Ground-water resources of the Pascagoula River basin, Mississippi and Alabama
Roy Newcome
1967, Water Supply Paper 1839-K
Abundant ground-water resources underlie the Pascagoula River basin. These resources have been developed intensively in only a few places--namely, Hattiesburg, Laurel, Meridian, and Pascagoula. Seepage from the ground water reservoirs sustains the base flows of the Leaf, Chickasawhay, Pascagoula, and Escatawpa Rivers and their tributaries. The fresh-water-bearing section is 300...
Delaware River basin - water data stations, 1967
D.W. Moody, F.L. Shaefer
1967, Open-File Report 67-160
This report presents information on station-type activities for acquiring surface-water, ground-water, and quality of water data in the Delaware River basin. The information was collected in 1966 through field offices of the Water Resources Division, U.S. Geological Survey as part of a pilot study for the Office of Water Data...
Preliminary report on Bureau of Mines Yellow Creek core hole No. 1, Rio Blanco County, Colorado
R. D. Carroll, D.L. Coffin, J. R. Ege, F.A. Welder
1967, Open-File Report 67-38
Analysis of geologic, hydrologic , and geophysical data obtained in and around Yellow Creek core hole No. 1, Rio Blanco County, Colorado, indicate a 1,615-foot section of oil shale was penetrated by the hole. Geophysical log data indicate the presence of 25 gallons per ton shale for a thickness of...
Complaints related to water wells after Salmon Event in Tatum salt dome area, Lamar County, Mississippi
R.E. Taylor
1967, Open-File Report 67-210
Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia
R. L. Wait, D. O. Gregg
1967, Open-File Report 67-267
Records of wells, test holes, springs, and surface-water stations in the Los Alamos area, New Mexico
E.C. John, Eugene Enyart, W.D. Purtymun
1967, Open-File Report 67-123
A reexamination of water yield in the Little Lost River basin, Idaho
H.A. Waite, S.O. Decker
1967, Open-File Report 67-268
An investigation of potential salt-water intrusion from inland waterways in the shallow alluvial and coastal deposits of Sunset and Bolsa Gaps, Orange County, California
J. R. Wall, J. A. Moreland, E. H. Cordes
1967, Open-File Report 67-269
Correlation and analysis of water-temperature data for Oregon streams
A.M. Moore
1967, Water Supply Paper 1819-K
Quality of surface waters for irrigation, Western states, 1963
S. K. Love
1967, Water Supply Paper 1952
The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data
Robert David Brown Jr., J. G. Vedder, R. E. Wallace, E. F. Roth, R. F. Yerkes, R. O. Castle, A. O. Waananen, R. W. Page, J. P. Eaton
1967, Professional Paper 579
No abstract available....
Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania
Grant Kimmel, G. R. Schiner
1967, Open-File Report 67-127
Memorandum on availability of water having less than 2,500 parts per million dissolved solids in alluvium of Rio Grande near El Paso, Texas
M. E. Davis
1967, Open-File Report 67-78
No abstract available....
Geology and water resources in the French Prairie area, northern Willamette Valley, Oregon
Don Price
1967, Water Supply Paper 1833
Geology and ground-water resources of Laramie County, Wyoming
Marlin E. Lowry, Marvin A. Crist, John R. Tilstra
1967, Water Supply Paper 1834
Laramie County, an area of 2,709 square miles, is in the southeast corner of Wyoming. Rocks exposed there range in age from Precambrian to Recent. The most extensive aquifers in the county are the White River Formation of Oligocene age, which is as much as 500 feet thick and consists...
Reconnaissance of the chemical quality of surface waters of the Neches River basin, Texas
Leon S. Hughes, Donald K. Leifeste
1967, Water Supply Paper 1839-A
The kinds and quantities of minerals dissolved in the surface water of the Neches River basin result from such environmental factors as geology, streamflow patterns and characteristics, and industrial influences. As a result of high rainfall in the basin, much of the readily soluble material has been leached from the...
General field and office procedures for indirect discharge measurements
M. A. Benson, Tate Dalrymple
1967, Techniques of Water-Resources Investigations 03-A1
The discharge of streams is usually measured by the current-meter method. During flood periods, however, it is frequently impossible or impractical to measure the discharges by this method when they occur. Consequently, many peak discharges must be determined after the passage of the flood by indirect methods, such as slope-area,...
Swatara Creek basin of southeastern Pennsylvania: An evaluation of its hydrologic system
Wilbur Tennant Stuart, William J. Schneider, James W. Crooks
1967, Water Supply Paper 1829
Local concentrations of population in the Swatara Creek basin of Pennsylvania find it necessary to store, transport, and treat water because local supplies are either deficient or have been contaminated by disposal of wastes in upstream areas. Water in the basin is available for the deficient areas and for dilution...
Chemical quality of surface water in the Allegheny River basin, Pennsylvania and New York
Edward F. McCarren
1967, Water Supply Paper 1835
The Allegheny River is the principal source of water to many industries and to communities in the upper Ohio River Valley. The river and its many tributaries pass through 19 counties in northwestern and western Pennsylvania. The population in these counties exceeds 3 million. A major user of the Allegheny...
Records of observation wells and water-level fluctuations in the Aberdeen-Springfield area, Bingham and Power Counties, Idaho, in 1966
H.E. Sisco, R.L. Whitehead
1967, Open-File Report 67-202
Water resources of the Marquette Iron Range area, Michigan
Sulo Werner Wiitala, Thomas Gwyn Newport, Earl L. Skinner
1967, Water Supply Paper 1842
Large quantities of water are needed in the beneficiation and pelletizing processes by which the ore mined from low-grade iron-formations is upgraded into an excellent raw material for the iron and steel industry. Extensive reserves of low-grade iron-formation available for development herald an intensification of the demands upon the area's...
Geologic reconnaissance in western Liberia
G. W. Leo, R.W. White
1967, Open-File Report 67-147
Irazu volcano, a large composite cone, consists of interbedded lava flows, lahars, and ash beds. This rock sequence, named the Irazu Group, has been divided into four formations; from the base: Reventado Formation, Sapper Formation, Birris Formation, and Cervantes Formation. Only the Reventado and Sapper Formations crop out in the...
Floods on Otter Creek in Linn County, Iowa
H.H. Schwob
1967, Open-File Report 67-195
No abstract available....
Records of wells on the Northern Neck Peninsula, Virginia (including well logs and chemical analyses of ground water)
Allen Sinnott
1967, Open-File Report 67-201
Water resources of lower Sycamore Creek, Maricopa County, Arizona
H. H. Schumann
1967, Open-File Report 67-194
