Carol A. Finn, D.R. Spydell, D.L. Williams
1985, Open-File Report 85-280
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateK.J. Lanfear, J.C. Schornick
1985, Open-File Report 85-92
R. L. Goemaat, L.D. Mize, D.E. Spiser
1985, Open-File Report 85-87
During the 1983-84 climatic years, the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, collected ground-water level data in Oklahoma from 1,083 sites in 77 counties. This report presents those data points....
P.B. Dawson, Reese Cutler, J.R. Evans
1985, Open-File Report 85-243
T.A. Moore, R.W. Stanton
1985, Open-File Report 85-20
K. Y. Lee, A.J. Froelich
1985, Open-File Report 85-217
No abstract available....
Clay M. Conway
1985, Open-File Report 85-240
Stratiform zinc-copper massive-sulfide deposits at Al Masane occur in thin dolomitic interbeds within Proterozoic felsic crystal tuff and mafic flows and volcaniclastics. These strata dip steeply westward and are underlain by shale and shaly graywacke to the east and overlain by lapilli crystal tuff to the west. This section is...
L. F. Hintze
1985, Open-File Report 85-119
No abstract available....
K.C. Galyean, D. B. Adams, D.L. Collins
1985, Open-File Report 83-858
Two years (water yr 1980 and 1981) of data collected by the U.S. Geological Survey for the U.S. Department of Energy, Naval Petroleum and Oil Shale Reserves, in the Parachute Creek drainage basin of northwestern Colorado are tabulated. Data were obtained from five surface water gages, two automatic sediment samplers,...
K. Y. Lee
1985, Open-File Report 85-230
George Garklavs, L.G. Toler
1985, Open-File Report 84-856
Ground-water flow velocity was estimated in a tract of land adjacent to a low-level radioactive-waste disposal site near Sheffield, Illinois, by measuring the time-of-travel between two wells spaced 110 feet apart. Rhodamine WT dye was the principal tracer used in the test. The leading edge and peak concentrations of Rhodamine...
J. M. Knott, S. W. Lipscomb
1985, Open-File Report 85-157
C.D. Masters
1985, Open-File Report 85-248
Myung W. Lee, S.Y. Suh
1985, Open-File Report 85-289
R.E. Needham
1985, Open-File Report 84-756
R.E. Needham
1985, Open-File Report 85-278
A. K. Cooper, M. S. Marlow, J.R. Childs
1985, Open-File Report 85-237
K.R. Ludwig
1985, Open-File Report 85-141
S.A. Frenzel, M.L. Jones
1985, Open-File Report 85-159
James M. Gerhart, George J. Lazorchick
1985, Open-File Report 84-748
Ground water in the 3,458-square-mile lower Susquehanna River basin occupies secondary openings in bedrock. The distribution of openings is a function of lithology, depth, and topography. Local flow systems account for most of the total ground-water flow. Average annual recharge for the lower basin is 1,857 million gallons per day,...
M. E. Gettings
1985, Open-File Report 85-15
Paleomagnetic studies of 25 oriented bedrock specimens from Jabal Mahd adh Dhahab, located 160 km southeast of Al Madinah, Kingdom of Saudi Arabia, have yielded important structural information relating to the geologic history of this base and precious metal deposit. Samples were collected along one traverse away from the mineralized...
F.W. Jennings, J.M. Botbol, G. I. Evenden
1985, Open-File Report 85-11
No abstract available....
E. A. Johnson, J.L. Hook
1985, Open-File Report 85-37
A. K. Cooper, M. S. Marlow, J.R. Childs
1985, Open-File Report 85-236
R. A. Crovelli
1985, Open-File Report 85-294