Mineral resources of the South Reveille Wilderness Study Area, Nye County, Nevada
M. F. Diggles, J. A. Saunders, D. A. Ponce, E.A. Rochette, J.T. Neubert
1986, Bulletin 1731-C
Bibliography on ground water in glacial-aquifer systems in the Northeastern United States
Denise A. Wiltshire, Forest P. Lyford, A.J. Cohen
1986, Circular 972
The U.S. Geological Survey established the Regional Aquifer-System Analysis (RASA) program to evaluate major interconnected aquifers or groups of aquifers that share similar characteristics within a region. One of the objectives of the Northeastern Glacial RASA is to provide information on the occurrence and quality of ground water in glacial...
Fluorometric procedures for dye tracing
James F. Wilson, Ernest D. Cobb, F. A. Kilpatrick
1986, Techniques of Water-Resources Investigations 03-A12
This manual describes the current fluorometric procedures used by the U.S. Geological Survey in dye tracer studies such as time of travel, dispersion, reaeration, and dilution-type discharge measurements. The advantages of dye tracing are (1) low detection and measurement limits and (2) simplicity and accuracy in measuring dye tracer concentrations using fluorometric techniques. The manual contains necessary...
Relationship of nonpoint-source discharges, streamflow, and water quality in the Galena River basin, Wisconsin
S. J. Field
1986, Water-Resources Investigations Report 85-4214
Four small tributaries of the Galena River Madden Branch tributary, Pats Creek, Apple River, and Madden Branch that drain nonpoint agricultural sources and that receive no significant point-source discharges were monitored from October 1980 through September 1982 to determine water quality. Streamflow in the tributaries during the 1981 water year was...
Benthic invertebrate population characteristics as affected by water quality in coal-bearing regions of Tennessee
A.D. Bradfield
1986, Water-Resources Investigations Report 85-4227
Benthic invertebrate and water quality data collected during previous U.S. Geological Survey studies to provide background hydrologic information on streams draining Tennessee coal reserves, were evaluated to identify possible relations between stream biota and water quality. Linear regressions produced low correlation coefficients relating the number of taxa/sample, total number of...
Thermal considerations and the Cajon Pass borehole
A.H. Lachenbruch, J.H. Sass, T. H. Moses Jr., S.P. Galanis Jr.
1986, Open-File Report 86-469
Archaeology and public perception of a trans-scientific problem; disposal of toxic wastes in the unsaturated zone
Isaac Judah Winograd
1986, Circular 990
Predicting the effects of toxic-waste disposal on the environment over periods of millenia to hundreds of millenia is a transscientific problem; that is, one not fully addressed by quantitative scientific and engineering endeavors. Archaeology is a pertinent adjunct to such predictions in several ways. First, and foremost, archaeological records demonstrate...
Hydrogeologic sections of the Edwards Aquifer and its confining units in the San Antonio area, Texas
Ted A. Small
1986, Water-Resources Investigations Report 85-4259
Twenty-seven geohydrology sections illustrate structural and stratigraphic relationships within the 180-mi-long Edwards aquifer. These sections were used to interpret the location of barriers within the Edwards aquifer. The sections are oriented generally south-southeast, which is approximately normal to both the east-northeast trending Edwards aquifer and the strike of the major...
Principles of logic and the use of digital geographic information systems
Charles Joseph Robinove
1986, Circular 977
Digital geographic information systems allow many different types of data to be spatially and statistically analyzed. Logical operations can be performed on individual or multiple data planes by algorithms that can be implemented in computer systems. Users and creators of the systems should fully understand these operations. This paper describes...
Hydrogeologic factors in the selection of shallow land burial sites for the disposal of low-level radioactive waste
John N. Fischer
1986, Circular 973
In the United States, low-level radioactive waste is disposed of by shallow land burial. Commercial low-level radioactive waste has been buried at six sites, and low-level radioactive waste generated by the Federal Government has been buried at nine major and several minor sites. Several existing low-level radioactive waste sites have...
Temperature, thermal-conductivity, and heat-flux data; Raft River area, Cassia County, Idaho (1974-1976)
T. C. Urban, W.H. Diment, Manuel Nathenson, E.P. Smith, J.P. Ziagos, M.H. Shaeffer
1986, Open-File Report 86-123
Ice in streams: Its formation and effects on flow
H.S. Santeford, G.R. Alger, J.A. Stark
1986, Water-Resources Investigations Report 86-4209
No abstract available. ...
Areal and temporal variations in the quality of surface water in hydrologic accounting unit 120301, Upper Trinity River basin, Texas
Frank C. Wells, Jack Rawson, Wanda J. Shelby
1986, Water-Resources Investigations Report 85-4318
Hydrologic Accounting Unit 120301 is located in north-central Texas and includes that part of the Trinity River basin upstream from the National Stream Quality Accounting Network station 08062700, Trinity River at Trinidad, Texas. Normal annual precipitation ranges from about 28 inches in the western part of the basin to almost...
The geology of Kentucky— A text to accompany the geologic map of Kentucky
Robert C. McDowell, editor(s)
1986, Professional Paper 1151-H
No abstract available....
Measurement of scour-depth near bridge piers
J. V. Skinner
1986, Water-Resources Investigations Report 85-4106
River-bed scour is a major source of damage to bridge piers and bridge abutments. When scour depth exceeds design limits, the supporting material around the footings is washed away and the structure becomes unstable. Equations for predicting scour-depth show a significant lack of agreement so portable equipment for measuring scour...
Quality-assurance results for field pH and specific-conductance measurements, and for laboratory analysis, National Atmospheric Deposition Program and National Trends Network; January 1980-September 1984
L.J. Schroder, M. H. Brooks, B.A. Malo, T. C. Willoughby
1986, Water-Resources Investigations Report 86-4139
Five intersite comparison studies for the field determination of pH and specific conductance, using simulated-precipitation samples, were conducted by the U.S.G.S. for the National Atmospheric Deposition Program and National Trends Network. These comparisons were performed to estimate the precision of pH and specific conductance determinations made by sampling-site operators. Simulated-precipitation...
Location of potential ground-water quality monitoring wells, Fort Pierce 1 degree x 2 degrees quadrangle, Florida
M.E. Thagard, P. R. Seaber
1986, Water-Resources Investigations Report 85-4133
No abstract available....
Effect of bank protection measures, Stehekin River, Chelan County, Washington
L. M. Nelson
1986, Water-Resources Investigations Report 85-4316
An investigation of the lower Stehekin River was conducted to study the effects on flood elevations and velocities from four bank protection and flood prevention measures that are being contemplated as a means of reducing erosional losses of river bank property. These measures are: bank armoring, armored revetment levees, spur...
Influence of size-fractioning techniques on concentrations of selected trace metals in bottom materials from two streams in northeastern Ohio
G. F. Koltun, Dennis R. Helsel
1986, Water-Resources Investigations Report 86-4114
Identical stream-bottom material samples, when fractioned to the same size by different techniques, may contain significantly different trace-metal concentrations. Precision of techniques also may differ, which could affect the ability to discriminate between size-fractioned bottom-material samples having different metal concentrations. Bottom-material samples fractioned to less than 0.020 millimeters by means...
Discharge and water quality of Horse Creek, southeastern Wyoming, May-November, 1985
J.F. Meyer, L.W. Lenfest Jr.
1986, Open-File Report 86-69
This report presents stream-discharge and water-quality data collected at five sites in the lower Horse Creek drainage of southeastern Wyoming, May through November, 1985. Data include stream-discharge measurements; field measurements of specific conductance, pH, and water temperature; and computer changes in stream discharge. Measured discharge in Horse Creek ranged from...
Catalog of South Dakota cores housed at the USGS Core Repository, Denver, Colorado
T.C. Michalski, D.L. Richards
1986, Open-File Report 86-89
Catalog of Utah cores housed at the USGS Core Repository, Denver, Colorado
T.C. Michalski, D.L. Richards
1986, Open-File Report 86-124
Simulation analysis of water-level changes in the Navajo sandstone due to changes in the altitude of Lake Powell near Wahweap Bay, Utah and Arizona
B. E. Thomas
1986, Water-Resources Investigations Report 85-4207
A two-dimensional, finite difference, digital computer model was used to simulate various concepts of groundwater flow near Wahweap Bay, Lake Powell. The filling of Lake Powell started in March 1963; and by 1983 the lake had risen almost 550 ft. This resulted in a maximum observed water level rise of...
Maps of debris-flow features evident after the storms of December 1955 and January 1982, Montara Mountain area, California
Water Resources Division, U.S. Geological Survey
1986, Open-File Report 86-363
No abstract available....
Catalog of Idaho and Nevada cores housed at the USGS Core Repository, Denver, Colorado
T.C. Michalski, D.L. Richards
1986, Open-File Report 86-355