J. W. Clarke, D.B. Vitaliano, V.S. Neuschel, and others
1961, Bulletin 1116-E
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Publication Extents
Not all publications have extents, not all extents are completely accurateR. C. Newcomb
1961, Professional Paper 383-A
J. W. Clarke, D.B. Vitaliano, V.S. Neuschel, and others
1961, Bulletin 1116-D
Raymond Dewey Sample, H. F. Albee, Hal G. Stephens
1961, Open-File Report 61-141
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-12
G. H. Davis
1961, Water Supply Paper 1535-B
Chemical analyses of waters of streams that drain the semiarid eastern slope of the southern Coast Ranges in California demonstrate that differences in the anion composition, especially in the ratio of bicarbonate to sulfate, are related chiefly to the lithologic character of the rocks exposed in the tributary drainage area....
J.E. Moore
1961, Open-File Report 61-106
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-14
Harald Drewes, G.D. Fraser, G. L. Snyder, H.F. Barnett Jr.
1961, Bulletin 1028-S
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-15
Charles F. Withington
1961, Open-File Report 61-174
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...
R. W. Davis, C.F. Dyer, J.E. Powell
1961, Water Supply Paper 1534
Artesian aquifers underlie most of South Dakota and large areas in adjacent States. About 15,000 wells have been completed since 1881 in these aquifers within South Dakota. Many wells that originally flowed have ceased to flow and have been abandoned, and others have been equipped with pumps. Many thousands, however,...
W. H. Condon
1961, Bulletin 1108-B
Edwin Butt Eckel
1961, Bulletin 1114
No abstract available....
James R. Balsley, J. L. Meuschke
1961, Open-File Report 61-10
Max D. Crittenden Jr., Louis Pavlides
1961, Open-File Report 61-39
Water Resources Division, U.S. Geological Survey
1961, Professional Paper 424-A
The Geological Survey is engaged in many different kinds of investigations in the fields of geology and hydrology. These investigations may be grouped into several broad, inter-related categories as follows:(a) Economic geology, including engineering geology(b) Regional geologic mapping, including detailed mapping and stratigraphic studies(c) Resource and topical studies(d) Ground-water studies(e)...
J. W. Clarke, D.B. Vitaliano, V.S. Neuschel, and others
1961, Bulletin 1146-B
Ruth Reece King, V.M. Jussen, E.S. Loud, G.D. Conant, M.C. Mead, E. H. de Chadenedes
1961, Bulletin 1115
Lucien M. Brush Jr.
1961, Professional Paper 282-F
The hydraulic, basin, and geologic characteristics of 16 selected streams in central Pennsylvania were measured for the purpose of studying the relations among these general characteristics and their process of development. The basic parameters which were measured include bankfull width and depth, channel slope, bed material size and shape, length...
H. L. James, L. D. Clark, C.A. Lamey, F.J. Pettijohn
1961, Professional Paper 310
Robert G. Reeves
1961, Open-File Report 61-126
No abstract available....
Thomas E. Mullens, Glen Arthur Izett
1961, Open-File Report 61-109
No abstract available. ...