Harley Barnes, Robert L. Christiansen
1967, Bulletin 1244-G
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Publication Extents
Not all publications have extents, not all extents are completely accurateR. L. Parker
1967, Professional Paper 440-D
R. K. Blankennagel
1967, Open-File Report 67-18
This report describes the testing techniques used by the U. S. Geological Survey to obtain hydrologic data in deep holes drilled in volcanic rocks at Pahute Mesa, Nevada Test Site. The testing program in each hole includes geophysical logging, pumping, and injecting and swabbing between straddle packers. Rock lithologies and...
G.H. Hughes
1967, Professional Paper 272-H
Roy Newcome
1967, Water Supply Paper 1839-K
Abundant ground-water resources underlie the Pascagoula River basin. These resources have been developed intensively in only a few places--namely, Hattiesburg, Laurel, Meridian, and Pascagoula. Seepage from the ground water reservoirs sustains the base flows of the Leaf, Chickasawhay, Pascagoula, and Escatawpa Rivers and their tributaries. The fresh-water-bearing section is 300...
R. W. Imlay
1967, Professional Paper 573-B
R. W. Mower
1967, Water Supply Paper 1839-E
The Clear Lake Springs in southeastern Millard County are the source of water for the maintenance of the Clear Lakes Migratory Waterfowl Refuge. Seasonal declines in the rate of discharge were noted during 1959-60.Fluctuations in the flow of Clear Lake Springs are caused both by natural variations in the quantity...
Frank Cogswell Canney, William L. Lehmbeck, Frank E. Williams
1967, Bulletin 1230-J
No abstract available....
Division Of Wildlife Research
1967, Wildlife Leaflet 478
George Vincent Cohee, Walter S. West, Lorna C. Wilkie
1967, Bulletin 1254-A
No abstract available....
M.R. Stewart
1967, Hydrologic Atlas 260
R.W. Cruff, T. H. Thompson
1967, Water Supply Paper 1839-M
This study compared potential evapotranspiration, computed from climatological data by each of six empirical methods, with pan evaporation adjusted to equivalent lake evaporation by regional coefficients. The six methods tested were the Thornthwaite, U.S. Weather Bureau (a modification of the Permian method), Lowry-Johnson, Blaney-Criddle, Lane, and Hamon methods. The test...
William M. McMaster
1967, Water Supply Paper 1839-N
Peter H. Mattson
1967, Bulletin 1254-B
C. Gilbert Bowles
1967, Open-File Report 67-26
No abstract available. ...
S. Anthony Stanin, Bismarck R. Cooper
1967, Open-File Report 68-257
Boyd R. Haley
1967, Open-File Report 67-104
No abstract available....
Water Resources Division, U.S. Geological Survey
1967, Water Data Report MN-66-1-2
Norman L. Hatch Jr.
1967, Bulletin 1254-D
D.L. Hart Jr.
1967, Open-File Report 67-285
The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies;...
E.M. MacKevett Jr., D. A. Brew, C. C. Hawley, L.C. Huff, James G. Smith
1967, Open-File Report 67-151
Water Resources Division, U.S. Geological Survey
1967, Water Data Report CO-66-2
Burnett W. Saunders
Ellis L. Yochelson, editor(s)
1967, Bulletin 1210
Loyd L. Young
1967, Open-File Report 67-283
James E. Case
1967, Open-File Report 67-39
A 40-50-mgal gravity low trends northeast along the Colorado mineral belt between Monarch Pass and Breckenridge, Colorado. The low is probably caused by a silicic Tertiary batholith of lower density than adjacent Precambrian crystalline rocks. Many major mining districts associated with silicic Tertiary intrusives are near the axis of the...