Robert M. Moxham, Walter S. West
1953, Circular 265
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateHelmuth Wedow
1953, Circular 248
E. W. Lohr, W. F. White, N.H. Beamer
1953, Circular 283
David B. Tait, R. C. Baker, G. A. Billingsley
1953, Circular 241
Roger Warren Swanson, Vincent Ellis McKelvey, Richard Porter Sheldon
1953, Circular 297
Roger Warren Swanson, W.R. Lowell, E. R. Cressman, D.A. Bostwick
1953, Circular 209
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...
Lorin Rollins Stieff, T. W. Stern, R.G. Milkey
1953, Circular 271
Donald Cave Duncan
1953, Circular 291
Montis Ruhl Klepper, F.S. Honkala, O.A. Payne, E. T. Ruppel
1953, Circular 260
William James Drescher, Frederick C. Dreher, Paul N. Brown
1953, Circular 247
Charles W. Drennen
1953, Circular 267
The Coastal Plain sediments of Fayette and Lamar Counties, Ala., are pre-Selma Late Cretaceous in age and are divided into three mappable units, from oldest to youngest: (i) the Coker formation, (2) the Gordo formation, and (3) a unit composed of the McShan and Eutaw formations undifferentiated. The Coker formation...
Verl Richard Wilmarth
1953, Circular 312
The Yellow Canary uranium deposit is on the west side of Red Creek Canyon in the northern part of the Uinta Mountains, Daggett County, Utah. Two claims have been developed by means of an adit, three opencuts, and several hundred feet of bulldozer trenches. No uranium ore has been produced...
Hugh Richard Gault, P.L. Killeen, W.S. West, R. F. Black, J.B. Lyons, M.G. White, J.J. Matzko
1953, Circular 250
No abstract available....
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...
D.F. Davidson, R.A. Smart, H.W. Peirce, J.D. Weiser
1953, Circular 305
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...
Diane Curtis, Shirley Loleta Simpson Houser
1953, Circular 281
R. C. Culler, Harold V. Peterson
1953, Circular 223
Donald Richard Wiesnet, Lois E. Randall, Benjamin E. Jones
1953, Circular 227
Donald R. Wiesnet, Lois Emily Randall, Benjamin E. Jones
1953, Circular 263
Loyd L. Young, Benjamin Earl Jones
1953, Circular 200
Fred Forrest Lawrence
1953, Circular 292
The Crystal River drains the western slope of the Elk Mountains, a relatively small range in the southern Rocky Mountain province, and flows into the Roaring Fork 13 miles southeast of Glenwood Springs, Colo. The lower 7 miles of the valley is cultivated, but upstream from this stretch the valley...
Jules Newton Stich
1953, Circular 234
Earle Rupert Cressman, W.H. Wilson, C.W. Tandy, W.J. Garmoe
1953, Circular 302