Electrical resistivity studies of subsurface conditions near Antigo, Wisconsin
H. Cecil Spicer
1952, Circular 181
Resistivity measurements are reported for the glaciated area near Antigo, Wis., to locate buried sand and gravel deposits in the glacial drift, which might be developed as aquifers, and to determine depths to the pre-Cambrian bedrock. The results of the resistivity study are presented both as cross sections and as...
U.S. Geological Survey fluorimetric methods of uranium analysis
F. S. Grimaldi, Irving May, Mary H. Fletcher
1952, Circular 199
Bentonite deposits of the Yellowtail district, Montana and Wyoming
Maxwell M. Knechtel, Sam H. Patterson
1952, Circular 150
Geochemical association of niobium (columbium) and titanium and its geological and economic significance
Michael Fleischer, K. J. Murata, Janet D. Fletcher, Perry F. Narten
1952, Circular 225
Twin low-oblique photography and the twinplex plotter
Water Resources Division, U.S. Geological Survey
1952, Circular 222
Reconnaissance for radioactive deposits in south-central Alaska, 1947-49
Robert M. Moxham, Arthur E. Nelson, M.G. White
1952, Circular 184
Water power resources of Hamma Hamma, Duckabush, and Dosewallips Rivers, Washington
Fred F. Lawrence
1952, Circular 109
Evaluation of streamflow records in Rogue River basin, Oregon
Donald Richardson
1952, Circular 187
This report presents data which are, in general, supplementary to those the surface-water investigations made in the past by the U. S. Geological Survey. Those have been essentially investigations of the operation of the many gaging stations on the Rogue River and tributaries. The data presented were obtained from a...
Floods in western Washington--Frequency and magnitude in relation to drainage basin characteristics
G. L. Bodhaine, W.H. Robinson
1952, Circular 191
This report presents a method of determining the magnitude and frequency of expected floods applicable for any area in western Washington (fig. 1). A composite frequency curve was developed that expresses the relation to mean annual floods of floods having recurrence intervals from 1.03 to 50 yr. This composite frequency...
New Year flood of 1949 in New York and New England
Water Resources Division, U.S. Geological Survey
1952, Circular 155
Selected papers on uranium deposits in the United States
Water Resources Division, U.S. Geological Survey
1952, Circular 220
The industrial utility of public water supplies in the West North-Central States, 1952
E. W. Lohr, P.C. Benedict, H. A. Swenson, T.B. Dover
1952, Circular 206
The carnotite prospects of the Craven Canyon area, Fall River County, South Dakota
Lincoln R. Page, Jack Allison Redden
1952, Circular 175
The recovery of ground-water levels in Brooklyn, New York, from 1947 to 1950
Norbert Joseph Lusczynski
1952, Circular 167
No abstract available....
Industrial clays, other than potential sources of alumina of the Columbia Basin
I. G. Sohn
1952, Circular 158
During World War II, the Columbia Basin in Idaho, Oregon, Washington, and the western portion of Montana developed into an important industrial area because of the abundance of hydroelectric ,Power and industrial raw materials. The industries that were established led to a substantial increase in Population, and additional industrial and...
The occurrence of zeunerite at Brooks Mountain, Seward Peninsula, Alaska
Walter S. West, Max Gregg White
1952, Circular 214
Hydrologic reconnaissance of the Green River in Utah and Colorado
H. E. Thomas
1952, Circular 129
The Green River, rising in Wyoming and draining high mountains in that state, northeast Utah and northwest Colorado, is a major tributary of the Colorado River. In the late summer, after the snow has melted from these mountains, the flow in the Green River reaches its minimum for the year....
Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho
James D. Vine, George Winfred Moore
1952, Circular 212
Uraniferous coal, carbonaceous shale, and carbonaceous limestone occur in the Bear River formation of Early Cretaceous age at the Fall Creek prospect, in the Fall Creek area, Bonneville County, Idaho. The uranium compounds are believed to have been derived from mildly radioactive silicic volcanic rocks of Tertiary age that rest...
Records of wells drilled for oil and gas in Montana
James David Vine, Charles Edgar Erdmann
1952, Circular 172
The coal deposits of the Alkali Butte, the Big Sand Draw, and the Beaver Creek fields, Fremont County, Wyoming
Raymond M. Thompson, Vincent L. White
1952, Circular 152
Large coal reserves are present in three areas located between 12 and 20 miles southeast of Riverton, Fremont County, central Wyoming. Coal in two of these areas, the Alkali Butte coal field and the Big Sand Draw coal field, is exposed on the surface and has been developed to some...
Sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana
Charles Herbert Hembree, B. R. Colby, H. A. Swenson, J.R. Davis
1952, Circular 170
Evaluation of streamflow records in Big Wood River basin, Idaho
Robert Paul Jones
1952, Circular 192
Coal resources of Virginia
Andrew Brown, Henry L. Berryhill Jr., Dorothy A. Taylor, James V. A. Trumbull
1952, Circular 171
The U. S. Geological Survey and the Virginia Geological Survey have cooperated in preparing this reappraisal of the coal resources of Virginia, which is based on a study of all information" on the reserves of the State available in the publications and files of the two organizations, supplemented by mine...
Water resources of the Detroit area, Michigan
Chester Owen Wisler, G.J. Stramel, Leslie Bostwick Laird
1952, Circular 183
The water used for all purposes in the Detroit area is obtained from three sources: Lake St. Clair and the Detroit River, their tributary streams and inland lakes, and ground water. During 1950 Lake St. Clair and the Detroit River provided 2,896 million gallons per day (mgd), or 98.3 percent...
Water-loss investigations: Volume 1--Lake Hefner studies technical report
Water Resources Division, U.S. Geological Survey
1952, Circular 229