Geohydrology of the Meadowbrook artificial-recharge site at East Meadow, Nassau County, New York
D. A. Aronson, J. B. Lindner-Lunsford, B. G. Katz
1983, Water-Resources Investigations Report 82-4084
No abstract available....
Hydrology and subsidence potential of proposed coal-lease tracts in Delta County, Colorado
Tom Brooks
1983, Water-Resources Investigations Report 83-4069
Potential subsidence from underground coal mining and associated hydrologic impacts were investigated at two coal-lease tracts in Delta County, Colorado. Alteration of existing flow systems could affect water users in the surrounding area. The Mesaverde Formation transmits little ground water because of the neglibile transmissivity of the 1,300 feet of...
Water resources of Manatee County, Florida
David P. Brown
1983, Water-Resources Investigations Report 81-74
Rapid development of Manatee County in southwest Florida is creating water-resource problems. This report presents an evaluation of the water resources and potential effects of water-resource developments. Most streams in the county have small drainage basins and minimal flow. Streamflow is variable with the base flow occurring from November to...
Preliminary appraisal of the hydrology of the Red Oak area, Latimer County, Oklahoma
M.V. Marcher, D. L. Bergman, J.D. Stoner, S. P. Blumer
1983, Water-Resources Investigations Report 83-4166
Bed rock in the Red Oak area consists of shale, siltstone, and sandstone of the McAlester and Savanna Formations of Pennsylvanian age. Water in bedrock occurs in bedding planes, joints, and fractures and is confined. The potentiometric surface generally is less than 20 feet below the land surface. Wells yield...
Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma
M.V. Marcher
1983, Water-Resources Investigations Report 83-4013
Bed rock in the Rock Island area of northeastern Le Flore County in southeastern Oklahoma consists of shale, siltstone, and sandstone of the McAlester, Hartshorne, and Atoka Formations of Pennsylvanian age. The area is on the south flank of the Backbone anticline; the rocks dip to the south at 5o-45o....
Preliminary appraisal of the hydrology of the Stigler area, Haskell County, Oklahoma
M.V. Marcher, T.L. Huntzinger, J.D. Stoner, S. P. Blumer
1983, Water-Resources Investigations Report 82-4099
Bed rock in the Stigler area of southeastern Oklahoma consists principally of shale, siltstone, and sandstone of the McAlester, Savanna, and Boggy Formations of Pennsylvanian age. These rocks have been folded to form the Stigler syncline on the north and the Antioch anticline on the south. An area of several...
Evidence of floods on the Potomac River from anatomical abnormalities in the wood of flood-plain trees
Thomas M. Yanosky
1983, Professional Paper 1296
Ash trees along the Potomac River flood plain near Washington, D.C., were studied to determine changes in wood anatomy related to flood damage, and anomalous growth was compared to flood records for April 15 to August 31, 1930-79. Collectively, anatomical evidence was detected for 33 of the 34 growing-season floods...
Effects of the drought of 1980-81 on streamflow and on ground-water levels in Georgia
R.F. Carter
1983, Water-Resources Investigations Report 83-4158
The 1980-81 drought resulted in the lowest rates of streamflow since 1954 in most areas of Georgia, and the lowest since 1925 in some areas. Over most of the State, minimum average streamflows for periods of 1, 7, 30, 60, 90, and 183 consecutive days receded to low levels estimated...
Floods in Kansas City, Missouri and vicinity, August 12-13, 1982
L.D. Becker, T.W. Alexander, L.A. Waite
1983, Water-Resources Investigations Report 83-4141
On August 12-13, 1982, a nearly stationary weather front in the vicinity of Kansas City, MO, produced intense thunderstorms. Excessive rainfall (12.6 inches in Raytown, MO) caused flash flooding during the nighttime and early daylight hours. Four deaths and damages unofficially estimated in excess of $30 million, occurred in the...
Water quality of Lake Arlington on Village Creek, north-central Texas; 1973 to 1981
Freeman L. Andrews, Willard J. Gibbons
1983, Water-Resources Investigations Report 83-4196
Water in Lake Arlington on Village Creek in north-central Texas had volume-weighted average concentrations of less than 240 milligrams per liter of dissolved solids, less than 30 milligrams per liter of dissolved chloride, and less than 40 milligrams per liter of dissolved sulfate between January 29, 1973, and August 20,...
Regional hydrology of the Blanding-Durango area, southern Paradox basin, Utah and Colorado
M.S. Whitfield, William Thordarson, W. J. Oatfield, E. A. Zimmerman, B. F. Rueger
1983, Water-Resources Investigations Report 83-4218
No abstract available....
A preliminary assessment of the hydrologic characteristics of the James River in South Dakota
R.D. Benson
1983, Water-Resources Investigations Report 83-4077
The James River in South Dakota has very restricted channel capacities within the Lake Dakota Plain. Channel capacities in Brown County are as little as 200 cubic feet per second, and spring flooding can be expected on an average of every other year. The river has potential for extended periods...
Ground water in carbonate rocks and regolith in the Fairview area, Tennessee
C.R. Burchett, Ann Zurawski, A.K. Sparkes, E. F. Hollyday
1983, Water-Resources Investigations Report 83-4134
Fourteen test wells drilled in the Fairview area, Tennessee, produce from 3 to 100 gallons per minute and have an average yield of 32 gallons per minute, measured while blowing water from the wells with compressed air. In comparison, the average yield of supply wells reported by drillers is 13...
Streamflow losses along the Balcones Fault Zone, Nueces River basin, Texas
L. F. Land, C.W. Boning, Lynn Harmsen, R.D. Reeves
1983, Water-Resources Investigations Report 83-4168
An investigation was conducted to quantify and to determine distribution of streamflow losses and gains that occur during sustained flow conditions in the Balcones Fault Zone of the Nueces River basin. The streams studied include the West Nueces, Nueces, Dry Frio, Frio, and Sabinal Rivers, and Seco, Hondo, and Verde...
Subsurface storage of freshwater in south Florida: A prospectus
M. L. Merritt, F.W. Meyer, W. H. Sonntag, D. J. Fitzpatrick
1983, Water-Resources Investigations Report 83-4214
A method of increasing storage capacity for freshwater in south Florida is to use brackish artesian aquifers as reservoirs. In this way, water deficiencies occurring during the annual dry season can be offset by surplus water obtained during the wet season and injected underground. Most of south Florida is underlain...
Preliminary report of the geohydrology near Cypress Creek and Richton salt domes, Perry County, Mississippi
C.B. Bentley
1983, Water-Resources Investigations Report 83-4169
Time of travel and dispersion study in the Androscoggin River basin, Maine
G.W. Parker, G.S. Westerman, G.S. Hunt, G.L. Morrill
1983, Water-Resources Investigations Report 83-4232
In a series of dye tracer studies at discharge ranging from 45 to 212 cubic meters per second, time of travel and dispersion characteristics were determined at 12 sampling sites along 123 kilometers of the Androscoggin River (Rumford to Prejepscot Dam). Dye-cloud centroid traveltimes ranged from approximately 120 hours at...
Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York, part 1: Geohydrology, modeling strategy, and regional evaluation
T. E. Reilly, H. T. Buxton, O.L. Franke, R. L. Wait
1983, Water-Resources Investigations Report 82-4045
A computer simulation of Long Island 's regional groundwater system has been used to evaluate the effects that new-installed sewers will have on ground-water levels. Results indicate maximum water-table decliners of as much as up to 18 feet in central Nassau County and about 9 feet in Suffolk County. Total...
Water-quality assessment of Francis E. Walter Reservoir, Luzerne and Carbon counties, Pennsylvania
J. L. Barker
1983, Water-Resources Investigations Report 83-4032
Water-quality data, both past and present, show that the waters of the upper Lehigh River basin are somewhat acidic, but otherwise are generally of good quality. This report contains a summary of all known water-quality data collected by the U.S. Geological Survey and other agencies, as well as a synopsis...
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...
Availability and chemical quality of water from surficial aquifers in Southwest Minnesota
D. G. Adolphson
1983, Water-Resources Investigations Report 83-4030
The principal surficial aquifers in southwest Minnesota consist of outwash and alluvium material deposited in river valleys. The largest and most productive of these aquifers occupy the valleys of the Cottonwood, Des Moines, Redwood, and Rock Rivers and of tributaries to the Big Sioux River. Minor aquifers, adequate only for...
An assessment of steady-state propane-gas tracer method for reaeration coefficients — Cowaselon Creek, New York
N. Yotsukura, D.A. Stedfast, R. E. Draper, W.H. Brutsaert
1983, Water-Resources Investigations Report 83-4183
Three tests were conducted in a straight 5.2-km reach of the Cowaselon Creek, Canastota, New York, in order to assess feasibility of the steady-state propane-gas tracer method as a means of estimating in situ reaeration coefficients. It is concluded that the steady-state method, which combines as instantaneous injection of dye...
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...
Correlation chart for Precambrian rocks of the Eastern United States
Douglas W. Rankin, T. W. Stern, James McLelland, R. E. Zartman, A.L. Odom
1983, Professional Paper 1241-E
Core KM-3, a surface-to-bedrock record of late Cenozoic sedimentation in Searles Valley, California
George I. Smith, V.J. Barczak, G. F. Moulton, J. C. Liddicoat
1983, Professional Paper 1256