Hydrogeologic aspects of an analog model study of the Fairfield-New Baltimore area, Ohio
A. M. Spieker
1965, Open-File Report 65-152
Use of analog models in the analysis of flood runoff
John Shen
1965, Professional Paper 506-A
Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska
Edward G. Sable
1965, Open-File Report 65-141
This remote 700 square mile area in the Brooks Range is topographically rugged and geologically diverse; it contains a granitic pluton, low-grade metamorphic rocks, sedimentary rocks, and mafic igneous rocks, as well as glacial features.Rocks of sedimentary origin include from oldest to youngest:1.Neruokpuk Formation Middle and Upper Devonian(?), more than...
Water-resources reconnaissance of the Ouachita Mountains, Arkansas
Donald R. Albin
1965, Water Supply Paper 1809-J
The Jenkins-Whitesburg area includes approximately 250 square miles in Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one...
Water resources appraisal of the Anchorage area, Alaska
David A. Sommers, Melvin V. Marcher
1965, Open-File Report 65-151
At the present, water use in the Anchorage area amounts to about 21 mgd (million gallons per day); of this amount ground water accounts for about 10 mgd. By 1980, 60 mgd may be required to meet the demand.The greatest potential problem is overpumping the ground-water reservoir resulting in excessive...
Water-supply potential from an asphalt-lined catchment near Holualoa Kona, Hawaii
Salwyn S.W. Chinn
1965, Water Supply Paper 1809-P
The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one...
Geology and ground-water resources of Waushara County, Wisconsin
William Kelly Summers
1965, Water Supply Paper 1809-B
Abundant ground water for irrigation is available in the outwash deposits in western Waushara County, and many more large-capacity wells can be developed in these deposits without seriously lowering the water level. Pumping for irrigation temporarily lowers water levels in the vicinity of the wells but has not lowered regional...
An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico
Robert L. Cushman
1965, Water Supply Paper 1809-D
The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one...
Geology and ground water of the Tualatin Valley, Oregon
D. H. Hart, R. C. Newcomb
1965, Water Supply Paper 1697
The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly,...
Ground and surface water in the Mesabi and Vermilion Iron Range area, northeastern Minnesota
R. D. Cotter, H. L. Young, L. R. Petri, C. H. Prior
1965, Water Supply Paper 1759-A
Within the Mesabi-Vermilion Iron Range area, water of good quality is available from the Biwabik Iron-Formation, from stratified drift, and from lakes and streams. About 700 bgy (billion gallons a year) leaves the area as surface water, of which about one-third comes from ground water. Leached, oxidized, and fractured parts of...
Floods of March-April 1960 in Eastern Nebraska and adjacent states
H.D. Brice, R.E. West
1965, Water Supply Paper 1790-A
Snowmelt floods, record breaking on many streams and outstanding in terms of total area affected and runoff volumes generated, occurred in late March and early April 1960 on Missouri River tributaries in adjacent parts of six states. In order of area affected, the States are Nebraska, South Dakota, Iowa, Kansas,...
Geology of the Model quadrangle in Kentucky
William B. Rogers
1965, Geologic Quadrangle 409
Chemical and modal analyses of the pre-Upper Silurian quartz monzonite, and the post-Lower Devonian granodiorite, Attean quadrangle, Somerset County, Maine
Arden Leroy Albee
1965, Open-File Report 65-1
No abstract available....
Veins in the northern part of the Boulder batholith, Montana
D. M. Pinckney
1965, Open-File Report 65-123
About 20 miles north of Butte and extending nearly to Helena, is an area of 350 square miles containing hundreds of veins and altered zones. The bedrock of the area is 1) late Cretaceous volcanic rocks, forerunners of the Boulder batholith, 2) the Boulder batholith of late Cretaceous to early...
Freshwater inflow data for Corps of Engineers model study of Houston, Texas, ship channel
R. E. Smith, E.G. Kaminski
1965, Open-File Report 65-149
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...
Late quaternary geologic history of the lower Chippewa Valley, Wisconsin
George W. Andrews
1965, Bulletin of the Geological Society of America (76) 113-124
The lower Chippewa Valley in west-central Wisconsin extends 65 miles from the Cary terminal moraine in Chippewa County to the Mississippi River Valley. The Chippewa Valley and its tributaries were filled with a valley train of sand and gravel during the maximum stand of the Cary ice, and entrenchment of...
A simple animal support for convenient weighing
H.P. Pan, J.W. Caslick, D.T. Harke, D.G. Decker
1965, Journal of Wildlife Management (29) 890-891
A simple animal support constructed of web belts to hold skittish pigs for weighing was developed. The support is easily made, noninjurious to the pigs, and compact, facilitating rapid, accurate weighing. With minor modifications, the support can probably be used in weighing other animals....
Eclogites and eclogites: Their differences and similarities
R. G. Coleman, Donald E. Lee, L. B. Beatty, W. W. Brannock
1965, GSA Bulletin (76) 483-508
Eclogites are divisible into three groups based on mode of occurrence: Group A, inclusions in kimberlites, basalts, or layers in ultramafic rocks; Group B, bands or lenses within migmatite gneissic terrains; Group C, bands or lenses within alpine-type metamorphic rocks. The compositions range from olivine basalt for Group A to...
Investigation of initial Sr87/Sr86 ratios in the Sierra Nevada Plutonic Province
P.M. Hurley, P. C. Bateman, H.W. Fairbairn, W.H. Pinson
1965, GSA Bulletin (76) 165-174
One to three whole-rock samples from each of more than a dozen discrete plutonic intrusions in the east-central Sierra Nevada batholith have been analyzed for Sr87/Sr86 and Rb/Sr ratios to obtain information on initial Sr87 abundances.The initial Sr87/Sr86 ratios in the rock magmas forming this province appear to have been in the range...
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...
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...
Relation of carbon 14 concentrations to saline water contamination of coastal aquifers
B.B. Hanshaw, W. Back, Meyer Rubin, Robert L. Wait
1965, Water Resources Management (1) 109-114
Naturally occurring stable or radioactive isotopes may be used in some places to identify the origin of saline water that contaminates some coastal aquifers. In a recent study to determine the origin of saline water in the Ocala Limestone aquifer near Brunswick, Georgia, the following sources were analyzed for C14 and...
Mathematical models of catchment behavior
David R. Dawdy, Terence O’Donnell
1965, Journal of the Hydraulics Division (91) 123-137
After an examination of trends in the modeling of hydrologic systems, a review of some recent studies is given. The authors' preliminary studies on the feasibility and efficiency of the automatic evaluation of catchment model parameters by use of a digital computer are described and some results presented....
Ages of minerals from metamorphic and igneous rocks near Iron Mountain, Michigan
Lyman Thomas Aldrich, G.L. Davis, H. L. James
1965, Journal of Petrology (6) 445-472
More than 100 independent isotopic ages have been determined for minerals from an area in northern Michigan about 35 miles square. Granites, pegmatites, and metamorphosed sedimentary and volcanic rocks have yielded Rb-Sr ages for feldspar, muscovite, and biotite, K-Ar ages for hornblende, muscovite, biotite, and feldspar, and U-Pb and Th-Pb ages for zircon. It was anticipated that we would learn from the measurements both...