Electrical resistivity measurements in the Neillsville area, Wisconsin
H. Cecil Spicer, George J. Edwards
1955, Open-File Report 55-173
Sixty-eight electrical depth profiles were completed in the vicinity of Neillsville, Wis. to obtain information on the water-bearing beds in the glacial moraine and consolidated sedimentary rocks in the area. No productive aquifers were found but the best areas for test drilling are described. The basic theory and interpretation procedures,...
Fossils from bore holes on the Eastern Shore Peninsula, Virginia
Ruth Todd, Julia A. Gardner, I. G. Sohn
1955, Open-File Report 55-181
This report lists Foraminifera, Mollusca, and Ostracoda in five bore holes that penetrated a maximum of 445 feet of section in sediments of Pleistocene and Miocene age, and discusses the paleoecologic and stratigraphic significance of the fossils. It includes the contents of references 6, 16, and 18 of Virginia Division...
Geologic investigations of radioactive deposits, semiannual progress report for June 1 to November 30, 1955
1955, Trace Elements Investigations 590
This report is a statement of progress during the six-months period from June 1 to November 30, 1955 on investigations of radioactive materials in the United States and Alaska, undertaken by the U.S. Geological Survey under the sponsorship of the U.S. Atomic Energy Commission. During the period the Geological Survey's program...
Preliminary geologic map showing the distribution of uranium deposits and principal ore-bearing formations of the Colorado Plateau region
1955, Miscellaneous Field Studies Map 16
No abstract available....
Uranium deposits of the northern part of the Boulder Batholith, Montana
George E. Becraft
1955, Trace Elements Memorandum 944
Uranium minerals and radioactivity anomalies occur in many silver-lead veins and chalcedony veins and vein zones in the Boulder batholith of southwestern Montanao Pitchblende has been identified in a few silver-lead veins. These veins occupy shear zones along which there is no evidence of large-scale lateral displacement. The wall rock...
The isotopic variation of common lead in galena from the Front Range and its geological significance
George Phair, Henry Mela
1955, Trace Elements Investigations 506
Origin of uranium deposits
Vincent Ellis McKelvey, D.L. Everhart, R.M. Garrels
1955, Trace Elements Investigations 504
A spectrographic method for determining the hafnium-zirconium ratio in zircon
C. L. Waring, H.W. Worthing
1955, Trace Elements Investigations 502
A colloidal method for the concentration of carbonaceous matter from rocks
Maurice Deul
1955, Trace Elements Investigations 501
The spectrophotometric determination of vanadium as thiocyanate in acetone-water medium
H.I. Feinstein
1955, Trace Elements Investigations 543
Coffinite, a uranous silicate with hydroxyl substitution : a new mineral
Lorin Rollins Stieff, T. W. Stern, A.M. Sherwood
1955, Trace Elements Investigations 538
Radioactivity and uranium content of the Sharon Springs member of the Pierre shale and associated rocks in western Kansas and eastern Colorado
Edwin R. Landis
1955, Trace Elements Investigations 573
As a part of the Geological Survey's program of investigating uranium-bearing carbonaceous rocks on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission, a reconnaissance of the Sharon Springs member of the Pierre shale in western Kansas and eastern Colorado was conducted during 1954. The Sharon Springs...
Criteria for outlining areas favorable for uranium deposits in parts of Colorado and Utah
E. J. McKay
1955, Bulletin 1009-J
Age determinations on New Hampshire granites
John B. Lyons, D. Gottfried, W.L. Smith, H.W. Jaffe, C. L. Waring
1955, Trace Elements Investigations 523
A comparison of two methods for converting grain counts to weight percent composition
Rechard C. Kellagher, Francis J. Flanagan
1955, Trace Elements Investigations 497
Direct radiometric measurement of the uranium and thorium series in equilibrium by gamma-ray scintillation spectrometer
Patrick M. Hurley
1955, Trace Elements Investigations 499
Water resources of the Indianapolis area, Indiana
Claude Martin Roberts, L.E. Widman, P.N. Brown
1955, Circular 366
Water used in the Indianapolis area comes from two sources: the White River and tributary streams and the underground reservoirs formed by the underlying glacial drift and limestone. Surface-water sources provide about 60 mgd (million gallons per day) for public supply and an additional 300 mgd is used by private...
The mineral composition of gummite
Clifford Frondel
1955, Trace Elements Investigations 508
Contribution to the crystallography of uranium minerals
Gabrielle Donnay, J.D.H. Donnay
1955, Trace Elements Investigations 507
Foraminifera from the Arctic Slope of Alaska; Part 2, Jurassic foraminifera
Helen Tappan
1955, Professional Paper 236-B
Photogeologic map of the Clay Hills-9 quadrangle, San Juan County, Utah
P. P. Orkild
1955, IMAP 79
Preliminary report on the geology of the upper La Paz Valley of Bolivia
Ernest Dobrovolny
1955, Open-File Report 55-42
Maps showing radiometry and geochemical sampling done at Wilson's Prospect, Garland County, Arkansas
Ernest Pete Beroni
1955, Open-File Report 55-14
Foraminifera of the Lodo Formation, central California; Part 2, Calcareous foraminifera (Miliolidae and Lagenidae, part)
M.C. Israelsky
1955, Professional Paper 240-B
Preliminary report on part of the Oat Hill quicksilver mine, Mayacmas district, Napa County, California
Philip Forsyth Fix
1955, Open-File Report 55-45
Oat Hill quicksilver mine, located in the Mayacmas district of northern California, and credited with having produced more than 160,000 flasks of quicksilver, was sampled cooperatively by the Buray of Mines and Geological Survey during 1944. 28 diamond drill holes totaling 8,120 feet were drilled by the Bureau of Mines...
