Geological and geophysical study of the preglacial Teays Valley in west-central Ohio
Stanley Eugene Norris, H. Cecil Spicer
1958, Water Supply Paper 1460-E
No abstract available....
References on laboratory and equipment methods in ground water hydrology
1958, Report
No abstract available....
Metamorphosed middle Paleozoic fossils from Central Massachusetts, eastern Vermont, and western New Hampshire
A. J. Boucot, G.J.F. Macdonald, C. Milton, James B. Thompson Jr.
1958, Geological Society of America Bulletin (69) 855-870
Study of thin and polished sections and spectrographic analyses indicate that the brachiopod most recently used to date the Bernardston Formation in Massachusetts probably came from Lower Devonian beds (chlorite zone) in Nova Scotia, and not from Bernardston, Massachusetts. Restudy of the faunule from the calcareous quartzite (garnet zone) of...
Military use of geologists in World War II
R. L. Nace
1958, Geological Society of America Bulletin (69) 615-616
No abstract available....
Stratigraphy of ocoee series, Great Smoky Mountains, Tennessee and North Carolina
P.B. King, J. B. Hadley, R. B. Neuman, W. Hamilton
1958, Geological Society of America Bulletin (69) 947-966
Much of the Great Smoky Mountains, which span the boundary between Tennessee and North Carolina, is formed of the Ocoee series, of later Precambrian age. This is a body of terrigenous clastic sedimentary rocks, which has minor intercalations of limestone and dolomite but no volcanic components or known fossils. The...
Photogeologic map of the Mount Ellen-4 Quadrangle, Wayne County, Utah
W. R. Hemphill
1958, Trace Elements Memorandum 1079
No abstract available...
Photogeologic map of the east half of Cahone Quadrangle, Montezuma and Dolores counties, Colorado
R.J. Hackman
1958, Trace Elements Memorandum 1071
No abstract available...
The isolation and identification of Trypanosoma cruzi from raccoons in Maryland
B. C. Walton, P. M. Bauman, L. S. Diamond, Carlton M. Herman
1958, American Journal of Tropical Medicine and Hygiene (7) 603-610
Five raccoons trapped at Patuxent Research Refuge, Laurel, Maryland, were found to have trypanosomes in the blood which were morphologically indistinguishable from Trypanosoma cruzi on stained smears. The organism grew well in culture. It developed and reproduced in Triatoma protracta, T. infestans, T. phyllosoma, and Rhodnius prolixus. Experimental infections were produced in raccoons, opossums,...
Preliminary geologic map of the Elk Ridge 4 SW Quadrangle, San Juan County, Utah
Richard Q. Lewis Sr., Russell H. Campbell
1958, Trace Elements Memorandum 1094
No abstract available...
Preliminary geologic map of the Elk Ridge 1 NW Quadrangle, San Juan Quadrangle, Utah
Richard Q. Lewis Sr., Russell H. Campbell
1958, Trace Elements Memorandum 1095
No abstract available...
Distribution of populations and hunting kill of the canvasback
R. E. Stewart, A. D. Geis, C.D. Evans
1958, Journal of Wildlife Management (22) 333-370
No abstract available. ...
Low-flow characteristics of Iowa streams
Harlan H. Schwob
1958, Bulletin 9
Study of the occurrence of low flow on interior Iowa streams and the Big Sioux River....
Studies on digenetic trematodes of the genera Gymnophallus and Parvatrema
H. W. Stunkard, Joseph R. Uzmann
1958, Biological Bulletin (115) 276-302
No abstract available....
Fur catch in the United States, 1957
U.S. Branch of Wildlife Research
1958, Wildlife Leaflet 398
No abstract available....
The solusphere - its inferences and study
F. H. Rainwater, W. F. White
1958, Geochimica et Cosmochimica Acta (14) 244-249
Water is a fundamental geologic agent active in rock decomposition, erosion, and synthesis. Solutes in water are of particular interest to geochemists as sources of raw material for synthesis or as products of decomposition. When geochemical studies move from the laboratory into natural environment many variables relating to solute hydrology...
Geology of Kapingamarangi Atoll, Caroline Islands
Edwin D. McKee
1958, GSA Bulletin (69) 241-278
Kapingamarangi Atoll of the Caroline Islands consists of a peripheral reef, 1000-4000 feet across, surrounding a nearly circular lagoon which is 5 by 6 nautical miles in area and about 240 feet at maximum depth. Thirty-three islands, most of which are less than half a mile in length, are scattered...
Flowtill in Southeastern Massachusetts
J. H. Hartshorn
1958, GSA Bulletin (69) 477-482
No abstract available....
Geology of the north half of the Mt. Abbot quadrangle, Sierra Nevada, California
D. G. Sherlock, Warren Hamilton
1958, GSA Bulletin (69) 1245-1268
The north half of the 15-minute Mt. Abbot quadrangle lies across the crest of the Sierra Nevada. The Cretaceous granitic rocks that underlie most of the area form eight large discordant plutons that range from quartz diorite to alaskite; the largest pluton is coarse prophyritic quartz monzonite. Pre-batholithic metasedimentary and...
Recent underwater surveys using low-frequency sound to locate shallow bedrock
W. O. Smith
1958, GSA Bulletin (69) 69-98
Underwater investigations at Lake Mead, Chicago, Passamaquoddy Bay, and on Long Island established the characteristics of sound waves that can be used in shallow geophysical exploration by the sonar method.At Lake Mead the sediments were for the most part clay of high water content which was easily penetrated by low-power...
The relation of phosphorites to ground water in Beaufort County, North Carolina
P.M. Brown
1958, Economic Geology (53) 85-101
Recent ground-water studies undertaken by the U.S. Geological Survey in cooperation with the North Carolina Division of Mineral Resources have delineated phosphorite deposits, tentatively regarded as being of middle Miocene age, in Beaufort County. These deposits lie unconforma-bly on limestone of Eocene age and are unconformably overlain by late Miocene...
Minerals of the cassiterite-bearing veins at Irish Creek, Virginia, and their paragenetic relations
Jewell J. Glass, A. H. Koschmann, John Stewart Vhay
1958, Economic Geology (53) 65-84
Major rock types of the Irish Creek district are gneisses and schists, intruded by granodiorite. All these rocks are believed to be Precambrian. The ore deposits are fissure veins consisting largely of quartz veins bordered by greisen, and enriched by recurrent deposition. From field and microscopic evidence six stages of...
Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah
D. A. Phoenix
1958, GSA Bulletin (69) 403-418
In southwestern Colorado and southeastern Utah, strata of conglomeratic sandstone are localized at the base of the Brushy Basin Member of the Morrison Formation of Jurassic age. These discrete lithologic units contain sedimentary structures oriented in a prevailing easterly direction. They are believed to cover about one-third of the underlying...
Stratigraphy of Upper Pennsylvanian and lower Permian rocks in the Sand Canyon area, Otero County, New Mexico
George O. Bachman, Philip T. Hayes
1958, GSA Bulletin (69) 689-700
The Magdalena Group of Pennsylvanian age and, in ascending order, the lower tongue of the Abo Sandstone (herein named the Danley Ranch Tongue), the Hueco Limestone, the upper tongue of the Abo Sandstone (herein named the Lee Ranch Tongue), and the Yeso Formation of Permian age are well displayed in...
Contact metamorphism adjacent to a teschenite intrusion
Howard G. Wilshire
1958, Journal of the Geological Society of Australia (6) 11-20
Shale adjacent to the upper contact of an annular teschenite intrusion was converted to andalusite hornfels in an aureole 2–4 feet wide. At some points along the contact there is no evidence of anhydrous recrystallization. Rarely, magmatic reaction with small shale xenoliths resulted in formation of cordierite‐sillimanite (?) hornfelses, and...
Radiotracer experiments in the Mohawk River, New York, to study sewage path and dilution
Eugene S. Simpson, W. Arthur Beetem, F. H. Ruggles
1958, Eos, Transactions, American Geophysical Union (39) 427-433
Sewage from the Knolls Atomic Power Laboratory near Schenectady, N. Y., was dosed with 4.53 curies of P prior to discharge into the Mohawk River. Its pattern of diffusion was measured in the river with immersible GM‐tubes and by sampling. The initial path of sewage was strongly influenced by differences...