Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1206
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Page 6253, results 156301 - 156325
Publication Extents
Not all publications have extents, not all extents are completely accurateV.E. McKelvey, L.E. Smith, R.A. Hoppin, F.C. Armstrong
1953, Circular 210
V.E. McKelvey, F.C. Armstrong, R. A. Gulbrandsen, R.M. Campbell
1953, Circular 301
V.E. McKelvey, D.F. Davidson, F. W. O’Malley, L.E. Smith
1953, Circular 208
John Beaver Mertie
1953, Circular 237
Monazite, a phosphate of the rare earths, is the principal mineral from which the cerium earths and thorium are obtained. Fluviatile monazite placers were mined in the Piedmont province of North and South Carolina from 1887 to 1911, and again intermittently from 1915 to 1917; but the principal sources In...
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1173
John Richard Rapp, W. H. Durum
1953, Circular 243
E. A. Moulder, Alfred E. Torrey, F. C. Koopman
1953, Circular 198
Robert M. Moxham, Walter S. West
1953, Circular 265
No abstract available....
Raymond L. Nace, W. H. Durum
1953, Circular 166
Robert G. Bates, Helmuth Wedow
1953, Circular 202
F. W. O’Malley, D.F. Davidson, R.A. Hoppin, R.P. Sheldon
1953, Circular 262
Wilbur Nathaniel Palmquist, Francis Ramey Hall
1953, Circular 299
Richard Porter Sheldon, R.G. Waring, M.A. Warner, R.A. Smart
1953, Circular 307
Arthur J. Rosier, L.J. Snell
1953, Circular 201
The Rapid Valley unit is in Pennington County, S. Dak., and extends from the east city limits of Rapid City southeastward for 21 miles along Rapid Creek. The bedrock formations that underlie the region are chiefly marine in origin, and they generally dip eastward from the center of the Black Hills...
John Richard Rapp, H. M. Babcock, W. H. Durum
1953, Circular 163
No abstract available....
M. I. Rorabaugh, Floyd F. Schrader, Leslie Bostwick Laird
1953, Circular 276
Troy Lewis Pewe
1953, Circular 289
W.H. Robinson, J.B. Ivey, G. A. Billingsley
1953, Circular 254
Sufficient water is available in the streams of the area surrounding Birmingham to supply any foreseeable demand; however, to utilize these streams impounding reservoirs and rather long supply lines will be required. Moderate supplies of ground water are available from wells, springs, and mines. The average water use in the...
Charles Thomas Pierson, Quentin Dreyer Singewald
1953, Circular 294
Pitchblende was discovered in July 1951 in the Alma mining district, Park County, Colo., by the U. S. Geological Survey acting on behalf of the U. S. Atomic Energy Commission. The pitchblende is associated with Tertiary veins of three different geologic environments: (1) veins in pre-Cambrian rocks, (2) the London...
R.P. Sheldon, M.A. Warner, M.E. Thompson, H.W. Peirce
1953, Circular 304
The U. S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Idaho and other western states. These data. will not be fully synthesized and analyzed for several years, but segments of the data, accompanied by little or no interpretation, are published as preliminary reports as...
Henry Louis Pree, William Harry Walker
1953, Circular 287
W.S. Twenhofel
1953, Circular 252
William James Drescher, Frederick C. Dreher, Paul N. Brown
1953, Circular 247
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...