Geology of the northern Crystal Falls area, Iron County, Michigan
F.J. Pettijohn
1952, Circular 153
The industrial utility of public water supplies in the West South-Central States, 1952
E. W. Lohr, J.R. Avrett, Burdge Irelan, G. A. Billingsley, T.B. Dover
1952, Circular 221
Water levels and artesian pressure in observation wells in the United States, 1949, Part 2, Southeastern States
Water Resources Division, U.S. Geological Survey
1952, Water Supply Paper 1157
Uranium-bearing coal and carbonaceous rocks in the Fall Creek area, Bonneville County, Idaho
James D. Vine, George Winfred Moore
1952, Circular 212
Uraniferous coal, carbonaceous shale, and carbonaceous limestone occur in the Bear River formation of Early Cretaceous age at the Fall Creek prospect, in the Fall Creek area, Bonneville County, Idaho. The uranium compounds are believed to have been derived from mildly radioactive silicic volcanic rocks of Tertiary age that rest...
Supergene and hydrothermal dispersion of heavy metals in wall rocks near ore bodies, Tintic district, Utah
H. T. Morris, T. S. Lovering
1952, Economic Geology (47) 685-716
Part I, T. S. Lovering. Preliminary work in the Tintic district, Utah, determined the relative distance of migration of ore metals in moist carbonate and silicic wall rocks near ore, and in ground water having a very sluggish circulation through mineralized ground. The analyses of efflorescences in the Tintic Standard mine openings at suitable localities indicated that under the conditions existing during the past 25 years lead has not...
Glaciation and drainage changes in the fish Lake Plateau, Utah
Clyde T. Hardy, S. Muessig
1952, Geological Society of America Bulletin (63) 1109-1116
The Fish Lake Plateau, nearly centrally located among the High Plateaus of Utah, exhibits glacial and other geomorphic features of regional significance. The plateau is divided into two areas by Fish Lake and the wide valley of Sevenmile Creek. The Fish Lake trough is a structural basin; Sevenmile Valley may be largely erosional. Volcanic rocks of Tertiary age underlie most of the plateau;...
The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage
Charles V. Theis
1952, Conference Paper
No abstract available ...
Discussion of “tide‐producing forces and artesian pressures”
Tom Culbertson, William O. George, Frederick E. Romberg
1952, Eos, Transactions, American Geophysical Union (33) 597-600
I was an employee of the Texas State Board of Water Engineers in charge of the Fort Stockton field office at the time that the data for this paper were gathered. Since I have done both extensive and detailed ground‐water work in the Fort Stockton area, including the setting and...
Nonsteady flow to a well of constant drawdown in an extensive aquifer
C.E. Jacob, S.W. Lohman
1952, Eos, Transactions, American Geophysical Union (33) 559-569
A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical...
Nonsteady flow to a well of constant drawdown in an extensive aquifer
C.E. Jacob, S.W. Lohman
1952, Eos, Transactions, American Geophysical Union (33) 559-569
A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical...
Origin of the Chattanooga shale
Louis C. Conant
1952, Trace Elements Investigations 237
Tonight I will try to present to you the chief facts we have observed that have a bearing on the old problem of how the black shales originated. Some of the ideas have been used before, and some are new. Some of those that have been used before, have been used to...
Geology of the area adjacent to the Free Enterprise uranium-silver Mine, Boulder District, Jefferson County, Montana
W.A. Roberts, A. J. Gude III
1952, Trace Elements Memorandum 140
Uranium minerals.occur in pods associated with cryptocrystalline silica, silver minerals, and scattered sulfide mineral grains in a hydrothermal vein that cuts quartz monzonite and alaskite at the Free Enterprise mine, 2 miles west of Boulder, Mont. The Free Enterprise vein is one of many silicified reef-like structures in this area,...
Ground water notes
Water Resources Division, U.S. Geological Survey
1952, Report
No abstract available....
Occurrence of uranium-bearing coal, carbonaceous shale, and carbonaceous limestone in the Fall Creek area, Bonneville County, Idaho
James D. Vine, George W. Moore
1952, Trace Elements Memorandum 340
Uraniferous coal, carbonaceous shale, and carbonaceous limestone occur in the Bear River formation of Upper Crestaceous age at the Fall Creek prospect, in the Fall Creek area, Bonneville County, IDaho. The uranium compounds are believed to have been derived from mildly radioactive silicic volcanic rocks of the Tertiary age...
Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana
William J. Hail Jr., James R. Gill
1952, Trace Elements Memorandum 446
A reconnaissance search for uraniferous lignite and carbonaceous shale was made in western Montana and adjacent parts of Idaho during the summer of 1951. Particular emphasis in the examination was placed on coal and carbonaceous shale associated with volcanic rocks, as volcanic rocks in many area appear to have released...
Memorandum on ground-water investigation of four proposed stock wells in Puertocito Area, Socorro County and Canoncito Area, Bernalillo and Valencia Counties, New Mexico
C.A. Repenning, S.E. Galloway
1952, Report
At the request of the Navajo Service, Office ot Indian Affairs, a groundwater iinvestigation of four proposed stock wells in the Puertocito Area, Socorro county and the Canoncito Area., Bernalillo and Valencia counties,New Mexico, was made in November, 1951 (see fig. 1). Although these areas are not on the Navajo...
Hybridization of Canada geese with blue geese in the wild
H.K. Nelson
1952, The Auk (69) 425-428
While carrying out hunter bag checks in the vicinity of Sand Lake National Wildlife Refuge, Columbia, South Dakota, during the 1950 waterfowl hunting season, the author examined two adult male geese which proved to be crosses between one of the smaller Canada Geese (possibly Richardson's Goose, Branta canadensis hutchinsi) and...
Water resources of the Buffalo-Niagara Falls region
Charles William Reck, Edward Taber Simmons
1952, Circular 173
No abstract available....
Silicone water-repellents (Mimeograph)
S. F. Snieszko
1952, Report
No abstract available at this time...
Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950
Donald Mraz
1952, Transactions of the American Fisheries Society (81) 150-161
To obtain information on the post-spawning movements of yellow perch that spawn in southern Green Bay, Lake Michigan, 4,172 fish caught in drop nets were marked by tagging with monel-metal strap tags attached to the right operculum and 24,799 were marked by clipping off the second or membranous dorsal...
Ground water in the Litchville area, Barnes County, North Dakota
P.D. Akin
1952, North Dakota Ground Water Studies 18
No abstract available....
Origin of the Mima Mounds, Thurston County region, Washington
R. C. Newcomb
1952, Journal of Geology (60) 461-472
There has been recent favorable consideration of the idea that the Mima mounds were made by gophers. The writer believes the evidence indicates that gophers function only in the reworking of the mound material, not in the primary construction. The plausibility of the earlier glacial or periglacial theory has been...
Chemical quality of the surface waters in the Saline River Basin, Kansas, a progress report
W. H. Durum
1951, Report
Ground-water resources of Chase County [Kansas]
H.G. O’Connor
1951, Kansas Geological Survey Bulletin (11) 28-49
Geology and ground-water resources of Lane County, Kansas
G.C. Prescott Jr.
1951, Kansas Geological Survey Bulletin (93)