anonymous
1953, Open-File Report 53-281
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Publication Extents
Not all publications have extents, not all extents are completely accurateFrank Darwyn Spencer, Margaret Isabelle Erwin
1953, Circular 258
No abstract available....
Charles Henry Prior, Robert Schneider, W. H. Durum
1953, Circular 274
The water supply of the Minneapolis-St. Paul area is adequate to satisfy present requirements and requirements for many years to come if the area continues to develop at about the present rate. The flow of -the Mississippi River at the Twin Cities is more than sufficient to meet the demands of...
Jules Newton Stich
1953, Circular 234
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1203
Frank Darwyn Spencer
1953, Circular 266
The Indiana coal field forms the eastern edge of the eastern interior coal basin, which is near some of the most densely populated and highly productive manufacturing areas of the United States. (See fig. 1. ) For this reason Indiana coal reserves are an important State and National asset. In...
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1165
F. W. O’Malley, D.F. Davidson, R.A. Hoppin, R.P. Sheldon
1953, Circular 262
H. E. LeGrand
1953, Open-File Report 53-152
M.G. White, P.L. Killeen
1953, Circular 255
Investigations in 1947 in the Lower Yukon-Kuskokwim region, Alaska found that previously reported radioactivity in the vicinity of Flat is due to uraniferous zircon, an accessory mineral in monzonite. The monzonite intrudes mafic igneous and Upper Cretaceous sedimentary rocks. The maximum equivalent-uranium content of the zircon is 0.14 percent, and...
Earle Rupert Cressman, W.H. Wilson, C.W. Tandy, W.J. Garmoe
1953, Circular 302
Walter S. West
1953, Circular 300
Radioactivity in the southern and eastern parts of the Darby Mountains, Seward Peninsula, Alaska, appears to be directly related to the occurrence of granite. Concentrates from placers derived from areas containing granite are more radioactive than concentrates from placers not derived from the granite and, generally, contain from 0.01 to...
John Richard Rapp, W. H. Durum
1953, Circular 243
Julius Schlocker, G. H. Davis
1953, Open-File Report 53-233
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1214
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1213
J. L. Meuschke, John R. Henderson Jr.
1953, Geophysical Investigations Map 101
No abstract available....
Philip T. Stafford, Kenneth J. Englund
1953, Coal Map 15
This report on coal in the Buckhorn quadrangle, Kentucky, is the second of a series of preliminary reports published by the U.S. Geological Survey as part of a program of investigation of the geology and coal resources of eastern Kentucky. The first report, Coal Investigations Map C5 (Johnston and Heck,...
E. A. Moulder, Alfred E. Torrey, F. C. Koopman
1953, Circular 198
No abstract available....
J. F. Poland, L.C. Dutcher
1953, Open-File Report 54-246
This memorandum was prepared at the request of Henry Harris, Acting Area Director, Bureau of Indian Affairs, Sacramento, Calif., to report on recent conditions at the Agua Caliente Spring, Palm Springs, Calif., and to suggest further possibilities for restoring the spring discharge to its pre-road-construction condition....
J.E. Maynard, R.M. Hazelwood
1953, Open-File Report 53-182
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1183
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...
Richard Walter Lemke
1953, Geologic Quadrangle 31
V.E. McKelvey, L.E. Smith, R.A. Hoppin, F.C. Armstrong
1953, Circular 210