Geology And Scenery Of The Central Wasatch Range Salt Lake And Summit Counties Utah PDF Download

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Geology and Scenery of the Central Wasatch Range, Salt Lake and Summit Counties, Utah

Geology and Scenery of the Central Wasatch Range, Salt Lake and Summit Counties, Utah
Author: Miriam H. Bugden
Publisher: Utah Geological Survey
Total Pages: 20
Release: 1991-01-15
Genre: Geology
ISBN: 1557913420

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This self-guided geologic trip will lead you through times when inland seas, ancient mountains, vast mud flats, sandy deserts, and massive glaciers ruled Utah's landscape. You will learn how colliding crustal plates changed Utah's face, how the metallic ores of the Park City and Big Cottonwood Canyon mining districts formed, how regional geological structures affect our local geology, and why the sheer walls of Big Cottonwood Canyon are so different from the tame, rolling hills of the Park City area.


Geologic Guide to the Central Wasatch Front Canyons, Salt Lake County, Utah

Geologic Guide to the Central Wasatch Front Canyons, Salt Lake County, Utah
Author: Utah Geological Survey Staff
Publisher: Utah Geological Survey
Total Pages: 18
Release: 2005-09
Genre: Science
ISBN: 1557917221

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Striking beauty, abundant recreational opportunities, historic mining and pioneer locales, and a unique geologic story stretching back over one billion years make Salt Lake County’s Wasatch Front canyons a world-class attraction. This guide highlights the six canyons open to vehicles. Topical pages present the region’s fascinating geologic history and active processes, while descriptions and maps with road mileage further explain each canyon’s geology.


Engineering Geology of the Salt Lake City Metropolitan Area, Utah

Engineering Geology of the Salt Lake City Metropolitan Area, Utah
Author: William R. Lund
Publisher: Utah Geological Survey
Total Pages: 77
Release: 1990
Genre: Engineering geology
ISBN: 1557910936

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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.


Geology of Utah

Geology of Utah
Author: William Lee Stokes
Publisher:
Total Pages: 342
Release: 1986
Genre: Geology
ISBN:

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Consensus Preferred Recurrence-interval and Vertical Slip-rate Estimates

Consensus Preferred Recurrence-interval and Vertical Slip-rate Estimates
Author: William R. Lund
Publisher: Utah Geological Survey
Total Pages: 114
Release: 2005-06-30
Genre: Science
ISBN: 1557917272

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This report presents the results of the Utah Quaternary Fault Parameters Working Group (hereafter referred to as the Working Group) review and evaluation of Utah’s Quaternary fault paleoseismic-trenching data. The purpose of the review was to (1) critically evaluate the accuracy and completeness of the paleoseismictrenching data, particularly regarding earthquake timing and displacement, (2) where the data permit, assign consensus, preferred recurrence-interval (RI) and vertical slip-rate (VSR) estimates with appropriate confidence limits to the faults/fault sections under review, and (3) identify critical gaps in the paleoseismic data and recommend where and what kinds of additional paleoseismic studies should be performed to ensure that Utah’s earthquake hazard is adequately documented and understood. It is important to note that, with the exception of the Great Salt Lake fault zone, the Working Group’s review was limited to faults/fault sections having paleoseismic-trenching data. Most Quaternary faults/fault sections in Utah have not been trenched, but many have RI and VSR estimates based on tectonic geomorphology or other non-trench-derived studies. Black and others compiled the RI and VSR data for Utah’s Quaternary faults, both those with and without trenches.