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Not all publications have extents, not all extents are completely accurate
Summary of the mineralogy of the Colorado Plateau uranium ores
Alice D. Weeks, Robert Griffin Coleman, Mary E. Thompson
1956, Trace Elements Investigations 583
In the Colorado Plateau uranium has been produced chiefly from very shallow mines in carnotite ores (oxidized vanadiferous uranium ores) until recent deeper mining penetrated black unoxidized ores in water-saturated rocks and extensive exploration has discovered many deposits of low to nonvanadiferous ores. The uranium ores include a wide...
X-ray powder data for uranium and thorium minerals
Clifford Frondel, Daphne Riska, Judith Weiss Frondel
1956, Trace Elements Investigations 575
The U.S. Geological Survey has in preparation a comprehensive volume on the mineralogy of uranium and thorium. This work has been done as part of a continuing systematic survey of data on uranium and thorium minerals on behalf of the Division of Raw Materials, U.S. Atomic Energy Commission. Pending publication of...
Sources of the elements in the sandstone-type uranium deposits of the Colorado Plateau
Eugene M. Shoemaker, W.L. Newman, A.T. Miesch
1956, Trace Elements Investigations 629
Sandstone-type uranium deposits of the Colorado Plateau are epigenetic. Certain elements have been added locally to the sandstone host to form the deposits; the added fraction of each element in the deposits is call extrinsic to distinguish it from the part present in the original unmineralized host. The principal extrinsic...
Zinc and copper mineralization of the Vazante area, Minas Gerais, Brazil
Samuel L. Moore
1956, Open-File Report 56-82
A large body of zinc and copper mineralization is exposed in a line of low hills about 5 kilometers east of the small village of Vazante in the northwestern part of the state of Minas Gerais, Brazil. The Vazante area can be reached by roads leading north from the State...
U.S. Geological Survey exploration program in the Trixie area, East Tintic mining district, Utah County, Utah
H. T. Morris, A.E. Disbrow, Thomas Seward Lovering
1956, Open-File Report 56-84
The Trixie area is in the south central part of the East Tintic mining district, Utah, and is believed to include the intersections of several mineralized pebble dike-fissure zones and a major, easterly trending fault. The fissure-fault intersections, which are considered to be favorable ore-locallizing structures, are concealed by lavas...
Engineering geology of the Katalla area, Alaska
Reuben Kachadoorian
1956, Open-File Report 56-66
A geological examination of the Katalla area, Alaska, was made during the summer of 1)55 at the request of and in cooperation with the Alaska Road Commission. The Katalla area herein defined lies in the Cordova A-1, A-2, B-1, and B-2 quadrangles (fig. 1), and encompasses most of the area...
Permafrost and ground-water conditions in the Glennallen area, Alaska
Donald R. Nichols
1956, Open-File Report 56-91
This report is an outgrowth of permafrost and geologic field studies now in progress in the southeastern Copper River basin, Alaska and is in response to inquiries for information on permafrost and ground-water conditions. Various private and governmental groups have encountered severe differential settlement of building foundations on permafrost, and...
Distribution of uranium in the Bisbee district, Cochise County, Arizona
Stewart R. Wallace
1956, Trace Elements Investigations 426
The Bisbee district has been an important source of copper for many years, and substantial amounts of lead and zinc ore and minor amounts of manganese ore have been mined during certain periods. The copper deposits occur both as low-grade disseminated ore in the Sacramento Hill stock and as massive...
Volumetric determination of uranium using titanous sulfate as reductant before oxidimetric titration
James S. Wahlberg, Dwight L. Skinner, Lewis F. Rader
1956, Trace Elements Investigations 614
A new method for determining uranium in samples containing 0.05 percent or more U3O8, using titanous sulfate as reducing agent, is much shorter, faster, and has fewer interferences than conventional methods using reductor columns. The sample is dissolved with sulfuric, nitric, perchloric, and hydrofluoric acids. Elements that would otherwise form insoluble...
Geology and ore deposits of the Chicago Creek area, Clear Creek County, Colorado
J. E. Harrison, J. D. Wells
1956, Trace Elements Investigations 432
The Chicago Creek area, Clear Creek County, Colo., forms part of the Front Range mineral belt, which is a northeast-trending belt of coextensive porphyry intrusive rocks and hydrothermal veins of Tertiary age. More than $4.5 million worth of gold, silver, copper, lead, zinc, and uranium was produced from the mines...
Geology of the Copper King uranium mine, Larimer County, Colorado
Paul Kibler Sims, George Phair, Robert Hadley Moench
1955, Trace Elements Investigations 424
The Copper King mine in Larimer County, Colo., in the northern part of the Front Range of Colorado, was opened in World War I in an unsuccessful attempt to mine copper and zinc ore. In 1949, following the discovery of pitchblende on the dump, the mine was reopened, and it...
Ore deposits on northwestern Chichagof Island, Alaska
Darwin L. Rossman
1955, Open-File Report 55-154
The area mapped includes most of northwestern Chichagof Island. The work, started in 1946, is a continuation of the geologic mapping done in the adjoining Chichagof mining district by Reed and Coats. The gold-bearing zone recognized by these writers continues through the area mapped by the writer to the northern...
Ground-water conditions between Oracle and Oracle Junction, Pinal County, Arizona
L.A. Heindl
1955, Open-File Report 55-63
The development of the San Manuel copper prospect has greatly increased traffic along State Highway 77. Considerable interest in commercial possibilities along that road has resulted in a request by the Arizona State Land Department for information about the ground-water conditions between Oracle and Oracle Junction. This request came too...
Relation of uranium to hypogene mineral zoning in the Front Range mineral belt, Colorado
Stewart Raynor Wallace, B. F. Leonard, R. H. Campbell
1955, Trace Elements Investigations 357
Many of the mining districts of the Colorado Front Range mineral belt contain mesothermal sulfide ores that exhibit a zonal distribution. Present data indicate that in most of the zoned districts pitchblende and/or secondary uranium minerals are most abundant in a transition zone between central areas containing predominantly pyritic gold...
Uranium deposits at the Jomac mine, White Canyon area, San Juan County, Utah
A.F. Trites, G.A. Hadd
1955, Trace Elements Investigations 561
The Jomac mine is in the White Canyon area. San Juan County, Utah, about 13 miles northeast of the town of White Canyon, Utah. The mine is owned by the Ellihill Mining Company, White Canyon, Utah. Mine workings consist pf two adits connected by a crosscut. Two hundred feet of...
Radioactivity and uranium content of some Cretaceous shales, central Great Plains
Harry A. Tourtelot
1955, Trace Elements Investigations 298
The Sharon Springs member of the Pierre shale of Cretaceous age, a hard black organic-rich shale similar to the Chattanooga shale, is radioactive throughout central and western South Dakota, most of Nebraska, northern Kansas, and northeastern Colorado. In the Missouri River valley, thin beds of the shale contain as much...