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Ground-water resources and simulated effects of withdrawals in the East Shore area of Great Salt Lake, Utah (TP-93)By: David W. Clark, Cynthia L. Appel, Patrick M. Lambert, and Robert L. Puryear The ground-water resources in the East Shore area of Great Salt Lake, Utah, were studied to better define the ground-water system; to document changes in ground-water levels, quality, and storage;...
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Seepage Study of a 15.3-Mile Section of the Central Utah Canal, Pahvant Valley, Millard County, Utah (TP-91)By: M. Enright Three sets of seepage measurements were made at ten canal sites and at all turnouts along a 15. 3-mile section of the Central Utah Canal during the summer of 1986. This report gives the results of seepage measurements of a 15....
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Seepage Studies of the Weber River and the Davis-Weber and Ogden Valley Canals, Davis and Weber Counties, Utah (TP-90)By: L. R. Herbert, R. W. Cruff, D. W. Clark, and C. Avery Ogden Valley canal in Davis and Weber Counties, Utah, were made to determine gains or losses of flow in those reaches. Three to five sets of seepage measurements were made on...
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Chemical Quality of Ground Water in Salt Lake Valley, Utah (TP-89)By: K. M. Waddell, R. L. Seiler, and D. K. Solomon During 1979-84, 35 wells completed in the principal aquifer in the Salt Lake Valley, Utah, that had been sampled during 1962-67 were resampled to determine if water-quality changes had occurred. The dissolved-solids concentration...
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Bedrock Aquifers of Eastern San Juan County, Utah (TP-86)By: C. Avery This study is one of a series of studies appraising the water-bearing properties of the Navajo Sandstone and associated formations in southern Utah. Some of the water-yielding formations are grouped into aquifer systems. The C aquifer is comprised of the DeChelly...
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Ground-Water Conditions in the Lake Powell Area, Utah (TP-84)By: P. J. Blanchard The Lake Powell area comprises about 2,450 square miles in south-central Utah. It is subdivided into three geographical areas by the Colorado and San Juan Rivers. The Henry Mountains area is north of the Colorado River, the Navajo Mountain area...
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Reconnaissance of the Quality of Surface Water in the Upper Virgin River Basin, Utah, Arizona, and Nevada (TP-83)By: P. J. Blanchard The Virgin River drainage from headwaters in Utah to Littlefield, Arizona, has an area of about 5,090 square miles in southwestern Utah, northwestern Arizona, and southeastern Nevada. In this area the river is about 110 miles long and receives water...
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Seepage Study of Six Canals in Salt Lake County, Utah (TP-82)By: G. W. Sandberg and L. G. Sultz A study of selected reaches of the Utah and Salt Lake, Utah Lake Distributing, Provo Reservoir, Draper Irrigation, East Jordan, and Jordan and Salt Lake City Canals in Salt Lake County, Utah, was made to determine...
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Ground-Water Conditions in the Kaiparowits Plateau Area, Utah and Arizona, with Emphasis on the Navajo Sandstone (TP-81)By: L. R. Herbert, R. W. Cruff, and K. M. Waddell The Kaiparowits Plateau area is located in central Garfield and eastern Kane Counties of Utah and north-central Coconino County of Arizona. The area covers about 4,850 square miles and includes the drainages of...
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Ground-Water Hydrology and Projected Effects of Ground-Water Withdrawals in the Sevier Desert, Utah (TP-79)By: W. F. Holmes The principal ground-water reservoir in the Sevier Desert is the unconsolidated basin fill. The fill has been divided generally into aquifers and confining beds, although there are no clear-cut boundaries between these units--the primary aquifers are the shallow and deep...
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Ground-Water Reconnaissance of the Central Weber River Area, Morgan and Summit Counties, Utah (TP-77)By: J. S. Gates, J. I. Steiger, and R. T. Green Ground water occurs in unconsolidated alluvium and older semiconsolidated to consolidated rocks; it has been developed to a limited extent for public, industrial, and domestic use. Alluvium of Quaternary age probably is the...
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Reconnaissance of the Quality of Surface Water in the Weber River Basin, Utah (TP-76)By: K. R. Thompson This reconnaissance of the quality of surface water in the Weber River basin encompassed an area of 2,080 square miles. Elevations in the basin range from 4,210 to 11,708 feet. The water-distribution system on the Weber River is well developed....
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Consumptive Use and Water Requirements for Utah (TP-75)By: A. L. Huber, F. W. Haws, T. C. Hughes, J. M. Bagley, K. G Hubbard, and E. A. Richardson Reliable guides or standards for estimating water requirements are essential for the planning, design, and operation of any water using enterprise. Particularly in a...
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Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water (TP-73)An investigation of the water resources of the Beryl-Enterprise area, Escalante Desert, Utah (pl. 1), was made during 1976-78 as part of a cooperative program with the Utah Department of Natural Resources, Division of Water Rights. Wells were the most important source of water...
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Reconnaissance of the Quality of Surface Water in the San Rafael River Basin, Utah (TP-72)By: J. C. Mundorff and K. R. Thompson The water-quality reconnaissance of the San Rafael River basin, Utah, encompassed an area of about 2,300 square miles. Data were obtained by the U.S. Geological Survey one or more times at 116 sites from June 1977...
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Hydrologic Reconnaissance of the Southern Great Salt Lake Desert and Summary of the Hydrology of West-Central Utah (TP-71)By: J. S. Gates and S. A. Kruer The southern Great Salt Lake Desert includes an area of about 2,600 square miles, more than 70 percent of which is barren, saline mudflats or salt flats. Great Salt Lake is the remnant of Lake Bonneville...
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Status of Development of Selected Ground-Water Basins in Utah (TP-7)By: H. E. Thomas, W. B. Helson, B. E. Lofgren, and R. G. Butler Utah's ground-water law, which became effective on March 22, 1935, has its basis in certain statutes passed by the Utah Legislature during its 1935 session, with minor additions or revisions...
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Bedrock Aquifers in the Lower Dirty Devil River Basin Area, Utah, with Special Emphasis on the Navaho Sandstone (TP-68)By: J. W. Hood and T. W. DanielsonThe lower Dirty Devil River basin area in southeastern Utah has an area of about 4,300 square miles and ranges in altitude from about 3,700 to more than 11,000 feet above mean sea level. Precipitation, the main...
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Seepage Study of the West Side and West Canals, Box Elder County, Utah (TP-67)By: R. W. CruffA study of the gains or losses of the West Side and West Canals from Cutler Reservoir to near Penrose, Box Elder County, Utah, was made to aid in water allocation for the canal system. Four sets of seepage measurements made...
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Aquifer Tests of the Navajo Sandstone New Caineville, Wayne County, Utah (TP-66)By: J. W. Hood and T. W. DanielsonGround water in the Navajo Sandstone near Caineville, Wayne County, Utah, was studied during 1975-77 as part of an investigation of water in bedrock in the lower Dirty Devil River basin area. The purpose of the study...
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