E.D. Gordon, Charles Francis Withington, V.T. Dow
1953, Trace Elements Investigations 213
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Publication Extents
Not all publications have extents, not all extents are completely accurateRobert G. Luedke, Eugene Merle Shoemaker
1953, Open-File Report 53-162
Walter S. West
1953, Trace Elements Investigations 53
George William Moore
1953, Trace Elements Investigations 235
R.G. Ray
1953, Open-File Report 53-228
R.G. Ray
1953, Open-File Report 53-229
J. M. Scott
1953, Open-File Report 53-234
John Lawrence Kulp, D.A. Brobst
1953, Open-File Report 53-143
No abstract available....
C.L. McGunness
1953, Open-File Report 53-164
John Henry Frederick Feth, Coyd Bickley Yost
1953, Circular 233
No abstract available....
C.S. Conover
1953, Open-File Report 53-46
E. M. Cushing
1953, Open-File Report 53-49
James Franklin Pepper, Wallace De Witt Jr., Gail M. Everhart
1953, Bulletin 1003-A
The Canton, Dover, Massillon, and Navarre quadrangles cover about 880 square miles in eastern Ohio. Canton is the largest city in the mapped area. In these four quadrangles, the well drillers generally recognize three "Clinton" sands - in descending order, the "stray Clinton", the "red Clinton", and the "white Clinton"....
Water Resources Division, U.S. Geological Survey
1953, Open-File Report 53-29
No abstract available. ...
Steven Norman Daviess, M. N. Bramlette
1953, Open-File Report 53-52
Clay is mined in open pits by several companies in the Alberhill district, and the refractory clays of relatively high alumina sediment are used largely for fire brick. The Alberhill Coal and Clay Company is the largest operator and has produced a little over 2,000,000 tons of clay, of which...
Water Resources Division, U.S. Geological Survey
1953, Trace Elements Investigations 280
Bruce R. Colby, C. H. Hembree, E. R. Jochens
1953, Circular 270
This report gives the results of an investigation by the U. S. Geological Survey of the sediments and dissolved minerals that are transported by the Moreau River. The Moreau River drainage basin is a narrow basin in northwestern South Dakota that covers about 5, 360 square miles of rolling, grassy plains,...
Arthur Earle Granger
1953, Circular 296
Helen L. Cannon
1953, Circular 264
Carl E. Kindsvater, R. W. Carter, Hubert Jerome Tracy
1953, Circular 284
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...
W. C. Alden
1953, Professional Paper 231
L. R. Page
1953, Professional Paper 247
No abstract available....
J. M. Scott
1953, Open-File Report 53-235
Bruce R. Colby, D.Q. Matejka, David Wellington Hubbell
1953, Circular 205
This report contains results of observations that were made from the time when a natural constriction was formed in the Niobrara River near Valentine, Nebr., to the time when it was widened by high flows. After the constriction was widened, insufficient turbulence was developed to suspend most of the sediment....