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Page 6061, results 151501 - 151525

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Generalized structure contour maps of the New Jersey coastal plain
Hoarce G. Richards, F. H. Olmsted, James L. Ruhle
1962, Geologic report (New Jersey) 4
Twelve generalized structural contour maps were prepared from a study of 169 well logs or sample logs of drill cuttings from the Coastal Plain of New Jersey, Delaware, and the E astern Shore of Maryland. The configuration of the tops of the nonmarine Cretaceous deposits (Patuxent , Patapsco, Raritan, and Magothy formations) and...
Physical properties of evaporite minerals
Eugene C. Robertson
1962, Trace Elements Investigations 821
The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick "rock salt" beds. These beds are...
Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah
L.C. Huff, F. G. Lesure
1962, Economic Geology (57) 226-237
Uranium-vanadium deposits in the Salt Wash Member of the Morrison Formation in Montezuma Canyon, San Juan County, Utah, exhibit zoning that is interpreted as a result of metal transport by diffusion. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The...
Diatremes and uranium deposits in the Hopi Buttes, Arizona
Eugene Merle Shoemaker, C. H. Roach, F. M. Byers Jr.
A.E.J. Engel, Harold L. James, B. F. Leonard, editor(s)
1962, Book chapter, Petrologic studies: A volume in honor of A. F. Buddington
The Hopi Buttes diatremes erupted in a shallow lake that was filled in as volcanic activity progressed in Pliocene time. At the end of the period of volcanism the landscape included low lava domes capping some of the diatremes, a few flows, and numerous craters of the maar type, surrounded...
Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid
D. B. Stewart, E. H. Roseboom Jr.
1962, Journal of Petrology (3) 280-315
Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible terminations have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different terminations may arise from variations in the relative amounts of additional components in magmas, or from...
Bedrock geology of the Thiel Mountains, Antarctica
A. B. Ford, J.M. Aaron
1962, Science (137) 751-752
Cordierite-bearing, hyper-sthene-quartz monzonite porphyry, the most widespread rock unit, is intruded by biotite granite and porphyritic biotite granite. Sedimentary and metasedimentary rocks, mainly quartzites and argillites, have been metamorphosed locally to hornfels and have been involved in high-angle faulting. Shear zones are common in the plutonic rocks....
The relative efficiency of nylon and cotton gill nets for taking lake trout in Lake Superior
Richard L. Pycha
1962, Journal of the Fisheries Research Board of Canada (19) 1085-1094
The change from cotton to nylon twine for gill nets in 1949–52 resulted in a sharp increase in the efficiency of the most important gear used for taking lake trout in Lake Superior, and, consequently, biased estimates of fishing intensity and abundance severely.From early May to the end of September...
Concentration method for the spectrochemical determination of seventeen minor elements in natural water
W. D. Silvey, R. Brennan
1962, Analytical Chemistry (34) 784-786
A method for the quantitative spectrochemical determination of microgram amounts of 17 minor elements in water is given. The chelating reagents 8-quinolinol, tannic acid, and thionalide are utilized to concentrate traces (1 to 500 μg.) of aluminum, cobalt, chromium, copper, iron, gallium, germanium, manganese, nickel, titanium, vanadium, bismuth, lead, molybdenum,...
Oxygen adsorption and the magnetic susceptibility of ice at low temperatures
F. E. Senftle, A. Thorpe
1962, Nature (194) 673-674
WHEN dealing with the magnetic susceptibility of tumour tissue1, we reported the magnetic susceptibility of ice at various temperatures from 273° K. down to 77° K. Since this publication, the authors have made many susceptibility measurements of ice, using the same equipment, and have obtained similar results, that is, a...
Behaviour of calcium carbonate in sea water
P. E. Cloud Jr.
1962, Geochimica et Cosmochimica Acta (26) 867-884
Anomalies in the behaviour of calcium carbonate in natural solutions diminish when considered in context. Best values found by traditional oceanographie methods for the apparent solubility product constant K'CaCO3 in sea water at atmospheric pressure are consistent mineralogically—at 36 parts per thousand salinity and T-25°C, K'aragonlte is...
Thorium and rare earths in the United States, exclusive of Alaska and Hawaii
J. C. Olson, J. W. Adams
1962, Mineral Investigations Resource Map 28
The accompanying map shows the location of the principal deposits of thorium and rare-earth minerals in the United States (excluding Alaska and Hawaii). Symbols of different shapes are used to depict deposits of different geologic types, and sizes of symbols denote the relative importance of the deposits. Because of scale...
The Vigil Network
Luna Bergere Leopold
1962, International Association of Scientific Hydrology - Bulletin (7) 5-9
Those of us who seek to explain the variations in hydrologic phenomena such as may be observed in the occurrence of floods or in changes in the shape of river channels are painfully aware of the lack of adequate data. Our existing data, collected mainly to serve immediate practical needs...
Rivers
Luna Bergere Leopold
1962, American Scientist (50) 511-537
Rivers are both the means and the routes by which the products of continental weathering are carried to the oceans of the world. Except in the most arid areas more water falls as precipitation than is lost by evaporation and transpiration from the land surface to the atmosphere. Thus there...
Distribution and detoxication of toxaphene in Clayton Lake, New Mexico
Burton J. Kallman, Oliver B. Cope, Richard J. Navarre
1962, Transactions of the American Fisheries Society (91) 14-22
The fate of toxaphene, applied in three treatments at a total calculated concentration of 0.05 p.p.m. to Clayton Lake, New Mexico, was followed over a 1.5-year period. A detailed description of the chromatographic method of analysis is given. Water concentrations of toxaphene were higher in leeshore samples than in windward...
Estimation of the brook and sea lamprey ammocoete populations of three streams
Bernard R. Smith, Alberton L. McLain
1962, Technical Report 4
Marking experiments on three streams in the Upper Peninsula of Michigan yielded quantitative estimates of populations of larval and transforming lampreys. The estimates not only gave an idea as to the numbers of ammocetes in the streams, but also confirmed the judgments of abundance based on earlier surveys with electric-shocking...
A photoelectric amplifier as a dye detector
Wesley J. Ebel
1962, Technical Report 4
A dye detector, based on a modified photoelectric amplifier, has been planned, built, and tested. It was designed to record automatically the time of arrival of fluorescein dye at predetermined points in a stream system. Laboratory tests and stream trials proved the instrument to be efficient. Small changes in color...
Water
Luna Bergere Leopold, Helene L. Baldwin
1962, Book
What do you use water for?If someone asked you this question you would probably think right away of water for drinking. Then you would think of water for bathing, brushing teeth, flushing the toilet. Your list would get longer as you thought of water for cooking, washing the dishes, running...