Aeromagnetic map of the Southbridge quadrangle, Worcester County, Massachusetts, and Windham and Tolland Counties, Connecticut
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 631
No abstract available....
Water resources data for Nevada, 1967
Water Resources Division, U.S. Geological Survey
1968, Water Data Report NV-67-1
The 1965 salt-water angling survey
David G. Deuel, John R. Clark
1968, Resource Publication 67
No abstract available....
Color photographs for water resources studies
William J. Schneider
1968, Photogrammetric Engineering (34) 257-262
Air-photo interpretation is very well suited to water resources studies where limited observations of hydrologic data must be extended to regional characteristics for large areas. It is also useful in monitoring the hydrologic regimen of an area to detect possible changes. Color aerial photography is generally superior to black-and-white photography...
Evaporation study at Warm Springs Reservoir, Oregon
D.D. Harris
1968, Report
The mass transfer-water budget method of computing reservoir evaporation was tested on Warm Springs Reservoir, whose contents and surface area change greatly from early spring to late summer. The mass-transfer coefficient computed for the reservoir is two to three times greater than expected and results in a computed evaporation much...
Ground-water resources of Monmouth County, New Jersey
Leo A. Jablonski
1968, New Jersey Division of Water Policy and Supply Special Report 23
Monmouth County includes an area of 538 square miles in east-central New Jersey. The climate is characterized by moderate temperature, moderate humidity, and moderate precipitation. The exposed rocks in the area are chiefly sands and clays, which range in age from Late Cretaceous through Recent. The formations strike northeast-southwest and dip...
Pedogenic formation of montmorillonite from a 2:1-2:2 intergrade clay mineral
Ronald L. Malcolm, W.D. Nettleton, R. J. McCracken
1968, Clays and Clay Minerals (16) 405-414
Montmorillonite was found to be the dominant clay mineral in surface horizons of certain soils of the North Carolina Coastal Plain whereas a 2:1-2:2 intergrade clay mineral was dominant in subjacent horizons. In all soils where this clay mineral sequence was found, the surface horizon was low in pH (below...
On the maintenance of anomalous fluid pressures: II. Source layer at depth
B.B. Hanshaw, J.D. Bredehoeft
1968, Geological Society of America Bulletin (79) 1107-1122
Physico-chemical mechanisms have been suggested to account for anomalous fluid pressures in the geologic environment which require a fluid source at depth. The persistence of anomalous pressure is a problem that involves nonsteady fluid flow. The hydrodynamics and particular boundary conditions control the time rate of pressure change and its...
O18/O16 ratios of coexisting minerals in glaucophane-bearing metamorphic rocks
Hugh P. Taylor Jr., Robert G. Coleman
1968, GSA Bulletin (79) 1727-1756
Oxygen isotope analyses have been obtained for coexisting minerals in several blue-schist-facies metamorphic rocks from California, Oregon, and New Caledonia. Detailed isotopic studies were made on a continuous exposure of schist in Ward Creek, California, previously described by Coleman and Lee (1962). The oxygen isotope fractionations among coexisting minerals in...
Composition of deeper subsurface waters along the Atlantic continental margin
Frank T. Manheim, M. K. Horn
1968, Southeastern Geology (9) 215-236
No abstract available....
Uranium disequilibrium in groundwater: An isotope dilution approach in hydrologic investigations
J.K. Osmond, H.S. Rydell, M. I. Kaufman
1968, Science (162) 997-999
The distribution and environmental disequilibrium patterns of naturally occurring uranium isotopes (U234 and U238) in waters of the Floridan aquifer suggest that variations in the ratios of isotopic activity and concentrations can be used quantitatively to evaluate mixing proportions of waters from differing sources. Uranium is probably unique...
Use of dye tracers to collect hydrologic data in Oregon
D.D. Harris, R.B. Sanderson
1968, Water Resources Bulletin (4) 51-68
Dye tracers have been used in Oregon in the Collection of hydrologic data on 2,350 miles of stream channels in the Long Tom, Umpqua, Willmette, and John Day River basins, and in the Carmen‐Smith power tunnel. These investigations demonstrated the usefulness, of dye tracers for determining: (1) estimates of traveltimes and travel...
Electric‐analog and digital‐computer model analysis of stream depletion by wells
C.T. Jenkins
1968, Groundwater (6) 27-34
Electric‐analog or digital‐computer models are used to compute the effect of ground‐water withdrawal or recharge on streamflow. The results can be generalized on a map showing lines of equal elapsed time. The lines indicate the time of recharging or discharging that is needed to affect the streamflow by a given fraction of the...
Field test results of the Model B panametrics radioisotope gage for monitoring suspended-sediment concentration in rivers and streams
J. V. Skinner
1968, Report
No abstract available...
Mortality among bobwhites confined to a heptachlor contaminated environment
J.F. Kreitzer, J. W. Spann
1968, Journal of Wildlife Management (32) 874-878
The lethal effects of heptachlor on bobwhites (Colinus virginianus) were studied at the Patuxent Wildlife Research Center during 1962 and 1963. A pair of adult birds was placed in each of 32 wire-covered field pens (20 x 50 x 61/2 ft) in May, 1962, and in 36 additional pens in...
Effect of predator reduction on waterfowl nesting success
D. S. Balser, Herbert H. Dill, H.K. Nelson
1968, Journal of Wildlife Management (32) 669-682
A 6-year study to determine the effect of nest-predator removal on waterfowl nesting success was conducted at the Agassiz National Wildlife Refuge in northwestern Minnesota from 1959 through 1964. Predators were removed from the west side of the Refuge while the east side served as a control area. At the...
Hydrogen and oxygen isotope fractionation between ice and water
James R. O’Neil
1968, Journal of Physical Chemistry (72) 3683-3684
No abstract available. ...
An aquifer test used to investigate a quality of water anomaly
Donald G. Jorgensen
1968, Groundwater (6) 18-20
An aquifer test and analyses of water samples, showed that the anomalous water quality of a municipal well was caused by leakage from a nearby abandoned well tapping another aquifer. ...
Silurian-devonian reef complex near Nowshera, West Pakistan
Karl W. Stauffer
1968, GSA Bulletin (79) 1331-1350
The first Paleozoic reef belt on the Indo-Pakistan subcontinent has recently been recognized near the town of Nowshera (lat 34°00′ N., long 72°00′ E.) in northern West Pakistan. It consists of nine separate hills aligned in a 15-mile-long, east-west band rising out of the Peshawar alluvial plain. Each hill is...
A fossil assemblage from the wicomico formation in Berkeley County, South Carolina
D.J. Colquhoun, Stephen M. Herrick, H.G. Richards
1968, Geological Society of America Bulletin (79) 1211-1220
Both megafossils and fossil Foraminifera have been obtained from unconsolidated sediments of the Wicomico Formation, which underlies the Penholoway terrace, a coastal feature that formed when the shoreline of the Atlantic Ocean stood about 70 feet higher than at present. Some of the fossils are Tertiary species and are assumed to have been derived from rocks...
Ground-water flow related to streamflow and water quality
Wayne A. Van Voast, R.P. Novitzki
1968, Water Resources Research (4) 769-775
A ground-water flow system in southwestern Minnesota illustrates water movement between geologic units and between the land surface and the subsurface. The flow patterns indicate numerous zones of ground-water recharge and discharge controlled by topography, varying thicknesses of geologic units, variation in permeabilities, and the configuration of the basement rock...
The non-colloidal origin of 'colloform' textures in sphalerite ores
E. Roedder
1968, Economic Geology (63) 451-471
"Colloform" ores have generally been considered to have been deposited as colloidal sulfide gels, and even transported as colloidal "sols." However, studies of doubly polished plates of "colloform" sphalerite-wurtzite assemblages from various deposits reveal crystal growth features that cannot have been formed by crystallization from gels, and indicate that most, and perhaps all, grew directly as minute...
Temperature, salinity, and origin of the ore-forming fluids at Pine Point, Northwest Territories, Canada, from fluid inclusion studies
E. Roedder
1968, Economic Geology (63) 439-450
Although the Pine Point ore is relatively poor in useable fluid inclusions, some sphalerite crystals from replacements, vugs, and from " colloform" crusts were found to contain primary or pseudosecondary liquid-gas inclusions adequate for study. Most (132 of 133) of these had low freezing temperatures, indicating exceedingly saline brines. The 112 inclusions suitable for filling-temperature determination homogenized at +51° to...
Analog simulation of ground-water development of the Saginaw Formation, Lansing metropolitan area, Michigan
K.E. Vanlier, M.L. Wheeler
1968, Report
This report was prepared as a part of the study of the water resources of Clinton, Eaton and Ingham Counties being made for the Tri-County Planning Commission by the Water Resources Division of the U. S. Geological Survey. The report describes one phase of the investigation, that is, the projections...
An evaluation of some geophysical methods for water exploration in the Piedmont Area by T. J. Joiner, J. C. Warman, and W. L. Scarbrough January‐February, 1968
Adel A. R. Zohdy
1968, Groundwater (6) 38-39
No abstract available. ...