Ground-water data for Michigan 1982
G.C. Huffman
1983, Open-File Report 83-753
Water levels, locations, depths, and aquifers tapped are given for 117 observation wells. Tabulated data include extremes of water levels for 1982 and for the period of record, pumpage of most major ground-water users in the State, and quality data on selected wells. The largest reported user of ground-water, the...
Instructions for using the U.S. Geological Survey data base of wells on Long Island, New York
George W. Hawkins, Gregory M. Terlecki
1983, Open-File Report 82-568
The population of central and eastern Long Island, New York depends on ground water for its supply of fresh water. Data on more than 7,500 wells on the island have been collected by various State and local agencies and compiled by the U.S. Geological Survey since 1906. During 1975-81, the...
Water resources data, Arizona, water year 1981
Water Resources Division, U.S. Geological Survey
1983, Water Data Report AZ-81-1
Water resources data for the 1981 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; measurements of ground-water levels; and quality of water from selected wells. Also included are discharge data for crest-stage partial-record stations...
Application of digital mapping technology to the display of hydrologic information; a proof-of-concept test in the Fox-Wolf River Basin, Wisconsin
G. K. Moore, L.G. Baten, G.J. Allord, C.J. Robinove
1983, Water-Resources Investigations Report 83-4142
The Fox-Wolf River basin in east-central Wisconsin was selected to test concepts for a water-resources information system using digital mapping technology. This basin of 16,800 sq km is typical of many areas in the country. Fifty digital data sets were included in the Fox-Wolf information system. Many data sets were...
Identification and classification of perennial streams of Arkansas
R. A. Hunrichs
1983, Water-Resources Investigations Report 83-4063
Perennial streams are identified in a map and classified according to the relative magnitude of their 7-day, 10-year low flows. Perennial streams are identified for the entire State of Arkansas with the exception of the Mississippi Alluvial Plain. Also presented are the 7-day, 10-year low flow values at continuous-record and...
Estimation of nonpoint sources of phosphorus for lakes in the Puget Sound region, Washington
Robert J. Gilliom
1983, Open-File Report 82-161
Control of eutrophication of lakes in watersheds undergoing development is facilitated by estimates of the amounts of phosphorus (P) that reach the lakes from areas under various types of land use. Using a mass-balance model, the writer calculated P loadings from present-day P concentrations measured in lake water and from...
Petroleum and mineral resources of Antarctica
Karel Kovar
John Charles Behrendt, editor(s)
1983, Circular 909
No known petroleum or mineral resources occur in Antarctica. The data on these subjects have been collected, mainly since the IGY (International Geophysical Year), 1957-58, as a part of other research carried out by geologists and geophysicists from a number of countries. Specific resource-related studies have not been made. Wright...
Assessment of gray whale feeding grounds and sea floor interaction in the northeastern Bering Sea
C.H. Nelson, K.R. Johnson, John H. Barber
1983, Open-File Report 83-727
A dense ampeliscid amphipod community in Chirikov Basin and around St. Lawrence Island in the northeastern Bering Sea has been outlined by summarizing biological studies, analyzing bioturbation in sediment samples, and examining sea floor photos and videotapes. The amphipod population is associated with a homogeneous, relict fine-grained sand body 0.10-1.5...
Scientific and technical, spatial, and bibliographic data bases and systems of the U.S. Geological Survey, 1983; including other Federal agencies
Water Resources Division, U.S. Geological Survey
1983, Circular 817
Water resources data, Florida, water year 1982; Volume 1B. Northeast Florida ground water
L.D. Fayard, D.M. Bonnet, R.G. Belles
1983, Water Data Report FL-82-1B
Water resources data for the 1982 water year for northeast Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; water-levels and water quality of wells; and discharge and water quality of springs. Additional water data were collected at various...
Automatic dilution gaging of rapidly varying flow
M.D. Duerk
1983, Water-Resources Investigations Report 83-4088
It is often difficult to obtain discharge ratings at urban gaging stations. This report presents the results of using an automated constant-rate dyedilution technique to measure discharge at two sites in Madison, Wisconsin. The sites selected have well-defined stage-discharge ratings, developed during previous hydrologic studies. One site has a 60-inch...
Water resources data, Missouri, water year 1982
L.A. Waite, D.O. Hatten, P. W. Cross
1983, Water Data Report MO-82-1
Water resources data for the 1982 water year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 112 gaging stations; stage and contents at 9 lakes and reservoirs; water quality at 30 gaging stations (including 1 lake) and...
Computation of continuous records of streamflow
E.J. Kennedy
1983, Techniques of Water-Resources Investigations 03-A13
Records of continuous streamflow, published in the U.S. Geological Survey annual Water Data Reports for the States and territories, are computed from field data, mainly discharge measurements and recorder charts or tapes. This manual describes the computation procedures used and some details of related field operations. It was compiled mostly...
Geochemical data for the Guadalupe Escarpment Wilderness Study Area, Eddy County, New Mexico
Thomas D. Light, J. A. Domenico
1983, Open-File Report 83-7
Analytical data, geographic coordinates, and sample locality map of geochemical samples from the Mount Henry Roadless Area, Lincoln County, Montana
David F. Siems, R. W. Leinz, R. E. Van Loenen, Gail Wadsworth, C. M. McDougal
1983, Open-File Report 83-88
An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America
John T. Turk
1983, Water Supply Paper 2249
The acidity of precipitation in the Northeastern United States and Southeastern Canada has increased in the past, probably as a result of anthropogenic emissions. The increase in New England and New York occurred primarily before the mid-1950's. Since the mid1960's, there has been no significant change in the acidity of...
Water resources data, Arkansas, water year 1982
T.E. Lamb, J.E. Porter, B.F. Lambert, J. Edds
1983, Water Data Report AR-82-1
No abstract available....
Seismicity map of the State of New Mexico
C. W. Stover, B.G. Reagor, S. T. Algermissen
1983, Miscellaneous Field Studies Map 1660
The data shown on this map and listed in table 1 are for earthquakes that were originally included in a study of seismic risk in the United States (Algermissen, 1969). This data file has been recompiled and updated through 1980. Some revisions of epicenters and intensities in the original file...
Hydrogeology of a landfill, Pinellas County, Florida
Mario Fernandez Jr.
1983, Water-Resources Investigations Report 82-30
The Pinellas County landfill site is on a flat, coastal area characterized by a high water table is subject to tidal flooding. Altitudes within the study area range from 8 to 12 feet above sea level. Three geohydrologic units underlie the landfill site: a surficial aquifer about 19 feet thick...
A preliminary appraisal of sediment sources and transport in Kings Bay and vicinity, Georgia and Florida
J. B. McConnell, D. B. Radtke, T.W. Hale, G. R. Buell
1983, Water-Resources Investigations Report 83-4060
Water-quality, bottom-material, suspended-sediment, and current-velocity data were collected during November 1981 in Kings Bay and vicinity to provide information on the sources and transport of estuarine sediments. Kings Bay and Cumberland Sound , the site of the Poseidon Submarine Base in southeast Georgia, are experiencing high rates of sediment deposition...
Precipitation-runoff modeling system; user's manual
G.H. Leavesley, R.W. Lichty, B.M. Troutman, L.G. Saindon
1983, Water-Resources Investigations Report 83-4238
The concepts, structure, theoretical development, and data requirements of the precipitation-runoff modeling system (PRMS) are described. The precipitation-runoff modeling system is a modular-design, deterministic, distributed-parameter modeling system developed to evaluate the impacts of various combinations of precipitation, climate, and land use on streamflow, sediment yields, and general basin hydrology. Basin...
Wyoming; basic data for thermal springs and wells as recorded in Geotherm
James D. Bliss
1983, Open-File Report 83-439
Water resources data for Oregon, water year 1982. Volume 2: Western Oregon
L.L. Hubbard, T.D. Parks, D.L. Weiss, L.E. Hubbard
1983, Water Data Report OR-82-2
No abstract available....
Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1982
Dale B. Peart, Nancy Thomas
1983, Water-Resources Investigations Report 83-4264
The U.S. Geological Survey maintains a quality-assurance program based on the analysis of reference samples for its two water-analysis laboratories located in Atlanta, Georgia, and Denver, Colorado. Reference samples containing inorganic constituents are prepared at the U.S. Geological Survey 's Ocala , Florida, office and disguised as routine samples, and...
Methods for estimating peak discharge and flood boundaries of streams in Utah
B. E. Thomas, K.L. Lindskov
1983, Water-Resources Investigations Report 83-4129
Equations for estimating 2-, 5-, 10-, 25-, 50-, and 100-year peak discharges and flood depths at ungaged sites in Utah were developed using multiple-regression techniques. Ratios of 500- to 100-year values also were determined. The peak discharge equations are applicable to unregulated streams and the flood depth equations are applicable...