Richard L. Bernknopf, David S. Brookshire, Russell H. Campbell, Carl D. Shapiro, Robert W. Fleming
1985, Open-File Report 85-276-D
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Page 4530, results 113226 - 113250
Publication Extents
Not all publications have extents, not all extents are completely accurateP. G. Schruben
1985, Open-File Report 86-34
R. B. O'Sullivan
1985, Miscellaneous Field Studies Map 1816
F.C. Frischknecht, D.P. O'Brien, R. Grette, P. V. Raab
1985, Open-File Report 85-614-B
No abstract available....
M. A. Kuntz, H.N. Elsheimer, L.F. Espos, P.R. Klock
1985, Open-File Report 85-593
J. P. Minard
1985, Miscellaneous Field Studies Map 1743
D. G. Emerson, J. D. Wald
1985, Open-File Report 85-700
Governmental units that have been identified as having flood hazard areas but do not have detailed base flood information are required to use the ' best available data ' to regulate new development or expansion of existing development in flood prone areas. Information for flood plain management has been identified...
J. V. Brahana, M. W. Bradley
1985, Water-Resources Investigations Report 83-4012
The Knox aquifer is composed of the Cambrian and Ordovician age carbonate rocks of the Knox Group. This aquifer occurs throughout Tennessee, west of the Valley and Ridge province. The Knox crops out in the Sequatchie Valley and in the Wells Creeks cryptoexplosive structure on the Northwestern Highland Rim. Groundwater...
W.C. Overstreet, T. H. Kiilsgaard, M. J. Grolier, D. L. Schmidt, J. A. Domenico, M. M. Donato, Theodore Botinelly, T. F. Harms
1985, Open-File Report 85-755
Kenneth R. Watts, Lloyd E. Stullken
1985, Open-File Report 81-344
The High Plains aquifer in Kansas is part of a regional system that extends from South Dakota to Texas. In Kansas, the aquifer underlies an area of 30,900 square miles in the western and south-central part. The aquifer is a hydraulically connected aggregation of unconsolidated water-bearing deposits. The High Plains...
1985, Open-File Report 85-493
This report summarizes the progress of water-resources studies in Utah by the U.S. Geological Survey from July 1, 1984, to June 30, 1985. Much of the work was done in cooperation with the State of Utah and local agencies. Additional supporting funds were transferred from other Federal agencies or appropriated...
G. D. Bath, C.E. Jahren
1985, Open-File Report 85-459
Margaret A. Daley, Elizabeth L. Ambos, Gary S. Fuis
1985, Open-File Report 85-531
N. B. Rybicki, Virginia Carter, R. T. Anderson, T. J. Trombley
1985, Open-File Report 85-77
No abstract available....
V.M. Glanzman
1985, Open-File Report 85-363
S. D. May, Arthur Grantz
1985, Open-File Report 85-742
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,...
R.J. Fleck, D.G. Hadley
1985, Open-File Report 85-727
Joe Edds, J.L. Spencer
1985, Open-File Report 85-478
The report contains 622 ground-water level measurements made in observation wells in Arkansas in the spring of 1985. In addition , the report contains well hydrographs relating to the Quaternary aquifer and the Sparta Sand aquifers, the most important aquifers with respect to ground-water availability and use in Arkansas. (USGS)...
S. D. May, B. D. Ruppel, Arthur Grantz
1985, Open-File Report 85-601
J. H. Dover
1985, Open-File Report 85-216
No abstract available....
D.E. Detra, J.E. Kilburn
1985, Open-File Report 85-244
No abstract available....
M.G. Detroy
1985, Open-File Report 84-815
A ground-water-quality monitoring network has been designed to collect data to describe the long-term chemical quality of major bedrock and Quaternary aquifer systems in Iowa. The network was designed because of data needs expressed by several State and Federal agencies. Areas where new or additional data are needed are nitrate and...
T.M. Messier, M. E. O'Neill, W.H. Lee
1985, Open-File Report 85-436
R. P. Fogelman, K. L. Johnson
1985, Open-File Report 85-485
A sedimentation study of Loch Lomond Reservoir in Santa Cruz County, California, was begun in 1982 to determine reservoir storage capacity and to establish permanent ranges for future studies. Results of a reservoir survey indicated a total storage capacity of 8,824 acre-ft in 1982. Comparison of thalweg profiles from this...