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Publication Extents

Not all publications have extents, not all extents are completely accurate
Results of exploration at Lost Creek schroeckingerite deposit, Sweetwater County, Wyoming
Douglas M. Sheridan, John T. Collier, Richard S. Sears
1952, Trace Elements Memorandum 288
The U. S. Geological Survey, on behalf of the Atomic Energy Commission, from July 1951 to February 1952, explored the Lost Creek schroeckingerite deposit, Sweetwater County, Wyoming, by means of auger- drilling, trenching, and bucket-drilling. This report presents an estimate of the inferred ore reserves obtained during this exploration. The inferred reserves are presented under...
Preliminary report on diamond-drill exploration on Outlaw Mesa, Mesa County, Colorado
George K. Brasher
1952, Trace Elements Memorandum 295
Outlaw Mesa is northeast of the Dolores River, about 10 miles southeast of Gateway, Mesa County, Colo. It is an oval-shaped area of about 17 square miles lying mostly within T. 50 N., R. 17 W«, and T. 50 No, R. 18 W., New Mexico principal meridian. The area is accessible by three unimproved...
Preliminary summary of reconnaissance for uranium on the Seward Peninsula, Alaska, During 1951
M.G. White, W.S. West
1952, Trace Elements Memorandum 322
Reconnaissance examinations for uranium were made at nine localities in the York, Nome, and Koyuk districts of the Seward Peninsula, Alaska, during .the 1951 field season. In addition carborne radiometric traverses were made of four roads in the Nome and Council districts. Only at Brooks Mountain in the York district are uranium-bearing deposits that required...
Cyclic fluctuations of water level as a basis for determining aquifer transmissibility
John G. Ferris
1952, Report
In coastal areas, wells near bodies of tidal water frequently exhibit sinusoidal fluctuations of water level, in response to periodic changes of tidewater stage.  Inland, the regulation of a surface reservoir often produces correlative changes of ground-water stage in wells adjacent either to the reservoir or to its attendant stream....
Geophysical observations in parts of the Grants District, McKinley County, New Mexico
Kenneth L. Cook, Calvin K. Moss
1952, Trace Elements Investigations 244
Geophysical observations near Haystack Mesa in the Grants district, McKinley County, New Mexico, had the dual objective of investigating the unusual occurrence of negative aeromagnetic anomalies in close association with airborne radioactivity anomalies, and of investigating other geophysical methods which might assist directly or indirectly in the search for uranium ores in the Grants district....
Carnotite resources of Outlaw Mesa, Mesa County, Colorado
G.K. Brasher
1952, Trace Elements Investigations 163
The U.S. Geological Survey explored Outlaw Mesa for carnotite deposits from 1949 through 1951 with 1,302 diamond-drill holes that totaled 222,150 feet. Total production from Outlaw Mesa from 1914 through 1951 was about 30,000 short tons of carnotite ore, having an estimated grade of about 0.40 percent U3O8 and 1.7 percent...
Carnotite resources of Club Mesa, Montrose County, Colorado
Leonid Bryner
1952, Trace Elements Investigations 147
Club Mesa is 1 mile west of Uravan, Montrose County, Colo. About 200,000 short tons of carnotite ore containing an estimated 0.45 percent U3O8 and 2.1 percent V2O5 has been mined from the mesa. This production represents about one-fifth of the carnotite ore mined from the Colorado Plateau. All the principal deposits on the...
Molting of northern yellow-throat in southern Michigan
R. E. Stewart
1952, The Auk (69) 50-59
During the summer of 1938, detailed studies were made of the molts of the Northern Yellow-throat, Geothlypis trichas brachidactyla, in southern Michigan. Observations of the post-natal molt were made each day on nestlings found near Geddes Pond, one mile east of Ann Arbor. Studies of the post-juvenal and post-nuptial...
Present and past ground-water conditions in the Morrison Formation in southwestern Colorado and southeastern Utah
D. A. Phoenix
1952, Trace Elements Investigations 161
Field and laboratory studies of ground-water conditions in the carnotite-bearing Morrison formation in southwestern Colorado and southeastern Utah were undertaken to determine possible relations between ground waters and the carnotite deposits. The ore-bearing sandstone consists of lenticular sandstone strata, interbedded within discontinuous layers of mudstone; these strata were deposited in a...
Where are the ducks?
W. Slavik, F.M. Uhler
Shirley A. Briggs, editor(s)
1952, Book chapter, The Potomac Valley: History and Prospect
Ground-water data collected in the Missouri River basin units in Kansas during 1951
B.J. Mason, Delmar W. Berry
1952, Report
Ground-water studies in the Missouri River Basin were begun by the United States Geological Survey during the fall of 1945 as a part of the program for development of the resources of the basin by the U.S. Bureau of Reclamation and other Federal Agencies. The studies of the ground-water resources...