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Publication Extents

Not all publications have extents, not all extents are completely accurate
Chemical quality of ground water in Hawaii
Lindsay A. Swain
1973, Report R48
As the quantity of water needed in certain localities of Hawaii is rapidly approaching the quantity of usable water available, identification and protection of the quality of existing and potential water supplies are becoming ever more critical. Certain factors are already identifiable as problems affecting the quality of ground water...
Selected storm events in 5-minute increments from Missouri rainfall stations at Kansas City, St. Louis, Springfield, and Columbia, Mo., for the period 1892-1970
Leland D. Hauth
1973, Report
The purpose of this report is to present daily precipitation (see table A) and continual incremental (5-minute duration) rainfall data through entire storm periods (see table B) at four of the longest first-order National Weather Service station records in Missouri. These basic data can be used in model studies, unit-hydrographic...
Aeromagnetic discovery of a Baltimore Gneiss dome in the Piedmont of northwestern Delaware and southeastern Pennsylvania
Michael W. Higgins, George Wescott Fisher, Isidore Zietz
1973, Geology (1) 41-43
In the central Appalachian Piedmont the “basement complex” is an assemblage of 1,100- to 1,300-m.y.-old gneisses, migmatites, and amphibolites that crops out in “domes” mantled by younger meta-sedimentary rocks of the Glenarm Series. Aeromagnetic data and reconnaissance field work indicate that a previously unknown Baltimore Gneiss dome, here called the...
Chemical stability of preserved oligotrophic water samples
V. A. Adomaitis, J.A. Shoesmith, G.A. Swanson
1973, Proceedings of the North Dakota Academy of Science (26) 1-5
Tests were conducted to determine whether changes that may occur in the chemical characteristics of stored oligotrophic waters collected on 15 sites in northeastern Minnesota were affected by chloroforming. Chloroform was added on site to one of each pair of samples to stabilize the organic content of the water by...
Chemical composition of a saline lake on Enderbury Island, Phoenix Island Group, Pacific Ocean
Robert A. Gulbrandsen, David W. Brown
1973, Journal of Research of the U.S. Geological Survey (1) 105-111
Ion activity products for the dissolution of calcite, aragonite, gypsum, monetite, brushite, dolomite, magnesite, hydroxyapatite, and fluorapatite were calculated for a South Pacific guano island brine with an ionic strength of 6.4. Environmental conditions for the brine at the time of analysis and of sampling indicated saturation with respect to calcite, aragonite, gypsum, hydroxyapatite and...
Dolomitization model for Upper Cambrian and Lower Ordovician carbonate rocks in the eastern United States
Leonard D. Harris
1973, Journal of Research of the U.S. Geological Survey (1) 63-78
Existing models for dolomitization emphasize that penecontemporaneous dolomitization can occur in both subtidal and supratidal environments if the necessary chemical and physical factors favorable for the development of magnesium-rich hypersaline waters exist. Holocene shallow-water hypersaline environments that have the potential to produce dolomite without deposition of more soluble evaporite minerals are found in Shark Bay, Australia,...
Graptolites from the Martinsburg Formation, Lehigh Gap, Eastern Pennsylvania
Jack Burton Epstein, William B. N. Berry
1973, Journal of Research of the U.S. Geological Survey (1) 33-38
Graptolites collected from the uppermost part of the Martinsburg Formation (Pen Argyl Member) at and near the contact with the overlying Shawangunk Formation at Lehigh Gap, Pa., indicate that the uppermost Martinsburg is as young as Edenian to early Maysvillian (upper subzone [Climacograptus spiniferus subzone] of zone 13 | Orthograptus truncatus intermedius zone]). The Martinsburg gradationally...
Microprobe analysis of biotites - A method of correlating tuff beds in the Green River Formation, Colorado and Utah
George A. Desborough, Janet K. Pitman, John Roswell Donnell
1973, Journal of Research of the U.S. Geological Survey (1) 39-44
Quantitative electron microprobe analyses of biotite grains for iron, magnesium, and titanium from tuff beds in the lacustrineGreen River Formation (Eocene) of Colorado and Utah provide a tentative method of identification and a permissive stratigraphic correlation of tuffs. Tuff beds that have been identified and correlated by stratigraphic means were sampled at five...
Interpretation of depositional environment in the Plympton Formation (Permian), Southern Pequop Mountains, Nevada, from physical stratigraphy and a faunule
Ellis L. Yochelson, George D. Fraser
1973, Journal of Research of the U.S. Geological Survey (1) 19-33
Field mapping in the southern part of the Pequop Mountains has shown the presence of a major structural high which has profoundly affected the stratigraphy of Pennsylvanian and Lower Permian beds; lesser effects of this high persisted into the later Permian.  Within the Park City Group (Permian), the Plymton Formation, overlying the Kaibab Limestone,...
The fractionation of humic acids from natural water systems
R.L. Wershaw, D.J. Pinckney
1973, Journal of Research of the U.S. Geological Survey (1) 361-366
Humic acids, the most abundant organic components of natural water systems, are complex mixtures of molecular aggregates of different chemical and physical properties. The first step in the study of such a mixture is the fractionation of the mixture. The most common approach with humic acids is to attempt to obtain a molecular weight fractionation...
Accessory apatite from hybrid granitoid rocks of the southern Snake Range, Nevada
Donald E. Lee, Robert E. Mays, Richard E. Van Loenen
1973, Journal of Research of the U.S. Geological Survey (1) 89-98
Analytical data, optical properties, and unit-cell parameters are presented for 24 samples of accessory apatites recovered from hybrid granitoid rocks of the southern Snake Range, Nev.  A complete chemical analysis is given for one. In the Snake Creek-Williams Canyonoutcrop area, where the hybrid rocks grade from granodiorite with 63 percent SiO2 to a...
Antimony-bearing orpiment, Carlin gold deposit, Nevada
Arthur S. Radtke, Charles M. Taylor, Chris Heropoulos
1973, Journal of Research of the U.S. Geological Survey (1) 85-87
Orpiment, As2S3, containing up to 1.5 percent antimony has been recognized in carbonaceous arsenic-rich gold ores in the unoxidized East ore body of the Carlin gold deposit. Associated hydrothermal minerals include realgar (AsS) and quartz. Stibnite, commonly associated with realgar in the ores, has not been observed associated with this type of orpiment....
Upper Cretaceous (Maestrichtian) fossils from the Kenai-Chugach Mountains, Kodiak and Shumagin Islands, Southern Alaska
Sandra H. B. Clark, David L. Jones
1973, Journal of Research of the U.S. Geological Survey (1) 125-136
A thick sequence of highly deformed flyschlike metasandstone, slate, and argillite crops out in southern Alaska in the Kenai-Chugach Mountains and on Kodiak and the Shumagin Islands to the southwest. These poorly fossiliferous rocks have long been considered Cretaceous in age because of scattered occurrences of fragmentary shells of Inoceramus. Mainly on the basis of...
Effect of septic-tank wastes on quality of water, Ipswich and Shawsheen River basins, Massachusetts
L.G. Toler, George B. Morrill III
1973, Journal of Research of the U.S. Geological Survey (1) 117-120
Many housing projects in the metropolitan area of Boston are beyond the reach of municipal sewer systems. Waste water disposed of through septic-tank or cesspool systems percolates to ground-water reservoirs and eventually reaches the streams. The dissolved-solids load in the streams receiving septic-tank effluent is increased by an amount that can be predicted from the...
A precautionary note on the use of mixed solvents in soxhlet extraction procedures
Alan A. Roberts, James George Palacas
1973, Journal of Research of the U.S. Geological Survey (1) 221-222
The variation in solvent composition of a mixed solvent used in Soxhlet extraction of sediments has apparently often been overlooked. Owing to azeotropic distillation of the solvent introduced into the apparatus, care must be taken to determine the composition of the solvent actually doing the extracting....
Geologic bench marks by terrestrial photography
Harold E. Malde
1973, Journal of Research of the U.S. Geological Survey (1) 193-206
A photograph made with a level camera, if taken at a known height above a permanent mark on the ground, can be later repeated with exactness for measurement of changes in terrain. Such a photograph is one of several means for establishing a geologic bench mark and is especially useful for monitoring the subtle...
Magnetizations of some Late Cretaceous glassy tuffs, volcanic breccias, and altered basalts of the Elkhorn Mountains volcanic field, Western Montana
W. F. Hanna
1973, Journal of Research of the U.S. Geological Survey (1) 179-192
New magnetization data for Late Cretaceous glassy welded tuffs, volcanic breccias, and altered basalts from the Elkhorn Mountains volcanic field, together with geologic, mineralogic, and K-Ar data, indicate that (1) the glassy tuffs have unusually strong, uniform remanent magnetizations which are reversely polarized, much of the remanence perhaps residing in submicroscopic single-domain iron oxide particles within...
Radiometric dating of intrusive rocks in the Cottonwood area, Utah
M. D. Crittenden Jr., J. S. Stuckless, R. W. Kistler, T. W. Stern
1973, Journal of Research of the U.S. Geological Survey (1) 173-178
Recently completed fission-track and K-Ar dating of zircon, sphene, apatite, muscovite, biotite, and hornblende indicate that the Clayton Peak stock was intruded 37-41 m.y. ago, the Alta stock about 32-33 m.y. ago, and the Little Cottonwood stock between 24 and 31 m.y. ago. Pb-a ages on zircon, though showing the same sequence, are about twice...
Geology of part of the southern complex, Marquette district, Michigan
W.F. Cannon, George C. Simmons
1973, Journal of Research of the U.S. Geological Survey (1) 165-172
The southern complex, south of the Marquette synclinorium in the Marquette district of Michigan, is dominantly granitic.  The granitic parts of the complex have Rb-Sr ages of about 2.5 b.y. and are classed as of Precambrian W age. The rocks are divided into two major units: (1.) Bell Creek Gneiss consisting mostly of...