F. A. Swenson
1953, Open-File Report 53-252
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Page 2661, results 66501 - 66525
Publication Extents
Not all publications have extents, not all extents are completely accurateAllen and others Sinnott
1953, Open-File Report 53-248
C.B. Simmons, G.A. LaRocque Jr.
1953, Open-File Report 53-247
G. A. Billingsley, J.H. Hubble
1953, Open-File Report 53-22
W.A. Beetem
1953, Open-File Report 53-20
D. F. Dougherty
1953, Open-File Report 53-55
C.N. Durfor, Walter B. Keighton
1953, Open-File Report 53-56
George D. Graeff Jr.
1953, Open-File Report 53-78
No abstract available....
L.C. Dutcher, A. A. Garrett
1953, Open-File Report 53-58
J.G. Ferris
1953, Open-File Report 53-65
J. H. Feth
1953, Open-File Report 53-66
No abstract available....
A. A. Garrett, L.C. Dutcher
1953, Open-File Report 53-76
David B. Tait, R. C. Baker, G. A. Billingsley
1953, Circular 241
Vinton Crews Fishel, J.K. Searcy, F. H. Rainwater
1953, Circular 273
William James Drescher, Frederick C. Dreher, Paul N. Brown
1953, Circular 247
P. W. Guild
1953, Economic Geology (48) 639-676
Various origins have been proposed for the itabirite and associated hematite ores of Minas Gerais, Brazil. The U.S. Geological Survey, in cooperation with the Brazilian Departamento Nacional da Produqao Mineral, has undertaken a comprehensive program of mapping of these Precambrian deposits, which bear many similarities to other Precambrian iron formations....
R. F. Kreiss, B. R. Colby, Ning Chien
1953, Eos, Transactions, American Geophysical Union 796-797
The author has developed equations and approximate curves to express the percentage of the total sediment discharge that is carried in suspension above the lowest point reached by the nozzle of a depth‐integrating sediment sampler. He assumes that bed load and suspended load are defined by the equations in a...
Harold C. Troxell
1953, Eos, Transactions, American Geophysical Union (34) 552-562
The steep and rugged mountains of Southern California contain considerable ground‐water storage. A large portion of the runoff is seepage from this storage The variations in runoff distribution depend on the geology, physiography, and soil cover of these mountain areas....
Carl Fries Jr.
1953, Eos, Transactions, American Geophysical Union (34) 603-616
Estimates of the weights of pyroclastic material and lava erupted by Parícutin Volcano from early 1943 to early 1952 have given a pyroclastic weight of some 2230 million metric tons and a lava weight of about 1330 million metric tons, making a total of 3560 million metric tons of solids....
W.B. Nelson, H.E. Thomas
1953, Eos, Transactions, American Geophysical Union (34) 74-84
Data collected at the Topaz Relocation Center provide an excellent record of the development and subsequent disappearance of a cone of depression caused by pumping. This Center occupied temporarily an area of natural ground‐water discharge on the floor of the Sevier Desert in west‐central Utah. Water for a population of 6500 was pumped from artesian wells which tapped aquifers...
Water Resources Division, U.S. Geological Survey
1953, Report
Carl H. Gaum
1953, Book chapter, The physical and economic foundation of natural resources; Volume 4: Subsurface facilities of water management and patterns of supply, type area studies
No abstract available....
H. Wedow Jr., J.M. Stevens, G.E. Tolbert
1953, Trace Elements Investigations 197
Several mines and prospects in the Fairbanks and Livengood quadrangles, east-central Alaska, were examined for the possible presence of radioactive materials in the summer of 1949. Also tested were pre-Cambrian and Paleozoic metamorphic and sedimentary rocks crossed by the Elliott Highway, which extends from Fox, near Fairbanks, northward about 70...
Donald G. Wyant
1953, Trace Elements Investigations 51
Deposits of uraniferous hydrocarbons are associated with carnotite in the Shinarump conglomerate of Triassic age at Shinarump Mesa and adjacent areas of the Temple Mountain district in the San Rafael Swell of Emery County, Utah. The irregular ore bodies of carnotite-bearing sandstone are genetically related to lenticular uraniferous ore bodies...
William James Drescher
1953, Water Supply Paper 1190
The principal water-bearing rocks underlying Brown County, Wis., are thick sandstone units of Cambrian and Ordovician age. Other aquifers include limestone and dolomite of Ordovician age, dolomite of Silurian age, and sands and gravel of Pleistocene and Recent age. Underlying the water-bearing formations are crystalline rocks of pre-Cambrian age which...