Flood boundaries and water-surface profile for the computed 100-year flood, Swift Creek at Afton, Wyoming, 1986
James G. Rankl, Joe C. Wallace
1989, Water-Resources Investigations Report 88-4064
Flood flows on Swift Creek near Afton, Wyoming, were analyzed. Peak discharge with an average recurrence interval of 100 years was computed and used to determine the flood boundaries and water surface profile in the study reach. The study was done in cooperation with Lincoln County and the Town of...
Programs and activities of the Kentucky District, Water Resources Division, U.S. Geological Survey
Lloyd H. Woosley (compiler), Robert J. Faust
1989, Open-File Report 89-50
Statistical analysis relating well yield to construction practices and siting of wells in the Piedmont and Blue Ridge provinces of North Carolina
Charles C. Daniel
1989, Water Supply Paper 2341-A
A statistical analysis was made of data from more than 6,200 water wells drilled in the fractured crystalline rocks of the Blue Ridge, Piedmont, and western edge of the Coastal Plain where crystalline rocks underlie sediments at shallow depths. The study area encompassed 65 counties in western North Carolina, an...
Water resources data for Utah, water year 1988
M. D. ReMillard, L. R. Herbert, G. W. Sandberg, G. A. Birdwell
1989, Water Data Report UT-88-1
No abstract available....
Bibliography of Water-Resources Investigations reports published by the U.S. Geological Survey from 1971 through 1982
Sharon A. Edmonds
1989, Open-File Report 89-69
This report contains a cross-referenced listing of 971 Water-Resources Investigations reports (WRIR's) published by the U.S. Geological Survey from 1971 through 1982. The reports are listed by WRIR number. Most requests for WRIR 's generally are by WRIR number; however, the Survey 's annual catalog, ' Publications of the U.S....
Chemical quality of agricultural drainage water tributary to Kesterson Reservoir, Fresno and Merced counties, California, January and August 1984
John A. Izbicki
1989, Open-File Report 87-380
Water resources data, Massachusetts and Rhode Island, water year 1987
R. A. Gadoury, R.S. Socolow, D. J. Kent, J.P. Russell
1989, Water Data Report MA-RI-87-1
Water-resources data for the 1987 water year for Massachusetts and Rhode Island consists of records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 96 gaging stations, monthend contents for 30 lakes and reservoirs, water quality for...
Applicability of ambient toxicity testing to national or regional water-quality assessment
J. F. Elder
1989, Open-File Report 89-55
Comprehensive assessment of the quality of natural waters requires a multifaceted approach. Based on experimentation designed to monitor responses of organisms to environmental stresses, toxicity testing may have diverse purposes in water quality assessments. These purposes may include identification that warrant further study because of poor water quality or unusual...
Water-resources activities of the U.S. Geological Survey in Wyoming, fiscal years 1988 and 1989
D. M. Oden (compiler)
1989, Open-File Report 89-262
There are two types of water-resources activities of the U.S. Geological Survey in Wyoming: collection of hydrologic data, and water-resources-appraisal projects. During Fiscal Years 1988 and 1989, the work was done in cooperation with 10 State agencies, 5 counties, 3 cities, 2 towns, 1 irrigation district, 2 Indian Tribes, and...
Climatic changes inferred from analyses of lake-sediment cores, Walker Lake, Nevada
I.C. Yang
1989, Water-Resources Investigations Report 89-4006
Suspended sediment and sediment-source areas in the Fountain Creek drainage basin upstream from Widefield, southeastern Colorado
Paul Von Guerard
1989, Water-Resources Investigations Report 88-4136
Suspended-sediment samples were collected from synoptic-sampling sites to determine suspended-sediment concentrations, loads, yields, and sediment-source areas in the Fountain Creek drainage basin upstream from Widefield, Colorado. Suspended-sediment yields ranged from 0.004 to 278 tons/sq mi/day. Twenty-four sites were sampled that represent urban and rural land use. The median suspended-sediment yield...
Sediment-transport characteristics and effects of sediment transport on benthic invertebrates in the Fountain Creek drainage basin upstream from Widefield, southeastern Colorado, 1985-88
Paul Von Guerard
1989, Water-Resources Investigations Report 89-4161
Sediment and benthic-invertebrate data were collected during water years 1985 through 1988 in the Fountain Creek drainage basin upstream from Widefield, Colorado. Sediment data collected include suspended-sediment concentrations and particle size analysis of suspended sediment, bedload, and bed material. Sediment-transport equations were derived for total suspended-sediment discharge and suspended-sand discharge...
Ground-water resources of selected high volcanic islands of Truk with emphasis on small village supplies
K. J. Takasaki
1989, Water-Resources Investigations Report 88-4163
Existing water supply sources in the Truk State were assessed. The first part of the assessment includes the high islands in the Truk Lagoon and the second part includes the principal inhabited outer islands of the Truk State. The high islands in the lagoons are remnant peaks of a partly...
Final revised analyses of major and trace elements from acid mine waters in the Leviathan Mine drainage basin, California and Nevada — October 1981 to October 1982
J.W. Ball, D. Kirk Nordstrom
1989, Water-Resources Investigations Report 89-4138
No abstract available....
Hydraulic data for shallow open-channel flow in a high-gradient flume with large bed material
Fred J. Watts
1989, Water-Resources Investigations Report 89-4001
Hydraulic data for shallow open-channel flow in a high-gradient flume with large bed material are reported. The bed surface consists of natural rock having particle-size range of 0.15 to 0.75 ft. Two different bed-surface configuration (roughness) were tested. The bed material was stable for all discharges. The flume wall was...
Selected ground-water quality data for the area near Fort Hall, Fort Hall Indian Reservation, southeastern Idaho, June 1989
D. J. Parliman, H.W. Young
1989, Open-File Report 89-594
The areal extent of anomalously high dissolved nitrogen concentrations in groundwater near Fort Hall on the Fort Hall Indian Reservation, Idaho is shown on a map. The study area includes that part of the reservation west of the Fort Hall Main Canal in townships 3, 4, and 5 south, ranges...
Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee
Patrick Tucci, D. W. Hanchar
1989, Water-Resources Investigations Report 88-4197
Nineteen wells were installed at nine sites in the Melton Valley area. The wells are intended to provide information on water levels in both regolith and bedrock, aquifer characteristics, and subsurface lithology. Well depths range from 24 to 86 ft for shallow wells, and from 126 to 301 ft for...
External quality-assurance results for the National Atmospheric Deposition Program and the National Trends Network during 1987
R.B. See, L.J. Schroder, T. C. Willoughby
1989, Water-Resources Investigations Report 89-4015
Summary of water-resources activities of the U.S. Geological Survey in Oregon: Fiscal year 1989
David A. Curtiss
1989, Open-File Report 89-242
No abstract available....
Quality of water from public-supply wells in principal aquifers of Illinois, 1984-87
David C. Voelker
1989, Water-Resources Investigations Report 88-4111
The quality of water from public-supply wells that tap the principal aquifers in Illinois are summarized. Water quality data collected during the study included inorganic and volatile organic constituents in 2,756 samples and soluble organic constituents in 330 samples from 2,080 public supply wells. Water quality differs among the aquifers...
Stability of nitrate-ion concentrations in simulated deposition samples used for quality-assurance activities by the U.S. Geological Survey
T. C. Willoughby, R.B. See, L.J. Schroder
1989, Water-Resources Investigations Report 89-4042
Three experiments were conducted to determine the stability of nitrate-ion concentrations in simulated deposition samples. In the four experiment-A solutions, nitric acid provided nitrate-ion concentrations ranging from 0.6 to 10.0 mg/L and that had pH values ranging from 3.8 to 5.0. In the five experiment-B solutions, sodium nitrate provided nitrate-ion...
Streamflow at selected gaging stations on the James River in North Dakota and South Dakota, 1953-82, with a section on climatology
Gregg J. Wiche, Rick D. Benson, Douglas G. Emerson
1989, Water-Resources Investigations Report 89-4039
Historic stream flow data were compiled and record extension techniques were used, when necessary, to develop a monthly stream flow record for 1953-82 at streamflow-gaging stations on the James River in North Dakota and South Dakota. The record extension techniques included both Maintenance of Variance Extension Type 1 and Ordinary...
Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 3
V.E. Stricklin
1989, Water-Resources Investigations Report 88-4120
This report delineates and describes the geohydrology and the susceptibility to contamination of the major aquifers in Area 3--Cullman, Fayette, Lamar, Marion, Walker, and Winston Counties , Alabama. The major aquifers in the study area are the Tuscaloosa, Pottsville, and Bangor aquifers. The Pottsville aquifer is the most extensively used...
Hydraulic and salinity characteristics of the tidal reach of the Peace River, southwestern Florida
Y.E. Stoker, S.E. Henderson, B. F. McPherson
1989, Water-Resources Investigations Report 88-4162
The tidal reach of the Peace River in southwestern Florida extends about 26 miles upstream from Charlotte Harbor and is characterized by flow-direction reversals, low velocities, and salinity gradients that vary with freshwater inflow, tides, and wind. Flow reversals generally occur on each tide throughout most of the tidal reach,...
Suspended-sediment data in the upper Rio Grande De Loiza basin, Puerto Rico
Senen Guzman-Rios
1989, Open-File Report 88-324
Fluvial sediment, a widely recognized pollutant of surface water , is reducing the efficiency and useful life of almost all reservoirs in Puerto Rico. Sediment transported from the upper basin of the Rio Grande de Loiza is eventually deposited in the bottom of Lago Loiza, a water reservoir. Suspended sediment...