Howard Klein
1965, Open-File Report 65-86
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateRalph L. Miller
1965, Open-File Report 65-110
H.H. Tanaka, D.L. Hart Jr., R.K. Knott
1965, Open-File Report 65-157
The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig....
Paul R. Seaber, Este F. Hollyday
1965, Open-File Report 65-146
This report describes the availability, quantity, quality, variability, and cost of development of the ground-water resources in the lower Susquehanna River basin. The report has been prepared for and under specifications established by the Corps of Engineers, U. S. Army, and the Public Health Service, Department of Health, Education, and...
Earl E. Brabb, Michael Churkin
1965, Open-File Report 65-20
No abstract available....
F.B. Titus Jr.
1965, Open-File Report 65-160
Salwyn S.W. Chinn
1965, Water Supply Paper 1809-P
The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one...
R. E. Smith, E.G. Kaminski
1965, Open-File Report 65-149
Richard A. Sheppard, Arthur J. Gude
1965, Circular 500
James R. Balsley, C.L. Kruger
1965, Open-File Report 65-12
Winchell Smith, R.L. Hanson, R.W. Cruff
1965, Open-File Report 65-150
This study investigated the relation between lag, or head loss (hL), in a typical stilling-well intake system of a stream-gaging station and rate of change of stage (ΔH/Δt) of the stream. The purpose of the study was to define such a relation in general terms and thus provide a rational...
Henry A. Waldrop, Fred Peterson
1965, Open-File Report 65-167
H.H. Tanaka, D.L. Hart Jr., R.K. Knott
1965, Open-File Report 65-156
The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig....
James R. Balsley, Carl L. Long
1965, Open-File Report 65-9
D. A. Jobin
1965, Open-File Report 65-80
R.M. Wallace
1965, Professional Paper 341-F
Charles Lee Roy Holt
1965, Water Supply Paper 1796
Portage County has abundant resources of generally good quality water and, although water problems exist locally, depletion or general scarcity of water is not likely in the foreseeable future. The county receives annually about 31 inches of precipitation, of which about 21 inches is lost as evaportranspiration. The average annual water...
E.V. Giusti, W.J. Schneider
1965, Professional Paper 422-G
Roger B. Morrison
1965, Professional Paper 477
Arthur Johnson
1965, Open-File Report 65-81
No abstract available....
Paul Livingston Applin, Esther English Richards Applin
1965, Professional Paper 447
No abstract available....
Blair F. Jones
1965, Professional Paper 502-A
Ralph Newton Eicher, A.T. Miesch
1965, Open-File Report 65-52
S. E. Rantz, A.M. Moore
1965, Open-File Report 65-131
D. H. Hart, R. C. Newcomb
1965, Water Supply Paper 1697
The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly,...