Arizona Water
John William Harshbarger, D.D. Lewis, H.E. Skibitzke, W. L. Heckler, L. R. Kister, H. L. Revised by Baldwin
1966, Water Supply Paper 1648
Ground-water conditions during 1965, South Vandenberg area, Vandenberg Air Force Base, California
S. G. Robson, F.W. Glessner
1966, Open-File Report 66-115
Induced recharge of an artesian glacial-drift aquifer at Kalamazoo, Michigan
J.E. Reed, Morris Deutsch, S.W. Wiitala
1966, Water Supply Paper 1594-D
As part of a program for managing its ground-water supply, the city of Kalamazoo has constructed induced-recharge facilities at the sites of several of its well fields. To determine the benefits of induced recharge in a water-management program, the U.S. Geological Survey, in cooperation with the city, conducted a series...
Selected X-ray crystallographic data, molar volumes, and densities of minerals and related substances
R. A. Robie, P. M. Bethke, Keith Beardsley
1966, Open-File Report 66-113
Chemistry of the lavas of the 1959-60 eruption of Kilauea Volcano, Hawaii
K. J. Murata, D.H. Richter
1966, Professional Paper 537-A
Geologic map of the Mt. Harvard quadrangle, Gunnison and Chaffee Counties, Colorado
M. R. Brock, Fred Barker
1966, Open-File Report 66-9
World distribution of soil, rock, and vegetation
J.M. Goldberg, F.R. Fosberg, Marie-Helene Sachet, Allen Reimer
1966, Open-File Report 66-50
Coking-coal deposits of the western United States
Paul Averitt
1966, Bulletin 1222-G
Paleozoic formations in the Wind River Basin, Wyoming
W. R. Keefer, J. A. Van Lieu
1966, Professional Paper 495-B
Progress report on proposed ground-water studies in the Lytle Creek-San Sevaine area, Upper Santa Ana Valley, California, 1965
J.J. French
1966, Open-File Report 66-44
The future for water in the Wolf River region, Wisconsin
C. L. R. Holt Jr.
1966, Open-File Report 66-62
Plant microfossils from the Fort Union Formation
Robert H. Tschudy, Sharon D. Van Loenen
1966, Open-File Report 66-133
As a part of continuing studies to provide palynological data from critical sequences for comparative biostratigraphic studies, the microfossils found in two Paleocene samples have been examined and photographed....
Contour of bedrock surface, Boone to Fowler, Colorado
R. Theodore Hurr, J.E. Moore, David B. Richards
1966, Open-File Report 66-66
Pilot hole of the University of New Mexico water well no. 7
J.B. Cooper
1966, Open-File Report 66-18
Geologic map of the Deadhorse Flat quadrangle, Nye County, Nevada
Donald C. Noble, Richard D. Krushensky, E. J. McKay, John R. Ege
1966, Trace Elements Investigations 866
Floods in Steger Quadrangle, Northeastern Illinois
Howard E. Allen
1966, Hydrologic Atlas 209
Terrestrial impact structures - a bibliography
Jacquelyn H. Freeberg
1966, Bulletin 1220
Stratigraphic names in the New London area, Connecticut
Richard Goldsmith
1966, Bulletin 1224-J
Geohydrology of Saline County, Nebraska
Philip A. Emery
1966, Hydrologic Atlas 216
Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee
Arnold Leslie Brokaw, John Rodgers, D. F. Kent, Robert A. Laurence, C. H. Behre Jr.
1966, Bulletin 1222-C
No abstract available....
Fur catch in the United States, 1965.
Division Of Wildlife Research
1966, Wildlife Leaflet 474
Paleozoic Gastropoda from the Moose River synclinorium, northern Maine
A. J. Boucot, E. L. Yochelson
1966, Professional Paper 503-A
Base of fresh ground water in southern Oklahoma
D.L. Hart
1966, Hydrologic Atlas 223
Magnitude and frequency of floods in the United States: Part 10. The Great Basin
E. Butler, J.K. Reid, V.K. Berwick
1966, Water Supply Paper 1684
The probable magnitude of floods of any recurrence interval between 1.1 and 50 years for any stream in the Great Basin can be determined by methods presented in this report.The Great Basin comprises nearly all of Nevada, western Utah, eastern California, and parts of Idaho, Oregon, and Wyoming. The physiography...
Channel and hillslope processes in a semiarid area, New Mexico
Luna Bergere Leopold, William W. Emmett, Robert M. Myrick
1966, Professional Paper 352-G
Ephemeral washes having drainage areas from a few acres to 5 square miles are shown by actual measurement to be accumulating sediment on the streambed. This aggradation is not apparent to the eye but is clearly shown in 7 years of annual remeasurement.A similar aggradation was in progress in the...