Time, distance, and drawdown relationships in a pumped ground-water basin
Fred Kunkel
1960, Circular 433
Several reasonable values are assumed for coefficients of transmissibility and storage of lenticular alluvial deposits, These values when substituted in the Theis (1935) nonequilibrium formula as modified by Wenzel (1942) give curves from which time, distance, drawdown relationships are estimated....
Geologic interpretation of magnetic data in the Copper River basin, Alaska
Gordon E. Andreasen, Arthur Grantz, Isidore Zietz
1960, Open-File Report 60-10
The Mesaverde group at Sunnyside, Utah
Harold Brodsky
1960, Open-File Report 60-18
The Mesaverde group of Late Cretaceous age at Sunnyside, Utah consists in ascending order; the Blackhawk formation, Castlegate sandstone and the Price River formation. The Mancos shale inter-tongues with the Blackhawk formation.The Mancos shale formed in an offshore marine environment, the Blackhawk formation formed in a mixed marine and continental...
Preliminary geologic map of the Deep Lake quadrangle, Stevens and Pend Orielle Counties, Washington
R. G. Yates, A.E. Ford
1960, Miscellaneous Field Studies Map 237
Total intensity aeromagnetic profiles of the Cape Lisburne area, Alaska
Gordon E. Andreasen
1960, Open-File Report 60-6
No abstract available....
Total intensity aeromagnetic profiles of the Kobuk River area, Alaska
Gordon E. Andreasen
1960, Open-File Report 60-7
No abstract available....
Engineering geology of the Katalla area, Alaska
Reuben Kachadoorian
1960, IMAP 308
Corals from well cores of Madison group, Williston basin
William Jasper Sando
1960, Bulletin 1071-F
Gravity survey in part of the Snake River Plain, Idaho — A preliminary report
Harry L. Baldwin Jr., David P. Hill
1960, Open-File Report 60-11
During the early summer of 1959, a total of 1,187 gravity stations were occupied on the western part of the Snake River plain in Idaho. An area of 2,000 square miles extending from Glenns Ferry, Idaho, to Caldwell, Idaho, was covered with a station density of one station per two...
Generalized geologic map of the Nelchina area, Alaska, showing igneous rocks and larger faults
Arthur Grantz
1960, IMAP 312
Total intensity aeromagnetic profiles of Cape Espenberg, Alaska
Gordon E. Andreasen
1960, Open-File Report 60-5
No abstract available....
Total intensity aeromagnetic profiles of the Yukon Flats-Kandik area, Alaska
Gordon E. Andreasen
1960, Open-File Report 60-9
Total intensity aeromagnetic profiles of the Minchumina area, Alaska
Gordon E. Andreasen
1960, Open-File Report 60-8
No abstract available....
Springs: their origin, development, and protection
G.H. Taylor
1960, Open-File Report 60-140
This paper has been prepared to describe springs briefly, to give some suggestions about developing and protecting them, and to list selected reports and books that contain more detailed explanations of springs and that describe how to develop and protect them from contamination....
Petrography of radioactive Tertiary igneous rocks, Front Range mineral belt, Colorado
John David Wells
1960, Bulletin 1032-E
No abstract available....
Geology and ground water in the Platte-Republican Rivers watershed and the Little Blue River basin above Angus, Nebraska, with a section on chemical quality of the ground water
C. R. Johnson, Robert Brennan
1960, Water Supply Paper 1489
This report describes an area of about 7,300 square miles in south-central Nebraska. Approximately one-fourth of the area, largely at its east end, consists of an undissected southeastward-sloping upland plain and is almost wholly irrigable; the remainder is in various stages of dissection and only parts of it are suitable...
Surface water supply of Hawaii, 1955-56
J. V. B. Wells
1960, Water Supply Paper 1449
Geologic and alteration maps of the East Tintic district, Utah
T. S. Lovering
1960, Miscellaneous Field Studies Map 230
No abstract available....
Preliminary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana
Everett D. Jackson
1960, Open-File Report 60-79
This paper presents some results of work done between 1951 and 1955 as a part of a comprehensive investigation of the stratigraphy, geochemistry, and petrography of the Ultramafic zone of the Stillwater complex by the U. S. Geological Survey. Detailed mapping of the chromite deposits of the complex was done...
Surface water supply of Hawaii, 1956-58
J. V. B. Wells
1960, Water Supply Paper 1569
Geochemical and heavy-mineral reconnaissance of the Concord quadrangle, Cabarrus County, North Carolina
Henry Bell, W.C. Overstreet
1960, Miscellaneous Field Studies Map 234
Origin and chemical composition of evaporite deposits
George William Moore
1960, Open-File Report 60-99
A comparative study of marine evaporite deposits forming at the present time along the pacific coast of central Mexico and evaporite formations of Permian age in West Texas Basin was made in order to determine if the modern sediments provide a basis for understanding environmental conditions that existed during deposition...
Experimental drill hole logging in potash deposits of the Carlsbad district, New Mexico
C.L. Jones, C. Gilbert Bowles, Kenneth Granville Bell
1960, Open-File Report 60-84
Experimental logging of holes drilled through potash deposits in the Carlsbad district, southeastern New Mexico, demonstrate the considerable utility of gamma-ray, neutron, and electrical resistivity logging in the search for and identification of mineable deposits of sylvite and langbeinite. Such deposits are strongly radioactive with both gamma-ray and neutron well...
Geology and ore deposits of the Klondike Ridge area, Colorado
John David Vogel
1960, Open-File Report 60-145
The region described in this report is in the northeastern part of the Colorado Plateau and is transitional between two major structural elements. The western part is typical of the salt anticline region of the Plateau, but the eastern part has features which reflect movements in the nearby San Juan...
Surface water supply of the United States, 1959, Part 9, Colorado River Basin
J. V. B. Wells
1960, Water Supply Paper 1633
