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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: 906

Seepage study of canals in Beaver Valley, Beaver County, Utah

A study of the gains or losses of nine canals near Beaver, Utah, was made to aid in the water allocation of the canal systems. The canals included in this study are Manderfield Ditch, Last Chance Canal, Christiansen Ditch, Mammoth Canal, City Ditch, Owens Ditch, South Field Ditch, Patterson Ditch and Aberdare Canal. Four sets of seepage measurements were made during 1974, but flow was observed in
Authors
R.W. Cruff, R. W. Mower

Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah

This report describes the study of the Rocky Point Canal system in the vicinity of Duchesne and the Grey Mountain-Pleasant Valley Canal system between Duchesne and Myton, in the Uinta Basin, Duchesne County, Utah. The Rocky Point Canal diverts from the left bank of the Duchesne River about 4 mi north of Duchesne. This canal splits into the upper Rocky Point Canal and the lower Rocky Point Canal ab
Authors
R.W. Cruff, J. W. Hood

Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado

This report presents a part of the results of an investigation of the hydrology of the northern Uinta Basin area by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources. The purpose of the report is to summarize the hydraulic and geohydrologic characteristics of the aquifers in the area.
Authors
J. W. Hood

Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah

The Pine Valley drainage basin is an area of about 730 square miles (1,890 square kilometres) in Millard, Beaver, and Iron Counties in southwestern Utah. Total annual precipitation in the basin averages about 410,000 acre-ft (acre-feet) or 506 hm3 (cubic hectometres). Less than 500 acre-ft (0.6 hm3) of runoff reaches the playa on the lowest part of the valley floor. There is no surface outflow fro
Authors
Jerry C. Stephens

Summary appraisals of the nation's ground-water resources – Great Basin region

Ground-water withdrawals by wells in the Great Basin Region were about 1.1 million acre-feet (1,360 cubic hectometres) in 1970. Most of these withdrawals were from 87 of the 234 hydrographic areas in the region. Withdrawals ranged from about 1,000 acre-feet (1.2 cubic hectometres) to more than 100,000 acre-feet (123 cubic hectometres). Jordan Valley, which includes Salt Lake City, had the largest
Authors
Thomas E. Eakin, Don Price, J. R. Harrill

Climatic and streamflow estimates for northeastern Utah

This report shows how information from 44 air-temperature, 59 precipitation, and 86 streamflow sites was converted to a common-time base of 1941-70, and how general relations were developed to extend the converted point values to unsampled sites.Two methods, regression and ratio, were used to convert the data to a common-time base. Both methods require a period of concurrent data at two sites. Aft
Authors
Fred K. Fields, D. Briane Adams

Water resources of Dinosaur National Monument, Colorado and Utah

Dinosaur National Monument, partly in the Rocky Mountain System and partly in the Colorado Plateaus physiographic province, covers an area of 322 square miles (834 square kilometres) in northwestern Colorado and northeastern Utah. The climate is generally cool and pleasant in May, early June, September, and October; winters are cold. Normal annual precipitation ranges from less than 8 to more than
Authors
C. T. Sumsion

Preliminary maps showing ground-water resources in the Lower Colorado River region, Arizona, Nevada, New Mexico, and Utah

This atlas was prepared to meet the need for information on the areal distribution, quantity, and availability of ground water in the lower Colorado River region, an area of about 140,000 square miles in parts of Arizona, Nevada, New Mexico, and Utah. The maps are necessarily generalized in places owing to the lack of sufficient data. In general the geohydrologic information pertains to large area
Authors
S. G. Brown

Salt-load computations - Colorado River, Cameo, Colorado, to Cisco, Utah

No abstract available.
Authors
Robert Brennan, Richard Ural Grozier