Geologic Resources of Summit County, Utah
Author: Miriam H. Bugden
Publisher:
Published: 1990
Total Pages: 28
ISBN-13:
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Author: Miriam H. Bugden
Publisher:
Published: 1990
Total Pages: 28
ISBN-13:
DOWNLOAD EBOOKAuthor: Hugh A. Hurlow
Publisher: Utah Geological Survey
Published: 2002
Total Pages: 60
ISBN-13: 155791656X
DOWNLOAD EBOOKThe 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
Author: Carl L. Ege
Publisher: Utah Geological Survey
Published: 2005
Total Pages: 64
ISBN-13: 1557917264
DOWNLOAD EBOOKWhether you are a geologist, history buff, or rockhound, this booklet will be a helpful guide to Utah?s mining districts. The booklet is divided up into three parts: the first part provides general information on what a mining district is, how many mining districts are in Utah, types of mineral deposits found at these districts, and landownership issues. The second part includes individual mining-district discussions containing information on location, production, history, geology, mineralogy, and current/future operations. The third part includes a glossary of geologic terms and other useful resources in the appendices, such as a descriptive list of minerals found in the districts, geologic time scale, and a list of mineral resources of the mining districts.
Author: Lehi F. Hintze
Publisher:
Published: 1973
Total Pages:
ISBN-13:
DOWNLOAD EBOOKAuthor: Francis X. Ashland
Publisher: Utah Geological Survey
Published: 2001
Total Pages: 82
ISBN-13: 1557916527
DOWNLOAD EBOOKThe purpose of this study is to provide geologic information important in assessing ground-water resources and siting water wells in the Snyderville basin. This geologic study was one phase of a cooperative and more comprehensive water-resource investigation. Subsequent phases conducted by the U.S. Geological Survey Water Resources Division (USGS WRD), focused on the hydrology of the Snyderville basin. The information presented in this report is generalized and is not intended to substitute for site-specific investigations. Future detailed studies will add to the understanding of the geology and ground-water resources of the study area and supplement the information presented herein. 59 pages + 15 plates
Author: Lehi F. Hintze
Publisher: Utah Geological Survey
Published: 2003
Total Pages: 324
ISBN-13: 1557916926
DOWNLOAD EBOOKThis bulletin serves not only to introduce the non-geologist to the rich geology of Millard County, but also to provide professional geologists with technical information on the stratigraphy, paleontology, and structural geology of the county. Millard County is unique among Utah’s counties in that it contains an exceptionally complete billion-year geologic record. This happened because until about 200 million years ago the area of present-day Millard County lay near sea level and was awash in shallow marine waters on a continental shelf upon which a stack of fossil-bearing strata more than 6 miles (10 km) thick slowly accumulated. This bulletin summarizes what is known about these strata, as well as younger rocks and surficial deposits in the county, and provides references to scientific papers that describe them in greater detail. Mountains North 30 x 60 (1:100,000-scale) quadrangles. These companion maps and this bulletin portray the geology of Millard County more completely and accurately than any previously published work.
Author: Geological Survey (U.S.)
Publisher:
Published: 1988
Total Pages: 316
ISBN-13:
DOWNLOAD EBOOKAuthor: Bryce T. Tripp
Publisher: Utah Geological Survey
Published: 2005
Total Pages: 87
ISBN-13: 1557917361
DOWNLOAD EBOOKThis project compiles basic information on the most important geologic and infrastructural factors that would be considered when planning a new high-calcium limestone quarry such as: (1) data on existing pits and prospects, (2) chemical analyses of high-calcium limestone, (3) the extent and spatial distribution of geologic formations having good potential for high-calcium limestone production, (4) references for geologic maps covering existing pits and prospects, and analytical data points, (5) locations of transportation corridors, and (6) locations of cement and lime plants, electric power plants, coal mines, and metal smelters that are large consumers of high-calcium limestone.
Author: Janae Wallace
Publisher: Utah Geological Survey
Published: 2012-01-16
Total Pages: 152
ISBN-13: 1557918538
DOWNLOAD EBOOKThis report characterizes the relationship of geology to groundwater occurrence and flow, with emphasis on determining the thickness of the valley-fill aquifer and water yielding properties of the fractured rock aquifers. Develops a water budget for the drainage basin and classifies the groundwater quality and identifies the likely sources of nitrate in groundwater.
Author: William R. Lund
Publisher: Utah Geological Survey
Published: 1990
Total Pages: 77
ISBN-13: 1557910936
DOWNLOAD EBOOKGeologic 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.