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Not all publications have extents, not all extents are completely accurate
A geochemical survey using heavy mineral concentrates in the Mount Belknap caldera vicinity, Utah
R. E. Tucker, W. Roger Miller, J. M. Motooka
1982, Open-File Report 82-602
Geochemical surveys of the rocks, heavy-mineral concentrates, and surface and spring waters in the vicinity of the Mount Belknap caldera, Tushar Mountains, west-central Utah, were conducted during the summers of 1978 and 1979. Anomalous concentrations of mostly lithophile elements, particularly niobium, beryllium, lead, yttrium, tin, zinc, manganese, and molybdenum in...
Habitat Suitability Index Models: Black bullhead
Robert J. Stuber
1982, FWS/OBS 82/10.14
The native range of the black bullhead (Ictalurus melas) extends from North Dakota eastward through southern Canada to the upper tributaries of the St. Lawrence River and southward and westward to Texas and northern Mexico (Trautman 1957; Hubbs and Lagler 1958: Scott and Crossman 1973). It has been wide ly...
Organic solutes in ground water at the Idaho National Engineering Laboratory
Jerry A. Leenheer, Jefferson C. Bagby
1982, Water-Resources Investigations Report 82-15
In August 1980, the U.S. Geological Survey started a reconnaissance survey of organic solutes in drinking water sources, ground-water monitoring wells, perched water table monitoring wells, and in select waste streams at the Idaho National Engineering Laboratory (INEL). The survey was to be a two-phase program. In the first phase,...
Hydrogeologic and water-quality characteristics of the Ironton-Galesville aquifer, southeast Minnesota
J. F. Ruhl, R. J. Wolf, D. G. Adolphson
1982, Water-Resources Investigations Report 82-4080
Quality of water in the Ironton-Galesville aquifer is generally acceptable for all kinds of uses. Calcium magnesium bicarbonate type water is most common. The dissolved-solids concentration ranges from about 200 to 1,000 milligrams per liter. The lowest values are in the northern part of the aquifer, where the bedrock is...
Hydrology of the low-level radioactive solid waste burial site and vicinity near Barnwell, South Carolina
James M. Cahill
1982, Open-File Report 82-863
Geologic and hydrologic conditions at a burial site for low-level radioactive waste were studied, and migration of leachates from the buried waste into surrounding unconsolidated sediments were evaluated. The burial site and vicinity are underlain by a sequence of unconsolidated sediments of Late Cretaceous, Tertiary, and Quaternary age. These sediments...
Catalog of available clear mylar templates used to determine latitude and longitude of sample localities between the latitudes of 51 degrees 00' and 71 degrees 30' at the scale of 1:63,360 and between the latitude of 49 degrees 00'00" north or south at the scale of 1:250,000
W. L. Campbell, George VanTrump Jr.
1982, Open-File Report 82-723
The present use of electro-mechanical plotting of sample points can give rise to location errors, particularly when map scale changes are involved, unless careful control is maintained. The following catalog of computer-generated mylar templates, with plots of latitude and longitude (longitudes equidistant north to south), sufficient to cover the latitudes...
Water use in the Mississippi Gulf Coast counties, 1980
J.A. Callahan
1982, Open-File Report 82-512
The population served by public water systems in the three counties of Mississippi 's Gulf Coast increased from about 227 ,000 to nearly 253,000 between 1975 and 1980. Water use by public systems increased from about 27.6 million gallons per day to more than 31.3 million gallons per day. Self-supplied...
Reconnaissance geologic map of southwestern Misheguk Mountain quadrangle, Alaska
S.M. Curtis, Inyo Ellersieck, C.F. Mayfield, I.L. Tailleur
1982, Open-File Report 82-611
This map is one of a series of three reconnaissance geologic maps of the southern Misheguk Mountain quadrangle (fig. 1). Because the geology in all three map areas is similar, a composite map explanation has been designed to facilitate their combined use and provide the reader with a better perspective...
Reconnaissance geologic map of southeastern Misheguk Mountain Quadrangle, Alaska
Charles F. Mayfield, S.M. Curtis, Inyo Ellersieck, I.L. Tailleur
1982, Open-File Report 82-613
This map is one of a series of three reconnaissance geologic maps of the southern Misheguk Mountain quadrangle (fig. 1). Because the geology in all three map areas is similar, a composite map explanation has been designed to facilitate their combined use and provide the reader with a better perspective...
Reconnaissance geologic map of south-central Misheguk Mountain Quadrangle, Alaska
Inyo Ellersieck, S.M. Curtis, C.F. Mayfield, I.L. Tailleur
1982, Open-File Report 82-612
This map is one of a series of three reconnaissance geologic maps of the southern Misheguk Mountain quadrangle (fig. 1). Because the geology in all three map areas is similar, a composite map explanation has been designed to facilitate their combined use and provide the reader with a better perspective...
Preliminary survey of ground-water resources for Island County, Washington
D.R. Cline, M. A. Jones, N. P. Dion, K. J. Whiteman, D. B. Sapik
1982, Open-File Report 82-561
Increased ground-water withdrawals associated with the population increase in Island County have caused concern about ground-water availability and potential seawater intrusion. The most widespread and widely used aquifer lies near sea level. Locally, available data also indicate that one or more water-bearing zones lie above the sea-level aquifer. Pumpage in...
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1982
John B. Townshend, J.E. Papp, E.A. Sauter, L.Y. Torrence
1982, Open-File Report 82-300-A
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...
The densities of halite-saturated WIPP-A and NBT-6 brines and their NaCl contents in weight percent, molal, and molar units from 20 to 100 degrees C
I-Ming Chou, B. Buizinga, M.A. Clynne, R.W. Potter
1982, Open-File Report 82-899
A series of density measurements has been performed at 30?, 50?, 70?, and 90?C for halite-undersaturated WIPP-A and NBT-6 brines with various NaCl contents approaching saturation. The densities of halite-saturated WIPP-A and NBT-6 brines were obtained by extrapolating these measured densities to halite saturation points. The maximum difference between the...