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Page 4029, results 100701 - 100725

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Water-resources investigations in Wisconsin
D. E. Maertz
1994, Open-File Report 94-321
The statewide average precipitation of 38.79 inches for the 1993 water year was 122 percent of the normal annual precipitation of 31.77 inches for water years 1961-90. Average precipitation values ranged from 103 percent of normal in northwestern Wisconsin to 150 percent of normal in southwestern Wisconsin (Pamela Naber Knox,...
Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)
H.K. Long, J.W. Farrar
1994, Open-File Report 94-42
This report presents the results of the U.S. Geological Survey's analytical evaluation program for eight standard reference samples--T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)--that were distributed in October 1993 to 158 laboratories registered...
Pesticide-sampling equipment, sample-collection and processing procedures, and water-quality data at Chicod Creek, North Carolina, 1992
T.K. Manning, K.E. Smith, C.D. Wood, J. B. Williams
1994, Open-File Report 94-50
Water-quality samples were collected from Chicod Creek in the Coastal Plain Province of North Carolina during the summer of 1992 as part of the U.S. Geological Survey's National Water-Quality Assessment Program. Chicod Creek is in the Albemarle-Pamlico drainage area, one of four study units designated to test equipment and procedures...
Specific yield as determined by type-curve analysis of aquifer-test data
Allen F. Moench
1994, Ground Water (32) 949-957
The commonly used analytical solution developed by Neuman for a homogeneous, water-table aquifer assumes that the drainage of pores in the zone above the water table due to lowering of the water table occurs instantaneously. Noninstantaneous drainage of pores in the unsaturated zone accounts for the finding that both type-curve...
The Venus geologic mappers' handbook
Kenneth L. Tanaka, H. J. Moore, G.G. Shaber, M. G. Chapman, E.B. Stofan, D.B. Campbell, P. A. Davis, J. E. Guest, G.E. McGill, P.G. Rogers, R.S. Saunders, J. R. Zimbelman
1994, Open-File Report 94-438
The geologic framework of southern Lake Michigan
D.S. Foster, D. W. Folger
1994, Journal of Great Lakes Research (20) 44-60
The bathymetry is controlled by the underlying bedrock. Bedrock comprises Silurian dolomite and Devonian limestone and shale. Quaternary sediment, 10 to 40 m thick, overlies bedrock. From Waukegan, Illinois, south to Indiana Harbor, the bottom is floored by till, sand, pebbles, and cobbvles. The lake floor is erosional or nondepositional...
Management of Pacific brant: Population structure and conservation issues
James S. Sedinger, David H. Ward, R. Michael Anthony, Dirk V. Derksen, Calvin J. Lensink, Karen S. Bollinger, Neil K. Dawe
Richard E. McCabe, Kelly G. Wadsworth, editor(s)
1994, Conference Paper, Transactions of the fifty-ninth North American wildlife and natural resources conference
Pacific brant (Branta bernicla) nest from the Yukon-Kuskokwim (Y-) Delta in southwestern Alaska along the coast of North America to the central Canadian arctic (Pacific Flyway Subcommittee on Pacific Brant 1992) (Figure 1). Birds from this population also nest in the Canadian arctic islands south of Prince Patrick Island and...
Effects of surficial geology, lakes and swamps, and annual water availability on low flows of streams in central New England, and their use in low-flow estimation
S. William Wandle Jr., Allan D. Randall
1994, Water-Resources Investigations Report 93-4092
Equations developed by multiple-regression analysis of data from 49 drainage basins in Massachusetts, New Hampshire, Rhode Island, Vermont, and southwestern Maine indicate that low flow of streams in this region is largely a function of the amount of water available to the basin and the extent of surficial sand and...