Hot brines and recent iron deposits in deeps of the Red Sea
A.R. Miller, C.D. Densmore, E.T. Degens, J.C. Hathaway, F.T. Manheim, P.F. McFarlin, R. Pocklington, A. Jokela
1965, Open-File Report 65-180
Sedimentary iron and heavy-metal deposits of undetermined size have been found in the middle of the Red Sea some 2000 meters below the surface of the sea. This discovery has been made from the Research Vessel Atlantis II, which is still at sea engaged in a series of oceanographic investigations which...
Waterpower resources in Nehalem River basin, Oregon
Loyd L. Young, Jesse Lane Colbert, David L. Gaskill, Arthur M. Piper
1965, Water Supply Paper 1610-C
No abstract available....
Ground-water data of selected test holes and wells along the Arkansas River in Sequoyah County, Oklahoma
H.H. Tanaka, D.L. Hart Jr., R.K. Knott
1965, Open-File Report 65-157
The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig....
Density comparison method for the measurement of isotopic variations in prepared waters
Joseph Howard McCarthy Jr., Thomas Seward Lovering, Herbert Williams Lakin
1965, Open-File Report 65-103
The falling-drop method of density determination has been modified so that the densities of a standard and a sample water are compared simultaneously. A constant temperature bath that does not vary more than 0.0001°C and an accurate double micropipet are described. The method has sufficient sensitivity and precision to distinguish...
An appraisal of the ground-water resources of the lower Susquehanna River basin (An interim report)
Paul R. Seaber, Este F. Hollyday
1965, Open-File Report 65-146
This report describes the availability, quantity, quality, variability, and cost of development of the ground-water resources in the lower Susquehanna River basin. The report has been prepared for and under specifications established by the Corps of Engineers, U. S. Army, and the Public Health Service, Department of Health, Education, and...
Ground-water data of selected test holes and wells along the Verdigris River in Wagoner and Rogers Counties, Oklahoma
H.H. Tanaka, D.L. Hart Jr., R.K. Knott
1965, Open-File Report 65-156
The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig....
Relation of electrochemical potentials and iron content to ground-water flow patterns
William Back, Ivan Barnes
1965, Professional Paper 498-C
This study was undertaken to develop means of measuring oxidation potentials in aquifer systems and to use the measured values in interpreting the behavior of iron in ground water. Anne Arundel County, Md., was selected as the area of study because of the wide range of concentration of iron-nearly zero...
Variations in chemical character of water in the Englishtown Formation, New Jersey
Paul R. Seaber
1965, Professional Paper 498-B
This investigation describes the variations in the chemical character of the water in the Englishtown Formation of Late Cretaceous age in the Atlantic Coastal Plain of New Jersey, and demonstrates the application of the concept of hydrochemical mapping to the study and evaluation of water-bearing materials. The chemistry of ground water...
Resource understanding: a challenge to aerial methods
Stewart L. Udall
1965, Photogrammetric Engineering (31) 63-75
Aerial survey methods are speeding acquisition of survey data needed to provide and manage the nation's resources. These methods have been applied to topographic mapping for a number of years and the record clearly shows their advantages in terms of cost and speed in contrast to the ground methods that...
Infrared photography and imagery in water resources research
Charles J. Robinove
1965, Journal - American Water Works Association (57) 834-840
This article briefly describes the characteristics of infrared radiation and demonstrates how infrared photography and infrared imagery can be applied to water resources research, specifically to the identification and description of hydrologic features....
Water resources data for Indiana, 1965
Water Resources Division, U.S. Geological Survey
1965, Water Data Report IN-65-1
The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
Osmotic equilibrium and overthrust faulting
B.B. Hanshaw, E-An Zen
1965, Geological Society of America Bulletin (76) 1379-1385
The two principal suggested modes of facilitating overthrust faulting are (1) lubrication at the sole by evaporite beds or micaceous shales and (2) flotation due to anomalously high (> hydrostatic) pore-water pressures. Past rapid sedimentation and tectonic compression have been suggested as important causes of anomalously high water pressure (Hubbert...
Solute erosion and chloride balance in selected river basins of the western conterminous United States
A. S. Van Denburgh, J. H. Feth
1965, Water Resources Research (1) 537-541
The estimated average rates of annual solute erosion in 11 important western river basins range from 180 tons per square mile (Willamette basin) to 4.2 tons per square mile (Gila basin). An average rate of 58 tons per square mile is indicated for the entire 545,000‐square‐mile area drained by the...
United States earthquake research program, earthquake prediction: program issue paper
Water Resources Division, U.S. Geological Survey
1965, Report
No abstract available....
Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast
R. L. Wait, J.T. Callahan
1965, Groundwater (3) 3-17
Studies of the hydrogeologic environments and the dynamic and equilibrium relations of fresh and salt water in aquifers have been intensified at several places along the southeastern Atlantic Coast. Some salt-water problems involve the coastal water-table aquifer, and others involve parts of the artesian system.On the sandy coastal islands of...
Tracing the continuity of pleistocene aquifers in northern New Jersey by seismic methods
H.E. Gill, John Vecchioli, W.E. Bonini
1965, Groundwater (3) 33-35
Seismic refraction measurements were used to draw a new bedrock contour map in Morris County, New Jersey, where the major ground‐water supplies are found in Quaternary sand and gravel deposits filling pre‐Pleistocene channels. Aquifer performance tests aided in tracing the continuity of the Quaternary aquifers in these channels. In one case, the lack of continuity between two wells substantiated the seismic prediction that two separate channels were involved. The success of the seismic exploration emphasizes the value of...
Biota of a late glacial rocky mountain pond
E.G. Kauffman, David S. McCulloch
1965, GSA Bulletin (76) 1203-1232
The sediments of a late glacial sag pond in Huerfano Park, south-central Colorado, have yielded a varied biota consisting of vertebrates, terrestrial and fresh-water mollusks, sponges, and pollen. Wood from the sediments has a radiocarbon age of 9600 ± 200 years. The vertebrate fauna contains the tooth of a prairie...
Chemical quality of ground water in the Minneapolis-St. Paul area, Minnesota
W.B. Mann IV, M.S. McBride
1965, Report
No abstract available....
An automatic camera device for measuring waterfowl use
Lewis M. Cowardin, J.E. Ashe
1965, Journal of Wildlife Management (29) 636-640
A Yashica Sequelle camera was modified and equipped with a timing device so that it would take pictures automatically at 15-minute intervals. Several of these cameras were used to photograph randomly selected quadrats located in different marsh habitats. The number of birds photographed in the different areas was used as...
The drill‐stem test: The petroleum industry's deep‐well pumping test
J.D. Bredehoeft
1965, Groundwater (3) 31-36
Drill‐stem tests provide the petroleum industry information on three critical properties of subsurface formations —pressure head, permeability, and water chemistry –that the ground‐water hydrologist also seeks in making pumping tests of water wells. As it is increasingly necessary to study the hydraulic and geochemical properties of deep‐lying rocks in order to understand the behavior of ground water,...
Natural controls involved in shallow aquifer contamination
M. Deutsch
1965, Groundwater (3) 37-40
Shallow aquifers, commonly the most important sources of ground water, are also those most susceptible to contamination. The mode of entry of contaminants to shallow aquifers is (1) directly, via wells or secondary openings in consolidated rocks, (2) percolation through the zone of aeration, (3) induced infiltration through the zone of saturation, and (4) interaquifer leakage...
Low deuterium content of Lake Vanda, Antarctica
R.A. Ragotzkie, I. Friedman
1965, Science (148) 1226-1227
Lake Vanda in Victoria Land, Antarctica, is permanently ice-covered and permanently stratified, with warm, salty water near the bottom. Deuterium analyses of lake water from several levels indicate that the lake has a low deuterium content, and that it is stratified with respect to this isotope. This low deuterium content...
Radiocarbon determinations for estimating groundwater flow velocities in central Florida
B.B. Hanshaw, W. Back, M. Rubin
1965, Science (148) 494-495
Carbon-14 activity was determined from HCO3- in samples of groundwater obtained from the principal artesian aquifer in Florida. From these data the "age" of water obtained from a series of wells, each progressively farther down gradient on the piezometric surface, was established. Relative carbon-14 ages indicated a velocity...
Environmental framework of ground‐water contamination
H. E. LeGrand
1965, Groundwater (3) 11-15
Ramifications of contamination are increasingly involved in the majority of ground‐water problems. The volume of usable ground water is shrinking in many places because of dispersion of contaminated water. Consideration of ground‐water contamination as a multitude of independent problems, separately solvable as each problem arises, is outmoded; wise policies, relating water supply to contamination potential, are needed to alleviate and to forestall problems. Methodology of...
Water levels: Water levels and trends November 1964-January 1965 (Abstracted from U. 5. Geological Survey “Water Resources Review”)
G.N. Mesnier
1965, Groundwater (3) 45-45
No abstract available. ...