of world geology. The total value of the mineral production of Kane County, Utah through 1985 is estimated at $21,854,000, of which more than 95 percent is attributed to construction materials, mined or quarried to build and maintain highways. Sand and gravel, crushed stone, coal, gemstones, pumice and volcanic ash, manganese ore, gold, uranium, silver, copper and lead were or have been produced, with the most important current commodities being construction and gem materials. The annual rate of production of these items is erratic, but the value averages a few hundred thousand dollars annually. The production of the construction materials is dependent on the schedules of the Utah Department of Transportation and other road building agencies. Gem materials are mined intermittently to supply the tourist trade. Currently, there are no large, regularly producing mining operations in the county. Other mineral deposits reported in Kane County include titanium and zirconium, gypsum and anhydrite, limestone and dolomite, clay, and vanadium. About 29 tests for petroleum have thus far been drilled without significant success. However, many had interesting shows of oil and gas and the potential for discovery remains high. 192 pages + 10 plates


Geology, Ore Deposits, and History of the Big Cottonwood Mining District, Salt Lake County, Utah

Geology, Ore Deposits, and History of the Big Cottonwood Mining District, Salt Lake County, Utah
Author: Laurence P. James
Publisher: Utah Geological Survey
Total Pages: 109
Release: 1979
Genre: Geology
ISBN: 1557910812

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The Big Cottonwood area lies in the highest portion of the Wasatch Mountains southeast of Salt Lake City. It contains exposed geologic features developed during two billion years of earth history. Discoveries of small but rich mineral deposits within the area led to a colorful, moderately productive, century-long period of metal mining. While there is no mining activity in the Big Cottonwood mining district today, the area is of considerable interest to students of regional geology and to numerous visitors to the mountain recreational areas. Major thrust faulting is well exposed in outcrops and in mine workings and is of economic importance on a regional scale. The unusual occurrence of the major ore bodies, at the intersections of steep fissure veins with several overthrust planes, similar to that of deposits mined in the adjoining Little Cottonwood (Alta) and American Fork districts to the south, is a classic regional feature. The small deposits in the older Precambrian rocks at the eastern edge of the district present features not seen elsewhere in the state. This report presents new detail on these and other aspects of the geology of the district, and records available geology and history of the many formerly-active underground mines. It presents an update on regional geology. It is written for readers of many interests, not merely for economic geologists. 98 pages + 4 plates


U.S. Geological Survey Bulletin

U.S. Geological Survey Bulletin
Author: John A. Karachewski
Publisher:
Total Pages: 230
Release: 1983
Genre: Geology
ISBN:

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Interaction of the Rocky Mountain Foreland and the Cordilleran Thrust Belt

Interaction of the Rocky Mountain Foreland and the Cordilleran Thrust Belt
Author: Christopher J. Schmidt
Publisher: Geological Society of America
Total Pages: 637
Release: 1988
Genre: Science
ISBN: 0813711711

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This volume emphasizes the interaction of the Cordilleran thrust belt and Rocky Mountain foreland in studies of regional structural geology, geophysics, and sedimentology from west-central Montana to Arizona. The volume outlines how the nature of the Rocky mountain foreland and its deformation affect the geometry of the Cordilleran thrust belt. Many of the structural and geophysical studies reported in this volume also address the question of which structures - forland or thrust belt - developed first in a specific region and how early formed structures influenced later ones. Several chapters address the nature and style of foreland development.


The Role of Salt in the Structural Development of Central Utah

The Role of Salt in the Structural Development of Central Utah
Author: Irving Jerome Witkind
Publisher:
Total Pages: 164
Release: 1994
Genre: Arapien Shale (Utah)
ISBN:

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Multiple episodes of diapirism, probably salt-generated, have determined the structural pattern of central Utah. The causative salt and other evaporites are integral components of the Arapien Shale of Middle Jurassic age, one of the most unusual stratigraphic units in central Utah.