E. M. Cushing, P. R. Speer, M.E. Schroeder
1960, Open-File Report 60-34
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Publication Extents
Not all publications have extents, not all extents are completely accurateL.C. Dutcher
1960, Open-File Report 60-39
L.C. Dutcher, W.J. Hiltzen
1960, Open-File Report 60-41
M. S. Griffin, E.N. Clark
1960, Open-File Report 60-61
J. W. Harshbarger, C.A. Repenning, J.T. Callahan
1960, Open-File Report 60-63
L.A. Heindl, O. J. Cosner
1960, Open-File Report 60-64
E. H. Herrick
1960, Open-File Report 60-69
J. W. Hood
1960, Open-File Report 60-71
R. L. Hosman
1960, Open-File Report 60-75
D. W. Hubbell
1960, Open-File Report 60-77
Hydraulic and sediment characteristics at six river sections upstream and downstream from the confluence of the Middle Loup and Dismal Rivers were measured and studied to determine some of the interrelationships between variables and the differences that exist between common variables when two flows unite. The two streams, which flow...
G. A. Izett
1960, Open-File Report 60-78
C.L. Jones
1960, Open-File Report 60-83
Between Project Gnome site and the International Minerals and Chemical. Corporation's plant site, in central eastern Eddy County, N. Mex., unconsolidated deposits of Quaternary age and redbeds of Triassic age attain a thickness of about 700 feet, and rest unconformably on evaporites of late Permian age. The upper Permiau evaporites...
K. S. Muir, P.M. Merritt, G.A. Miller
1960, Open-File Report 60-102
Investigation of the ground-water resources of Santa Barbara County was continued during 1959 by the U. S. Geological Survey in cooperation with the Santa Barbara County Water Agency. Monthly water-level measurements were made in 203 wells, in 8 of which automatic water-level recorders were operated. Earlier measurements, covering the period...
J. R. Rapp
1960, Open-File Report 60-118
G. R. Schiner
1960, Open-File Report 60-121
No abstract available....
P. R. Speer
1960, Open-File Report 60-129
B.L. Stacy
1960, Open-File Report 60-130
Cottonwood Creek basin is a 377 square mile area in central Oklahoma. The rim of the basin has altitudes as high as 1,300 feet, and the mouth is at an altitude of 910. Deposits of Quaternary age consist of alluvium along the stream courses and high terrace deposits along the...
Kenneth L. Cook
1960, Open-File Report 60-30
No abstract available. ...
F.E. Wright, C. W. Wright
1960, Open-File Report 60-158
Fred Kunkel
1960, Circular 433
Several reasonable values are assumed for coefficients of transmissibility and storage of lenticular alluvial deposits, These values when substituted in the Theis (1935) nonequilibrium formula as modified by Wenzel (1942) give curves from which time, distance, drawdown relationships are estimated....
J. V. B. Wells
1960, Water Supply Paper 1553
Eugene T. Oborn
1960, Water Supply Paper 1459-G
Robert Wayne Schnabel
1960, Geologic Quadrangle 134
No abstract available....
Randolph Wilson Bromery, J. R. Henderson, G. L. Zandle
1960, Geophysical Investigations Map 223
No abstract available....
J. V. B. Wells
1960, Water Supply Paper 1558