Gilbert H. Espenshade
1961, Open-File Report 61-46
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Page 6053, results 151301 - 151325
Publication Extents
Not all publications have extents, not all extents are completely accurateJames R. Balsley, M. E. Hill, J. L. Meuschke
1961, Open-File Report 61-11
No abstract available. ...
C. S. Annell, A.W. Helz
1961, Bulletin 1084-J
Clarence Albert Horr, A.T. Myers, P. J. Dunton, Harold Julius Hyden
1961, Bulletin 1100
Paul R. Barnett
1961, Bulletin 1084-H
D.M. Lemmon, Ogden Tweto
1961, Open-File Report 61-87
Harold Lloyd James, K. L. Wier
1961, Open-File Report 61-76
No abstract available....
Karl M. Waage
1961, Bulletin 1102
Howard Hamilton Waldron
1961, Bulletin 1028-T
Bill L. Stacy
1961, Open-File Report 61-177
Unconsolidated water-bearing alluvial deposits border the Canadian River in the vicinity of Norman, Oklahoma. These Quaternary materials are divided on the basis of topgraphic position into 'high terrace deposits' and 'alluvium.' The high terrace lies at an elevation of 50 to 60 feet above the alluvium, which in turn lies...
Robert George Schmidt, W. T. Pecora, Bruce Bryant, W. G. Ernst
1961, Bulletin 1081-E
Arthur A. Baker
1961, Open-File Report 61-5
Arthur Grantz
1961, IMAP 342
R.G. Petersen
1961, Miscellaneous Field Studies Map 196
Lawrence Allen Warner, E. N. Goddard, and others
1961, Bulletin 1090
Robert Jacob Dunham
1961, Open-File Report 61-42
The Chadron area covers 375 square miles about 25 miles southeast of the Black Hills. Recurrent mild tectonic activity and erosion on the Chadron arch, a compound anticlinal uplift of regional extent, exposed 1900 feet of Upper Cretaceous rocks, mostly marine shale containing pyrite and organic matter, and 600 feet...
M. Gordon Wolman, Lucien M. Brush Jr.
1961, Professional Paper 282-G
The size and shape of equilibrium channels in uniform, noncohesive sands, 0.67 mm and 2.0 mm in diameter, were studied experimentally in a laboratory flume 52 feet long in which discharge, slope, sediment load, and bed and bank material could be varied independently. For each run a straight trapezoidal channel...
Edwin Butt Eckel
1961, Bulletin 1114
No abstract available....
R. D. Cotter, J.E. Rogers
1961, Water Supply Paper 1539-A
The Mountain Iron-Virginia area is a broad, southwest-trending valley in the central part of the Mesabi Range. The valley, which heads in the Laurentian Divide, and covers about 120 square miles, coincides approximately with a bedrock valley filled with as much as 150 feet of glacial deposits. A complex sequence of...
Bruce R. Colby, David Wellington Hubbell
1961, Water Supply Paper 1593
A procedure was presented in 1950 by H. A. Einstein for computing the total discharge of sediment particles of sizes that are in appreciable quantities in the stream bed. This procedure was modified by the U.S. Geological Survey and adapted to computing the total sediment discharge of a stream on...
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-14
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-15
Harald Drewes, G.D. Fraser, G. L. Snyder, H.F. Barnett Jr.
1961, Bulletin 1028-S
Reuben Clair Newcomb, Stuart G. Brown
1961, Water Supply Paper 1539-I
A.H. Chidester, Henry Wilson Worthington
1961, Open-File Report 61-32