Clyde Polhemus Ross
1950, Bulletin 955-E
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Publication Extents
Not all publications have extents, not all extents are completely accurateDeane Frederick Kent
1950, Circular 71
A study of ground water as related to mining in cavernous limestones and dolomites in eastern Tennessee was made in 1946 by the U. S. Geological Survey. Surface and subsurface mapping indicated the geologic control of underground channels. Several methods of tracing water were tried and new techniques in using...
V.P. Sokoloff (translator), H. E. Hawkes
1950, Open-File Report 48-21
Frank E. Byrne, Henry V. Beck, Charles H. Bearman, Claude W. Matthews
1950, Circular 40
Carl E. Dutton
1950, Circular 84
Norman M. Denson
1950, Circular 78
No abstract available....
Charles Brian Read, R. T. Duffner, G. H. Wood, A.D. Zapp
1950, Circular 89
A study of water quality degradation due to brine contamination was made in an area of about 1,700 sq mi in east-central Oklahoma. The study area coincides in part with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age. Water samples collected from 180 wells completed in the Vamoosa-Ada aquifer...
Henry L. Berryhill, Donald M. Brown, Andrew Brown, Dorothy A. Taylor
1950, Circular 81
The Antlers aquifer, which consists of as much as 900 feet of friable sandstone, silt, clay, and shale crops out in areas of 1 ,860 square miles and underlies about 4,400 square miles in southeastern Oklahoma. Precipitation ranges from 34 to 50 inches per year across the outcrop area which...
Judith Weiss Frondel, Michael Fleischer
1950, Circular 74
During 1980, an estimated 121 million gallons of water per day was pumped in a 26-county area in east-central Georgia from sand aquifers of Paleocene and Late Cretaceous age. Maximum withdrawals were at the kaolin mining and processing centers in Twiggs, Wilkinson, and Washington Counties, where water levels have declined...
Max E. Willard, Daniel Linehan
1950, Open-File Report 50-52
Three segments of the proposed relocation of Route 116, stations 7 to 135, in Cheshire, Mass. require shallow cuts. For the purpose of obtaining information on the depths to bedrock, and on the nature of the overlaying materials, seismic and geologic studies were made of the segments in October 1949....
Edward Huntington Cobb
1950, Open-File Report 50-32
No abstract available....
S. W. Hobbs, R. E. Wallace, Allan Bingham Griggs
1950, Open-File Report 50-40
G. A. Macdonald, J.B. Orr
1950, Bulletin 974-A
Roland W. Brown
1950, Professional Paper 221-D
Albert Herbert Koschmann
1950, Open-File Report 50-19
W.C. Stoll
1950, Professional Paper 229
Charles B. Hunt, V.P. Sokoloff
1950, Professional Paper 221-G
J. L. Meuschke
1950, Open-File Report 50-47
Morris Mordecai Thompson
1950, Circular 82
Water Resources Division, U.S. Geological Survey
1950, Circular 72
The index lists the stream-flow ana reservoir stations in the Pacific Slope Basins in California for which records have been or are to be published for periods prior to September 30, 1948. The stations are listed in downstream order. Tributary streams are indicated by indention....
T.B. Dover
1950, Open-File Report 50-69
Pure water does not exist in nature. Because water is a powerful solvent, every drop of rain water carries dissolved or suspended material - dust, pollen, and smoke, as well as the atmospheric gases, oxygen, nitrogen and carbon dioxide. When rain falls, the water running over the rocks and percolating...
Lincoln Ridler Page
1950, Trace Elements Investigations 88
F.W. Cater, L.C. Craig, D. A. Phoenix
1950, Trace Elements Investigations 110
R.W. Stallman
1950, Open-File Report 50-97
M.L. Brashears Jr.
1950, Open-File Report 50-59
Since 1932 the United States Geological Survey in cooperation with the New York Water Power and Control Commission, the Nassau County Department of Public Works, the Suffolk County Water Authority, and the Suffolk County Board of Supervisors has conducted studies dealing with the occurrence, movement, quantity, quality, and temperature of...