Circular Utah Geological And Mineral Survey
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Circular - Utah Geological and Mineralogical Survey
Author | : Utah Geological and Mineralogical Survey |
Publisher | : |
Total Pages | : 500 |
Release | : 1968 |
Genre | : Geology |
ISBN | : |
Utah. State Dept. of Publicity and Industrial Development. Raw Materials Division. Circular
Author | : Utah Geological and Mineralogical Survey |
Publisher | : |
Total Pages | : 58 |
Release | : 1952 |
Genre | : Geology |
ISBN | : |
Guide for the Preparation of Reports for the Utah Geological Survey
Author | : William R. Lund |
Publisher | : |
Total Pages | : 88 |
Release | : 1992 |
Genre | : Government publications |
ISBN | : |
Selected Mining Districts of Utah
Author | : Carl L. Ege |
Publisher | : Utah Geological Survey |
Total Pages | : 64 |
Release | : 2005 |
Genre | : Business & Economics |
ISBN | : 1557917264 |
Whether 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.
A Summary of the Ground-water Resources and Geohydrology of Grand County, Utah
Author | : Chris Eisinger |
Publisher | : Utah Geological Survey |
Total Pages | : 36 |
Release | : 1999 |
Genre | : Science |
ISBN | : 9781557916266 |
In Grand County, ground water has been withdrawn primarily from two types of aquifers: fractured rock and unconsolidated deposits. Some of the better water-yielding rock units are grouped together into nine aquifers, including: the Lower Paleozoic aquifer, the Cutler aquifer, the Wingate aquifer, the Navajo aquifer, the Entrada aquifer, the Morrison aquifer, the Dakota aquifer, the Wasatch aquifer, and the Parachute Creek aquifer. This report summarizes published information regarding ground-water conditions in Grand County. During the preparation of this report we identified several types of information that are not presently available, but can be useful for evaluating ground-water resources, including: (1) structure contour maps showing the depth to aquifers, (2) isopach maps showing the thickness of aquifers, and (3) fracture domain maps showing the predominant orientations of rock discontinuities.
High-calcium Limestone Resources of Utah
Author | : Bryce T. Tripp |
Publisher | : Utah Geological Survey |
Total Pages | : 87 |
Release | : 2005 |
Genre | : Nature |
ISBN | : 1557917361 |
This 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.
Bulletin - Utah Geological and Mineral Survey
Author | : Utah Geological and Mineral Survey |
Publisher | : |
Total Pages | : 532 |
Release | : 1976 |
Genre | : Geology |
ISBN | : |
Rainbow of Rocks
Author | : Marjorie A. Chan |
Publisher | : Utah Geological Survey |
Total Pages | : 20 |
Release | : 2002-10 |
Genre | : Science |
ISBN | : 1557916810 |
Sunrise illuminates Colorado Plateau’s canyon country. In the early morning light, cliffs radiate a rich red glow, and a sculptured panorama of sandstone is revealed in a rich palette of crimson, vermilion, orange, salmon, peach, pink, gold, yellow, and white. Nearby are black, spherical rock marbles (iron concretions) collecting in small depressions, like puddles of ball bearings. These natural spherical balls have been called various names such as iron nodules, iron sandstone balls, or moki marbles. However, we use the name “iron concretion” to describe both the composition (iron oxide that is the dark mineral which cements the sandstone grains) and the formed shape (concretion). What paints the sandstone such rich colors? Why is red a dominant color? Where do the black marbles come from? How did the black marbles form? Is there a relationship between sandstone colors and the marbles? This booklet explores the answers to these questions and poses other questions yet unanswered.