F. W. O’Malley, D.F. Davidson, R.A. Hoppin, R.P. Sheldon
1953, Circular 262
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Publication Extents
Not all publications have extents, not all extents are completely accurateDagfin John Cederstrom, Paul McKelvey Johnston, Seymour Subitzky
1953, Circular 275
anonymous
1953, Open-File Report 53-281
S.C. Creasey, A.E. Granger
1953, Miscellaneous Field Studies Map 9
The Lake Valley district was originally developed as a manganese-silver district, but the known silver-bearing ore bodies have long since been worked out. The critical shortage of manganese during World War II renewed interest in the manganese deposits; from October 1941 through June 1942 the U. S. Geological Survey and...
Roger Warren Swanson, W.R. Lowell, E. R. Cressman, D.A. Bostwick
1953, Circular 209
Andrew J. Lang, Jack Allison Redden
1953, Circular 245
The Fourmile area, Custer County, S. Dak., is underlain by pre-Cambrian metamorphic rocks that surround the granitic core of the Black Hills. The main structure in the area is the upright limb of an overturned anticline that plunges about 30 ? S. 10 ? E. Three units of metamorphic rocks...
R. C. Culler, Harold V. Peterson
1953, Circular 223
Roger Warren Swanson, Vincent Ellis McKelvey, Richard Porter Sheldon
1953, Circular 297
John William Mangan, Jack Bennett Graham
1953, Circular 257
No abstract available...
W.S. Twenhofel
1953, Circular 252
David B. Tait, R. C. Baker, G. A. Billingsley
1953, Circular 241
Arthur Johnson, William Stephens Twenhofel
1953, Circular 280
Full development of a proposal to divert the headwaters of the Yukon River drainage from Canada into the Taiya River valley of Alaska would make available more than a half million kilowatts of electrical energy. Utilization of this block of power, for which there is at present no local market,...
Chester Keeler Wentworth, Gordon Andrew Macdonald
1953, Bulletin 994
Holly Clyde Wagner
1953, Bulletin 995-A
Frank Saverio Grimaldi
1953, Open-File Report 53-81
No abstract available....
J. L. Meuschke, John R. Henderson Jr.
1953, Geophysical Investigations Map 101
No abstract available....
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1212
This volume is one of a series of 18 reports presenting measurements of stage, discharge, and content of streams, lakes, and reservoirs in the United States during the water year ending September 30, 1951. Since 1888, when the United States Geological Survey first studied streamflow in relation to problems of...
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,...
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1171
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1208
Arthur E. Flint, Charles E. Brown
1953, Open-File Report 53-72
The exploratory holes were drilled as part of a larger geologic investigation, the objective of which is to determine in the Dubuque, Iowa, area the probable occurrence of zinc and lead ore stratigraphically lower than that which has been mined.The primary purpose of the drilling was to supply information required...
Lorin Delbert Clark
1953, Open-File Report 53-37
The Norway Lake area straddles the south margin of the Sagola basin, an embayment of Ruronian sedimentary rocks into the west side of a complex of crystalline and sedimentary rocks of pre-Ruronian age. The north part of the Norway Lake area is underlain by the Randville dolomite, an unnamed succession...
Richard Walter Lemke
1953, Geologic Quadrangle 31
V.E. McKelvey, L.E. Smith, R.A. Hoppin, F.C. Armstrong
1953, Circular 210
Luna Bergere Leopold, Thomas Maddock Jr.
1953, Professional Paper 252
Some hydraulic characteristics of stream channels - depth, width, velocity, and suspended load - are measured quantitatively and vary with discharge as simple power functions at a given river cross section. Similar variations in relation to discharge exist among the cross sections along the length of a river under the...