Floods of May-July 1950 in southeastern Nebraska
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1137-D
Four floods occurred in southeast Nebraska during the period of May to July 1950. Two of these were the greatest known in the State if the size of the drainage areas is considered, and the other two were not so spectacular but were of notable size and of possible hydrologic...
Floods of November-December 1950 in the Central Valley basin, California
C. G. Paulsen
1953, Water Supply Paper 1137-F
The flood of November-December 1950 in the Central Valley basin was the greatest in most parts of the basin since the turn of the century and probably was exceeded in the lower San Joaquin River basin only by the historic flood of 1862. In respect to monetary loss, the 1950...
Remarks on the program of the Water Resources Division, U. S. Geology Survey, and water problems in California, made before the Association of American State Geologists, Feb. 14, 1953, Los Angeles, California
J. F. Poland
1953, Open-File Report 53-218
Summary report on the geology and ground-water resources of the Baton Rouge Area, Louisiana
Rex Rupert Meyer, A.N. Turcan Jr.
1953, Open-File Report 53-192
Preliminary geologic map of the Glasgow quadrangle, Montana
Water Resources Division, U.S. Geological Survey
1953, Open-File Report 53-137
Water power of the coast streams of Oregon
Randolph O. Helland
1953, Open-File Report 53-109
Fifth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California
Walter Hofmann
1953, Open-File Report 53-121
This report is the fifth in a continuing series of annual progress reports giving the results of discharge measurements made at more than 120 selected sites in the "Tecolote Tunnel Area" of the Santa Ynez Mountains. This area derives its name from the tunnel now being built by the Bureau...
Trace elements research quarterly progress report - April 1 to June 30, 1952
Water Resources Division, U.S. Geological Survey
1953, Trace Elements Investigations 280
Geology and geography of the Henry Mountains region, Utah
Charles B. Hunt, Paul Averitt, Ralph L. Miller
1953, Professional Paper 228
The Henry Mountains region in southeastern Utah is one of the classic areas in geology because of the study made there by Grove Karl Gilbert in 1875 and 1876. His report on the geology of the mountains was the first to recognize that intrusive bodies may deform their host rocks...
A geologic and geophysical reconnaissance of the Doney Park-Black Bill Park area, Arizona, with reference to ground water, with a section on geophysics
John Henry Frederick Feth, Coyd Bickley Yost
1953, Circular 233
No abstract available....
Geologic map of the Smelterville and vicinity quadrangle, Idaho
Water Resources Division, U.S. Geological Survey
1953, Open-File Report 53-29
No abstract available. ...
Geology and ground-water resources of the Covington-Newport alluvial area, Kentucky
Eugene H. Walker
1953, Circular 240
Low flows on Neches River, Texas, September-October 1952, dam B reservoir to mouth of Village Creek
V.L. Austin, W.O. George
1953, Open-File Report 53-6
No abstract available....
Annotated bibliography of U.S. Geological Survey reports on water-power resources, including floods and droughts
Loyd L. Young, Benjamin Earl Jones
1953, Circular 200
Volcanic debris in uraniferous sandstones, and its possible bearing on the origin and precipitation of uranium
Aaron Clement Waters, Harry Clifford Granger
1953, Circular 224
Ground-water conditions in the Soil and Moisture Conservation Demonstration Area near Torrington, Goshen County, Wyoming, with a section on the chemical quality of the ground water
F. N. Visher, H. M. Babcock, W. H. Durum, R. A. Krieger
1953, Circular 238
Sedimentation in small reservoirs on the San Rafael Swell, Utah
Norman Julius King, Mervyn M. Mace
1953, Circular 256
Movement of sediment from upland areas and eventually into main drainages and rivers is by no means through continuous transportation of material from the source to the delta. Instead it consists of a series of intermittent erosional and depositional phases that present a pulsating movement. Hence, sediment carried off upland...
Public and industrial water supplies of the Jackson Purchase region, Kentucky
Henry Louis Pree, William Harry Walker
1953, Circular 287
Ground-water factors affecting the drainage of Area IV, First Division, Buffalo Rapids irrigation project, Montana
E. A. Moulder, Alfred E. Torrey, F. C. Koopman
1953, Circular 198
No abstract available....
Ground-water conditions in the Milwaukee-Waukesha area, Wisconsin
Frank Clingan Foley, W.C. Walton, W.J. Drescher
1953, Water Supply Paper 1229
Three major aquifers underlie the Milwaukee-Waukesha area: sandstones of Cambrian and Ordovician age, Niagara dolomite of Silurian age, and sand and gravel deposits of Pleistocene age. The Maquoketa shale of Ordovician age acts as a more or less effective seal between the Pleistocene deposits and Niagara dolomite above and the...
Surface water supply of the United States, 1950, Part I, North Atlantic slope basins
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1171
Surface water supply of the United States, 1951, Part V, Hudson Bay and upper Mississippi River basins
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1208
Surface water supply of the United States, 1951. Part 8. Western Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1212
This volume is one of a series of 18 reports presenting measurements of stage, discharge, and content of streams, lakes, and reservoirs in the United States during the water year ending September 30, 1951. Since 1888, when the United States Geological Survey first studied streamflow in relation to problems of...
Ground-water data collected in the Missouri River basin units in Kansas during 1952
B.J. Mason, S.J. Underwood
1953, Open-File Report 54-188
No abstract available....
Water supply of the Birmingham area, Alabama
W.H. Robinson, J.B. Ivey, G. A. Billingsley
1953, Circular 254
Sufficient water is available in the streams of the area surrounding Birmingham to supply any foreseeable demand; however, to utilize these streams impounding reservoirs and rather long supply lines will be required. Moderate supplies of ground water are available from wells, springs, and mines. The average water use in the...
