Geophysical maps of Salt Lake Valley, Utah
Water Resources Division, U.S. Geological Survey
1954, Open-File Report 54-95
No abstract available....
Graphs showing percentage composition of sediments from water-bearing formations in southern Maryland, and maps showing the altitude of the base of sediments of Miocene age, and hardness of water sediments of Cretaceous age, in the same area
E. G. Otton
1954, Open-File Report 54-224
Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico
Donald Carl Laub
1954, Open-File Report 54-164
Sedimentary copper-uranium deposits lie along the eastern flank of the Sangre de Cristo Range in the Coyote mining district, Mora County, New ilexico. The oldest rocks in the district are pre-Cambrian granites, pegmatites and metasediments. These are unconformably overlain by marine limestones and shales of Pennsylvanian age and fluviatile sediments...
The quality and character of Pacific Northwest waters
Herbert A. Swenson
1954, Report
This paper is a general discussion of the quality and chemical character of surface and ground waters in the Pacific Northwest as shown by the available data. Previous quality of water studies reported in the literature are reviewed. The composition of natural waters is considered as to the source and...
Radioactive deposits in California
George W. Walker, Tom G. Lovering
1954, Trace Elements Investigations 229
Reconnaissance examination by Government geologists of many areas, mine properties, and prospects in California during the period between 1948 and 1953 has confirmed the presence of radioactive materials in place at more than 40 localities. Abnormal radioactivity at these localities is due to concentrations of primary and secondary uranium minerals,...
Caribbean land and sea through the ages
Wendell Phillips Woodring
1954, Geological Society of America Bulletin (65) 719-732
The oldest part of the Caribbean region proper is in northern Central America, where Permian (?) and Lower Permian marine deposits rest on metamorphic rocks of unknown, possibly middle Paleozoic, age. According to present dating, geosynclinal deposition spread eastward in Late Jurassic time to include Cuba, farther eastward and southward...
Some notes on the relation of ground‐water levels to pond levels in limestone sinks of southwestern Georgia
E. L. Hendricks
1954, Eos, Transactions, American Geophysical Union (35) 796-804
Records of water levels in limesink ponds in southwestern Georgia and of water‐table levels in the vicinity of these ponds are used to demonstrate: (1) some ponds with highly impermeable beds are virtually unaffected by water‐table levels, except when water‐table levels are above the rim of the impervious materials; (2) interchange of water between pond and water table occurs when beds are relatively permeable. Three phases in the relation between pond level and water‐table level are recognized: (1) water‐table level higher than pond level causing ground‐water flow into the pond; (2) ground‐water level below pond level but in direct contact...
Copper cities copper deposit, Globe-Miami district, Arizona
N. P. Peterson
1954, Economic Geology (49) 362-377
The Copper Cities copper deposit in the Globe-Miami district, Arizona, is now in process of development. It is of the "porphyry" type and occurs in a body of quartz monzonite that has been intruded by smaller masses of granite porphyry. The hypogene sulfides are pyrite, chalcopyrite, and a very little molybdenite. Pyritic mineralization extends over a large area...
Uranium in natural waters
Philip Forsyth Fix
1954, Trace Elements Memorandum 783
No abstract available....
Sedimentary facies of iron-formation
H. L. James
1954, Economic Geology (49) 235-293
The sedimentary iron-formations of Precambrian age in the Lake Superior region can be divided on the basis of the dominant original iron mineral into four principal facies: sulfide, carbonate, oxide, and silicate. As chemical sediments, these rocks reflect certain aspects of the chemistry of the depositional environments. The major control, at least for the sulfide,...
The chemical quality of surface waters in Devils Lake basin, North Dakota
H. A. Swenson, B. R. Colby
1954, Science (119) 614-614
No abstract available....
Chemical and physical characteristics of Delaware River water from Trenton, N. J., to Marcus Hook, Pa., 1949-52
C.N. Durfor, Walter B. Keighton
1954, Science (119) 613-614
No abstract available....
Ground-water field trip, Tucson to Nogales, Arizona
D.R. Coates, L.C. Halpenny
1954, Open-File Report 54-52
A field excursion following the route described herein was conducted as a part of the curriculum of the 6th Ground Water Short Course, which was held by the Geological Survey at the University of Arizona in April 1954. The route log and descriptive text were designed to provide a general...
Water resources of the Louisville area, Kentucky and Indiana
M. I. Rorabaugh, F. F. Schrader, L.B. Laird
1954, Science (119) 477-477
No abstract available....
Ground water in the High Plains of west-central United States
S. W. Lohman
1954, Science (119) 446-446
No abstract available....
Symposium on land erosion: Introduction
H.V. Peterson
1954, Eos, Transactions, American Geophysical Union (35) 243-244
One of the very obvious geologic phenomena that is continuously in operation throughout the Earth's land surface is erosion, the process of wearing away the soil or the surface mantle. The falling of rain drops on an unprotected slope, the flow of water across land or in a channel, the borings of a rodent, the...
Marsh and aquatic weed problems in wildlife habitat
A. C. Martin
1954, Weeds (3) 139-142
To most people, the word weeds signifies pest plants of the farm, roadside, or other upland areas. However, weeds also occur on, under, or near water. Fifteen million dollars have been spent on a single aquatic nuisance in the South—the prolific water-hyacinth which clogs navigable streams and lakes with its growth....
Ground water in the Navajo country
J. W. Harshbarger
1954, Science (119) 421-421
No abstract available....
Geology and ground water resources of the Matanuska Valley agricultural area, Alaska
F.W. Trainer
1954, Science (119) 356-356
No abstract available....
Developed and potential water power of the United States and other countries of the world
B. E. Jones, L.L. Young
1954, Science (119) 328-329
No abstract available....
The copper and uranium deposits of the Coyote district, Mora County, New Mexico
C.M. Tschanz, D.C. Laub, G.W. Fuller
1954, Trace Elements Investigations 356
The copper and uranium-vanadium deposits of the Coyote district, Mora County, N. Mec, are confined to the lower 2,000 feet of the Sangre de Gristo formation of Pennsylvanian and Permian age. A narrow belt of deposits in steeply dipping or overturned rocks extends for 7 miles along Coyote Creek south...
Uranium-bearing lignite in southwestern North Dakota
George W. Moore, Robert E. Melin, Roy C. Kepferle
1954, Trace Elements Investigations 463
Uranium-bearing lignite was mapped and sampled in the Bullion Butte, Sentinel Butte, HT Butte, and Chalky Buttes areas in southwestern North Dakota. The uraniferous lignite occurs at several stratigraphic positions in the Sentinel Butte member of the Fort Union formation of Paleocene age. A total of 261 samples were collected...
Stratigraphy of parts of De Soto and Hardee Counties, Florida
Maximilian H. Bergendahl
1954, Trace Elements Investigations 458
The late Cenozoic stratigraphy of part of central Florida immediately south of the land-pebble phosphate district was studies in detail to determine the southern limit of the economically important Bone Valley formation and its relations with marine rocks of late Miocene and Pliocene age in south-central Florida. In addition a...
Pumpage and ground-water levels in Arizona in 1953
L. C. Halpenny
1954, Report
No abstract available....
Carnotite-bearing sandstone in Cedar Canyon, Slim Buttes, Harding County, South Dakota
James R. Gill, George W. Moore
1954, Trace Elements Investigations 411
Carnotite-bearing sandstone and clay have been found in the Chadron formation of the White River group of Oligocene age in the southern part of the Slim Buttes area, Harding County, S. Dak. Locally the mineralized sandstone contains as much as 0.23 percent uranium. The uranium and vanadium ions are believed...