R.S. McQuivey
1967, Open-File Report 67-154
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Publication Extents
Not all publications have extents, not all extents are completely accurateR. K. Blankennagel
1967, Open-File Report 67-18
This report describes the testing techniques used by the U. S. Geological Survey to obtain hydrologic data in deep holes drilled in volcanic rocks at Pahute Mesa, Nevada Test Site. The testing program in each hole includes geophysical logging, pumping, and injecting and swabbing between straddle packers. Rock lithologies and...
Norman G. Bailey
1967, Open-File Report 67-7
When the Apollo astronauts land on the Moon, their precise location will not be known. The real-time geologic mapping planned for the first mission could best be done if the exact position of the landing site were determined. The astronauts may have to find their position, with or without assistance...
R. L. Knutilla
1967, Open-File Report 67-135
No abstract available....
D.M. Culbertson, L. E. Young, J.C. Brice
1967, Open-File Report 68-68
D.W. Moody, F.L. Shaefer
1967, Open-File Report 67-160
This report presents information on station-type activities for acquiring surface-water, ground-water, and quality of water data in the Delaware River basin. The information was collected in 1966 through field offices of the Water Resources Division, U.S. Geological Survey as part of a pilot study for the Office of Water Data...
M. G. Bonilla
1967, Open-File Report 67-23
This report summarizes geometric aspects of approximately 35 instances of historic faulting of the ground surface in the continental United States and adjacent parts of Mexico. This information is of immediate importance in the selection and evaluation of sites for vital structures such as nuclear power plants. The data are...
R. D. Carroll, D.L. Coffin, J. R. Ege, F.A. Welder
1967, Open-File Report 67-38
Analysis of geologic, hydrologic , and geophysical data obtained in and around Yellow Creek core hole No. 1, Rio Blanco County, Colorado, indicate a 1,615-foot section of oil shale was penetrated by the hole. Geophysical log data indicate the presence of 25 gallons per ton shale for a thickness of...
F.E. Clarke, Ivan Barnes
1967, Open-File Report 67-45
R.W. Clement
1967, Open-File Report 67-46
D.E. Click, B. N. Aldridge
1967, Open-File Report 67-47
Alberto Condes de la Torre
1967, Open-File Report 67-66
J.J. Cook
1967, Open-File Report 67-67
W.P. Cross
1967, Open-File Report 67-69
E. G. Crosthwaite
1967, Open-File Report 67-70
E.J. Crosthwaite, M.J. Mundorff, E.H. Walker
1967, Open-File Report 67-71
The lower Henrys Fork region includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River in eastern Idaho. The northwestern and western parts of the area are part of the Snake River lava plain. The central part of the area is occupied by...
R.V. Cushman
1967, Open-File Report 67-72
D. L. Daniels
1967, Open-File Report 67-73
D. L. Daniels
1967, Open-File Report 67-74
Walter Danilchik
1967, Open-File Report 67-75
M. E. Davis
1967, Open-File Report 67-78
No abstract available....
M. E. Davis, E. R. Leggat
1967, Open-File Report 67-79
The Hueco Bolson, as defined in this report, is in the extreme western part of Texas and includes that part of El Paso County between the Franklin and Hueco Mountains north of the Rio Grande....
G.C. Doty
1967, Open-File Report 67-84
Bernard Dunn
1967, Open-File Report 67-85
J. R. Ege
1967, Open-File Report 67-86
Analysis of oil assays, structure sections, and isopach maps of the Parachute Creek Member of the Green River Formation indicates that numerous locations in the western part of the Piceance Creek basin could be selected with an oil shale section at least 500 feet thick that contains not less than...