Publications
This list of Water Resources Mission Area publications includes both official USGS publications and journal articles authored by our scientists. A searchable database of all USGS publications can be accessed at the USGS Publications Warehouse.
Filter Total Items: 18418
Selected hydrologic data, lower Bear River drainage basin, Box Elder County, Utah
This report presents selected basic data from a study of the ground- water resources of the lower Bear River drainage basin, Box Elder County, Utah. The study was made during 1970-72 by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. Incorporated in this report are data collected by the Geological Survey and by other organizations
Authors
L.J. Bjorklund, L. J. McGreevy
Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972
No abstract available.
Authors
Celso Puente
Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971
No abstract available.
Authors
R.D. Steger
Ground water in selected areas in the Klamath Basin, Oregon
GROUNDWATER FEATURES OF SIX LOWLAND AREAS IN THE KLAMATH BASIN OF OREGON--KLAMATH MARSH AREA, AND SPRAGUE RIVER, SWAN LAKE, YONNA, POE, AND LANGELL VALLEYS--ARE DESCRIBED. RUGGED MOUNTAINS AND RIDGES SURROUND AND SEPARATE THESE LOWLANDS WHERE FLOORS RANGE IN ALTITUDE FROM 4,100 FEET IN POE VALLEY TO 4,600 FEET NORTH OF KLAMATH MARSH. THE SIX AREAS EXTEND OVER A NORTH-SOUTH DISTANCE OF 70 MILES, AN
Authors
A.R. Leonard, A.B. Harris
Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971
No abstract available.
Authors
B.C. Massey
Floods in Iowa: Technical manual for estimating their magnitude and frequency
No abstract available.
Authors
Oscar G. Lara
The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin
The Pine and Popple Rivers, virtually unaltered by man, flow through a semiprimitive area of forests, lakes, and glacial hills. White-water streams, natural lakes, fish and animal life, and abundant vegetation contribute to the unique recreational and aesthetic characteristics of the area. Resource planning or development should recognize the interrelationships within the hydrologic system and the
Authors
Edward L. Oakes, Stephen J. Field, Lawrence P. Seeger
Water resources and geology of Mount Rushmore National Memorial, South Dakota
Ground water suitable for public supply can be obtained from fractured metamorphic and igneous rooks at Mount Rushmore National Memorial, S. Dak.
The memorial comprises three main drainage basins: Starling basin, Lafferty Gulch basin, and East Boundary basin. Ground water is most prevalent in Lafferty Gulch basin but Starling basin contributes the most surface water.
The total water supply was obt
Authors
J.E. Powell, James Jennings Norton, D. G. Adolphson
Improvement of trout streams in Wisconsin by augmenting low flows with ground water
Approximately 2 cubic feet per second of ground water were introduced into the Little Plover River in 1968 when natural streamflow ranged from 3 to 4 cubic feet per second. These augmentation flows were retained undiminished through the 2-mile reach of stream monitored. Maximum stream temperatures were reduced as much as 5?F (3?C) at the augmentation site during the test period, although changes b
Authors
R.P. Novitzki
Chemical quality of surface water in the Flaming Gorge Reservoir area, Wyoming and Utah
Construction of Flaming Gorge Dam on the Green River by the U.S. Bureau of Reclamation started in 1959, and storage began in November 1962. A reconnaissance study was made during the period 1966-68 to determine the effects of the reservoir on the chemical quality of the effluent water and to describe the quality of the impounded water and inflowing water.The major inflow to the reservoir is from t
Authors
R. J. Madison, Kidd M. Waddell
Water resources of the Big Sioux River Valley near Sioux Falls, South Dakota
The major sources of water in the Big Sioux River valley between Sioux Falls and Dell Rapids, S.Dak., are the Big Sioux River and the glacial outwash aquifer beneath the flood plain. The river and the aquifer are hydraulically connected.
The Big Sioux River has an average annual discharge of 246 cubic feet per second, on the average exceeds bankfull stage every 2.3 years, and has moderate basin st
Authors
Donald G. Jorgensen, Earl A. Ackroyd