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Page 6063, results 151551 - 151575

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Gravity survey in the western Snake River Plain, Idaho-a progress report
David P. Hill, Jimmy J. Jacobson
1961, Open-File Report 61-63
From June 24 through August 16, 1960, a regional gravity survey was made in 3,600 square miles of the Snake River Plain in southwestern Idaho. Six hundred and seventy-two gravity stations were established between latitudes 42?30N and 43?30N and between longitudes 115?15W and 116?15W at an average density of one...
Potential water power of Lake Chakachamna, Alaska
Bruce Lawellin Jackson
1961, Open-File Report 61-74
Lake Chakachamna, in view of its area, altitude, and location on a region of high precipitation and runoff, has a large potential power value. The outflow from the lake, based on limited streamflow records varies from less than 60 cfs to well over 15,000 cfs, with an annual flow in...
Geology of the Huntsville quadrangle, Alabama
T.H. Sanford Jr., G.T. Malmberg, L.R. West
1961, IMAP 329
The 7 1/2-minute Huntsville quadrangle is in south-central Madison County, Ala., and includes part of the city of Hunstville. The south, north, east, and west boundaries of the quadrangle are about 3 miles north of the Tennessee River, 15 1/2 miles south of the Tennessee line, 8 miles west of...
Geochemistry of the Frenchy Incline uranium deposit, San Miguel County, Colorado
Alfred T. Miesch
1961, Open-File Report 61-98
The Frenchy Incline uranium deposit is in the Salt Wash member of the Morrison formation, on the central part of the Colorado Plateau, and consists of sandstone and mudstone that have been impregnated with uranium and vanadium minerals in addition to other constituents. The compositions of the deposit and its...
Geology and mineral deposits of the Carlile quadrangle, Crook County, Wyoming
M.H. Bergendahl, R. E. Davis, G. A. Izett
1961, Bulletin 1082-J
The Carlile quadrangle-is along the northwestern flank of the Black Hills uplift in Crook County, Wyo. The area-is primarily one of canyons and divides that are a result of downcutting by the Belle Fourche River and its tributaries through an alternating succession of sandstone, siltstone, and mudstone or shale beds....