W.D. Wood, L.J. Snell
1977, Water-Resources Investigations Report 77-135
No abstract available. ...
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Publication Extents
Not all publications have extents, not all extents are completely accurateArthur O. Westfall, Earl E. Webber
1977, Water-Resources Investigations Report 77-23
A time-of-travel study was made on a 106-mile reach of the Tuscarawas River to determine average velocity and dispersion characteristics between selected points. The reach was divided into five subreaches, and a fluorescent dye used as a tracer material. At about the 50-percent flow-duration level, time of travel of the...
A. T. Rutledge
1977, Water-Resources Investigations Report 77-89
The swamps, marshes, and open waters of Tsala Apopka Lake, Florida, were mapped and the hydrologic connection between the lake and the Floridan limestone aquifer was studied from October 1975 to September 1976. Tsala Apopka Lake is a series of shallow , interconnected lakes, ponds, and marshes whose water surface...
Donald Robert Rima, Mary S. Moran, E. Jean Woods
1977, Water-Resources Investigations Report 77-86
Ground water occurs in the Murfreesboro area in solution openings in the otherwise dense paleozoic limestones that underlie most of central Tennessee. Test drilling based on conceptual models of ground-water occurrence in carbonate-rock aquifers indicate that multimillion-gallon-per-day supplies could be developed from strategically located production wells in the Shiloh and...
W. D. Nichols
1977, Water-Resources Investigations Report 77-73
Continued decline of water levels in the Englishtown aquifer, in New Jersey, has caused considerable concern regarding the ability of the aquifer to meet future yield demands. A detailed study of the capability of the aquifer to yield water entailed the use of a digital computer simulation model to evaluate...
W.D. Wood, L.J. Snell
1977, Water-Resources Investigations Report 77-134
No abstract available. ...
R. A. Pettijohn
1977, Water-Resources Investigations Report 77-40
Studies of seven landfills in the Indianapolis, Indiana, area indicate that in five of the landfills movement of ground water is from the deep aquifers into the uppermost aquifer. In the other two landfills, movement of ground water is from the shallow aquifers to the deeper aquifers, so that leachate...
Ann Zurawski
1977, Open-File Report 77-609
No abstract available....
H.R. Seitz
1977, Open-File Report 76-886
John S. Bader, J.L. Chisholm, S. C. Downs, R.L. Bragg
1977, Open-File Report 77-848
Charles R. Wood, David B. MacLachlan
1977, Open-File Report 77-407
N.E. Hutchison, N.G. Stuthman, C.F. Merk, W.L. Isherwood Jr.
1977, Open-File Report 77-729-I
Ferdinand Quinones-Marquez, Pedro Vazquez, Rafael Pena
1977, Open-File Report 77-237
E. F. Hubbard
1977, Open-File Report 77-423
Alfred R. Taylor
1977, Open-File Report 77-521
C.R. Tuttle, John Peck
1977, Open-File Report 77-544
Water Resources Division, U.S. Geological Survey
1977, Water Data Report CO-76-1
S. M. Coleman (compiler), K. L. Pierce
1977, Miscellaneous Field Studies Map 904
H. R. Covington
1977, Miscellaneous Field Studies Map 862
P.R. Carlson, B. F. Molnia, S.C. Kittelson, J.C. Hampson Jr.
1977, Miscellaneous Field Studies Map 876
R. G. Bohannon
1977, Miscellaneous Field Studies Map 922
Water Resources Division, U.S. Geological Survey
1977, Water Data Report OH-76-2
Water Resources Division, U.S. Geological Survey
1977, Water Data Report OH-76-1
N. R. D. Albert, W. C. Steele
1977, Miscellaneous Field Studies Map 767-C
W.N. Blair, N.J. Page, M. G. Johnson
1977, Miscellaneous Field Studies Map 861
No abstract available....