Publications
The majority of publications in this section address water resources in Utah or in bordering states. Some of the publications are included because one or more of the authors work at the Utah Water Science Center but have provided expertise to studies in other geographic areas.
Filter Total Items: 916
Quality of surface water in the Sevier Lake basin, Utah Quality of surface water in the Sevier Lake basin, Utah
Few data are available on the quality of surface waters in the Sevier Lake basin. Because of the need for information not only on the chemical-quality but also on the other water-quality characteristics of the basin, the U.S. Geological Survey, as part of its cooperative program with the Utah State Engineer, evaluated the available data in 1963. Based on this evaluation, a reconnaissance...
Authors
D. C. Hahl, R.E. Cabell
Reevaluation of the ground-water resources of Tooele Valley, Utah Reevaluation of the ground-water resources of Tooele Valley, Utah
This study of the geohydrology of Tooele Valley, Utah, was made by the U.S. Geological Survey in cooperation with the Utah State Engineer during the period 1958-63. The purpose of the study was to update an earlier investigation of ground water in Tooele Valley made by the Geological Survey during 1940-42 (Thomas, 1946). The construction of approximately 256 wells in the valley since...
Authors
Joseph S. Gates
Water-resources appraisal of the Snake Valley area, Utah and Nevada Water-resources appraisal of the Snake Valley area, Utah and Nevada
The Snake Valley area is a north-trending narrow depression that extends about 135 miles along the central Nevada-Utah border. The area covers about 3,480 square miles. Within the area, the principal ground-water reservoir is in the unconsolidated deposits of Quaternary and Tertiary age that underlie about 1.2 million acres. Carbonate rocks of Paleozoic age may form another reservoir...
Authors
James W. Hood, F. Eugene Rush
Water resources of the Upper Colorado River Basin - Technical report Water resources of the Upper Colorado River Basin - Technical report
No abstract available.
Authors
William Vaughn Iorns, Charles Herbert Hembree, Godfrey L. Oakland
Ground-water resources of Pavant Valley, Utah Ground-water resources of Pavant Valley, Utah
Pavant Valley, in eastern Millard County in west-central Utah, is in the Great Basin section of the Basin and Range province. The area of investigation is 34 miles long from north to south and 9 miles wide from east to west and comprises about 300 square miles. Agriculture, tourist trade, and mining are the principal industries. The population of the valley is about 3,500, of which about...
Authors
R. W. Mower
Calcium, sodium, sulfate, and chloride in stream water of the western conterminous United States to 1957 Calcium, sodium, sulfate, and chloride in stream water of the western conterminous United States to 1957
This Hydrologic Atlas shows concentrations of calcium, sodium (or sodium plus potassium), sulfate, and chloride in stream water of 11 of the Western States, regardless of the sources from which the mineral constituents came. The maps are, in a sense, a historical summary, showing concentrations observed to 1956 and reported in published references. Data on chemical quality of stream...
Authors
John Henry Frederick Feth
Selected hydrologic data, upper Sevier River basin, Utah Selected hydrologic data, upper Sevier River basin, Utah
This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later. Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation...
Authors
Carl H. Carpenter, Gerald B. Robinson, Louis Jay Bjorklund
Chemical composition of snow in the northern Sierra Nevada and other areas Chemical composition of snow in the northern Sierra Nevada and other areas
Melting snow provides a large part of the water used throughout the western conterminous United States for agriculture, industry, and domestic supply. It is an active agent in chemical weathering, supplies moisture for forest growth, and sustains fish and wildlife. Despite its importance, virtually nothing has been known of the chemical character of snow in the western mountains until...
Authors
John Henry Frederick Feth, S. M. Rogers, Charles Elmer Roberson
Developing a state water plan: Ground-water conditions in Utah, spring of 1964 Developing a state water plan: Ground-water conditions in Utah, spring of 1964
This report is the first in a series of annual reports which will describe ground-water conditions in Utah. It was prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and was designed to provide the data for interested parties, such as legislators, administrators, and planners to keep abreast of changing ground-water conditions in the state. Because...
Authors
Ted Arnow, R.G. Butler, R. W. Mower, Joseph S. Gates, R.M. Cordova, C.H. Carpenter, L.J. Bjorklund, R.D. Feltis, G.B. Robinson, G. W. Sandberg
Summary of floods in the United States during 1959 Summary of floods in the United States during 1959
This report describes the most outstanding floods that occurred in the United States during 1959. The floods of January-February in Ohio and adjacent States were the most outstanding floods of the year 1959 with respect to area affected, number of streams having maximum discharge of record, rare occurrence of peaks, and great amount of damage caused. Floods in the Rock River basin in...
Authors
E. L. Hendricks
Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report
During the 1960 and 1961 water years an annual load of about 2 million tons of dissolved minerals was contributed to the Great Salt Lake area by surficial sources. Almost 60 percent of this load was sodium and chloride. Of the six units contributing to the lake area, three - the Bear River, the Jordan River, and the unit comprising drains and sewage canals – contributed about three...
Authors
D. C. Hahl, R.H. Langford