Geology and thorium-bearing deposits of the Lemhi Pass area, Lemhi County, Idaho, and Beaverhead County, Montana
William N. Sharp, Wayne S. Cavender
1962, Bulletin 1126
Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources
Sam H. Patterson, John W. Hosterman, John Warfield Huddle
1962, Bulletin 1122-F
The Haldeman and Wrigley 7th-minute quadrangles are near the western edge of the eastern Kentucky coal field and cover an area of approximately 117 square miles in parts of Carter, Rowan, Elliott, and Morgan Counties, Ky. The rocks exposed in the two quadrangles are of Early and Late Mississippian and...
Geology of the Littleton quadrangle, Jefferson, Douglas, and Arapahoe counties, Colorado
Glenn R. Scott
1962, Bulletin 1121-L
Geology of the magnesite belt of Stevens County, Washington
Ian Campbell, John S. Loofbourow Jr.
1962, Bulletin 1142-F
Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky
Robert Denny Trace
1962, Bulletin 1122-E
The fault systems of the Levias-Keystone and Dike-Eaton areas, in the Kentucky-Illinois fiuorspar district, are a complex northeastward-trending sys- tem and a simple northwestward-trending system of steeply dipping normal faults, associated in part with a lamprophyre dike. Fluorspar mining started in the area about 1900 and, as of 1945, more...
Uranium occurrences in sedimentary rocks of Pennsylvania
Harry Klemic
1962, Bulletin 1107-D
No abstract available....
Uranium and other trace elements in Devonian and Mississippian black shales in the central midcontinent area
Edwin R. Landis
1962, Bulletin 1107-E
No abstract available....
Flow-duration and high- and low-flow tables for California streams
Winchell Smith, C.F. Hains
1962, Open-File Report 62-128
Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho
E. G. Crosthwaite
1962, Open-File Report 62-34
This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury...
Geologic reconnaissance and test-well drilling at proposed Air Force facility, near Lompoc, California
G.A. Miller, R. E. Evenson
1962, Open-File Report 62-85
Relation of surface and ground water in the Souris River Valley near Minot, North Dakota
Edward Bradley
1962, Open-File Report 62-10
Ground-water reconnaissance in Round Valley, Custer County, Idaho
E. G. Crosthwaite
1962, Open-File Report 62-33
Round Valley in central Idaho contains alluvial deposits of Pleistocene and Recent age which yield adequate supplies of ground water for stock and domestic wells. The alluvial deposits are underlain by Challis Volcanics of Oligocene or Early Miocene age and a few wells obtain domestic and stock water from the...
Water levels in observation wells in Santa Barbara County, California, in 1961
K. S. Muir
1962, Open-File Report 62-91
Investigation of the ground-water resources of Santa Barbara County was continued during 1961 by the U. S. Geological Survey in cooperation with the Santa Barbara County Water Agency. Monthly water-level measurements were made in 190 wells, in 9 of which automatic water-level recorders were operated. Earlier measurements, covering the period...
Floods on St. Vrain and Lefthand Creeks at Longmont, Colorado
C.T. Jenkins
1962, Open-File Report 63-53
No abstract available....
Oxidized zinc deposits of the United States: Part 1. General geology
A. V. Heyl, C. N. Bozion
1962, Bulletin 1135-A
No abstract available....
Surface water of Beaver Creek Basin, in South-Central Oklahoma
L.L. Laine, J.J. Murphy
1962, Open-File Report 62-162
Annual discharge from Beaver Creek basin is estimated to have averaged 217,000 acre-feet during a 19-year base period, water years 1938-56, equivalent to an average annual runoff depth of 4.7 inches over the 857 square-mile drainage area. About 55,000 acre-feet per year comes from Little Beaver Creek basin, a tributary...
Geophysical methods of exploring for buried channels in the Monument Valley area, Arizona and Utah
R.A. Black, F.C. Frischknecht, R. M. Hazlewood, W. H. Jackson
1962, Bulletin 1083-F
Preliminary geologic map of the Unionville quadrangle, Nevada
R. E. Wallace, D.B. Tatlock, Norman J. Silberling, W. P. Irwin
1962, Miscellaneous Field Studies Map 245
Geologic and hydrologic aspects of test-well drilling
Phillip W. Johnson, Natalie D. White, Harry G. Page
1962, Open-File Report 62-161
Bentonite deposits of the northern Black Hills district, Wyoming, Montana, and South Dakota
Maxwell M. Knechtel, Sam H. Patterson
1962, Bulletin 1082-M
The northern Black Hills bentonite mining district includes parts of Crook County, Wyo., Carter County, Mont., and Butte County, S. Dak. Within this district, many beds of bentonite occur interspersed with sedimentary strata of Cretaceous age that have an average total thickness of about 3,000 feet and consist chiefly of...
Preliminary geologic map of the Elk Park quadrangle, Jefferson and Silver Bow Counties, Montana
H.W. Smedes, M. R. Klepper, D. M. Pinckney, G.E. Becraft, E. T. Ruppel
1962, Miscellaneous Field Studies Map 246
Geologic and structure map of the Minnekahta NE quadrangle, Fall River and Custer Counties, South Dakota
D.E. Wolcott, C.G. Bowles, D.A. Brobst, E.V. Post
1962, Miscellaneous Field Studies Map 242
No abstract available....
Preliminary geologic map and sections of the Wheeler Peak quadrangle, White Pine County, Nevada
D. H. Whitebread, A.B. Gribbs, W.B. Rogers, J. W. Mytton
1962, Miscellaneous Field Studies Map 244
Geology of the Frenchie Creek quadrangle, north-central Nevada
L.J. Patrick Muffler
1962, Open-File Report 62-90
Relation between ground water and surface water in Brandywine Creek basin, Pennsylvania
F. H. Olmsted, A. G. Hely
1962, Professional Paper 417-A
The relation between ground water and surface water was studied in Brandywine Creek basin, an area of 287 square miles in the Piedmont physiographic province in southeastern Pennsylvania. Most of the basin is underlain by crystalline rocks that yield only small to moderate supplies of water to wells, but the...