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Page 4785, results 119601 - 119625

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Not all publications have extents, not all extents are completely accurate
Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results
Arthur H. Lachenbruch, J.H. Sass, L.A. Lawver, M.C. Brewer, T.H. Moses
1982, Open-File Report 82-1039
As permafrost is defined by its temperature, the only way to determine its depth is to monitor the return to equilibrium of temperatures in boreholes that penetrate permafrost. Such measurements are under way in 25 wells on the Alaskan Arctic Slope; 21 are in Naval Petroleum Reserve Alaska (NPRA), and...
Determination and analysis of bearing capacity of calcarenites off the Florida Keys
J.S. Booth, R.A. Farrow, G.N. Wiley, R.C. Circe
1982, Open-File Report 82-309
A specially designed instrument was used to determine the in situ bearing capacity at 12 sites in the carbonate sand seaward of the Florida Keys. The resulting data set not only represents unique information in such an environment, but also provided an opportunity to determine whether bearing capacity is controlled...
Drainage areas of the Kanawha River basin, West Virginia
M.V. Mathes, J.R. Kirby, D.D. Payne Jr., R.A. Shultz
1982, Open-File Report 82-351
This report lists in tabular form approximately 1,500 drainage area divisions in the Kanawha River basin of West Virginia. Drainage areas, compiled in downstream direction, are for streams having a drainage area of approximately 5 square miles and larger and for U.S. Geological Survey gaging stations. Sites on streams for...
Electrical studies at the proposed Wahmonie and Calico Hills nuclear waste sites, Nevada Test Site, Nye County, Nevada
D.B. Hoover, Michael P. Chornack, K.H. Nervick, M. M. Broker
1982, Open-File Report 82-466
Two sites in the southwest quadrant of the Nevada Test Site (NTS) were investigated as potential repositories for high-level nuclear waste. These are designated the Wahmonie and Calico Hills sites. The emplacement medium at both sites was to be an inferred intrusive body at shallow depth; the inference of the...
Estimated oil and gas reserves, Gulf of Mexico Outer Continental Shelf and Continental Slope, December 31, 1981
Jack E. Hewitt, Jeff P. Brooke, John H. Knipmeyer, R.M. Surcouf
1982, Open-File Report 82-34
Remaining recoverable reserves of oil* and gas in the Gulf of Mexico Outer Continental Shelf and Continental Slope have been estimated to be about 2.90 billion barrels of oil and 39.8 trillion cubic feet of gas, as of December 31, 1981. These reserves are recoverable from 445 studied fields under...
An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78
J.J. Murphy, J.R. Ritter, A.E. Brown, J.P. Chiarella
1982, Open-File Report 81-1115
Data recorded from 1973 through 1978 by monitors on West Branch Brandywine Creek at Modena, East Branch Brandywine Creek below Downingtown, and Brandywine Creek at Chadds Ford were analyzed to evaluate the effectiveness of the monitors in describing water-quality conditions. The data show that the stream at Modena and below...
Evaulation of remote sensing, geological and geophysical data for south-central New York and northern Pennsylvania
M. H. Podwysocki, H. A. Pohn, J. D. Phillips, M. D. Krohn, T. L. Purdy, I.S. Merin
1982, Open-File Report 82-319
A study was made of the relationship between lineaments observed on Landsat satellite images and the geologic framework of a portion of the Allegheny Plateau of south-central New York and northern Pennsylvania. The area is underlain by a relatively thick sequence of salt and other evaporites in the Silurian Salina...
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...
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 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...
A field study of littoral processes in Estero Bay, California
J.R. Dingler, R. J. Anima, D.E. Molzan, Gretchen Luepke, C.L. Peterson
1982, Open-File Report 82-537
Estero Bay, which lies on the central California coast, has rocky headlands at both ends and sandy beaches within it. The shoreline of the bay has adjusted to be in equilibrium with the predominant wave climate, which is from the northwest. Because of its present shoreline configuration, the net southward...
Field, model, and computer simulation study of some aspects of the origin and distribution of Colorado Plateau-type uranium deposits
F.G. Ethridge, D.K. Sunada, Noel Tyler, Sarah Andrews
1982, Open-File Report 82-589
Numerous hypotheses have been proposed to account for the nature and distribution of tabular uranium and vanadium-uranium deposits of the Colorado Plateau. In one of these hypotheses it is suggested that the deposits resulted from geochemical reactions at the interface between a relatively stagnant groundwater solution and a dynamic, ore-carrying...
Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina
Page C. Valentine
1982, Professional Paper 1222
Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina is based on the study of 24 wells along two transects, one extending across the seaward-dipping sedimentary basin termed the 'Southeast Georgia Embayment' northeastward to the crest of the Cape Fear Arch, and the other alined east-west, parallel...