Floods of November and December 1965 in southern California
E. R. Hedman, E.G. Pearson
1966, Open-File Report 66-61
Severe flooding occurred in southern California in late November and late December 1965 as a result of three heavy storms. Rain occurred on most days during the period November 13-26 and December 28-31, with major amounts distributed in three periods: November 13-19, 21-26, and December 28-31. More than 12 inches...
Flood-frequency of streams in Jackson, Mississippi
K. V. Wilson
1966, Open-File Report 66-155
Effect of treated effluent diversion on Yahara River flow, Wisconsin
K.B. Young
1966, Open-File Report 66-157
Before December 1958 the treated sewage effluent from the Madison, Wisconsin, metropolitan area was discharged into the Yahara River at the north end of Lake Waubesa, which is upstream from the USGS gaging station on the Yahara River near McFarland, Wis. Since December 1958 the effluent has been diverted southward...
Waterpower resources and reconnaissance geology of sites in the Alsea River basin, Oregon
Loyd L. Young, D. W. Neal, David L. Gaskill
1966, Water Supply Paper 1610-D
No abstract available....
Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan
Carl E. Dutton, H. L. James, R. W. Johnson Jr., K. L. Wier
1966, Open-File Report 66-37
No abstract available. ...
Precambrian geology of Florence SE quadrangle, Florence County, Wisconsin
Carl E. Dutton
1966, Open-File Report 66-35
No abstract available....
Effects of agricultural conservation practices on the hydrology of Corey Creek basin, Pennsylvania, 1954-60
Benjamin L. Jones
1966, Water Supply Paper 1532-C
Analyses of data collected from two small basins in northern Pennsylvania during the period May 1954 to September 1960 indicated that changes in land use and land treatment have affected suspended- sediment discharge from the basins. Extensive land use and land-treatment changes have taken place in the 12.2-square-mile Corey Creek...
Ground-water development in the high plains of Colorado, with a section on chemical quality of the ground water
Arnold J. Boettcher, Robert Brennan
1966, Water Supply Paper 1819-I
The High Plains of Colorado includes all or part of 11 counties and has an area of about 9,500 square miles. The land surface slopes eastward and in most areas is gently rolling owing to erosion by ephemeral streams. The Ogallala Formation, of Pliocene age, is the principal aquifer. In...
Delaware water
William Charles Rasmussen, John W. Odell, Norman Howard Beamer
1966, Water Supply Paper 1767
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
World distribution of soil, rock, and vegetation
J.M. Goldberg, F.R. Fosberg, Marie-Helene Sachet, Allen Reimer
1966, Open-File Report 66-50
Extent and frequency of floods on Delaware River in vicinity of Belvidere, New Jersey
George M. Farlekas
1966, Open-File Report 66-43
A stream overflowing its banks is a natural phenomenon. This natural phenomenon of flooding has occurred on the Delaware River in the past and will occur in the future. T' o resulting inundation of large areas can cause property damage, business losses and possible loss of life, and may result...
The future for water in the Wolf River region, Wisconsin
C. L. R. Holt Jr.
1966, Open-File Report 66-62
Ground-water inventory for 1965, Edwards Air Force Base, California
F. W. Giessner, J.A. Westphal
1966, Open-File Report 66-49
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...
Ground water in the Cimarron River basin: New Mexico, Colorado, Kansas, and Oklahoma
Water Resources Division, U.S. Geological Survey
1966, Open-File Report 66-159
This report on ground water in the Cimarron River basin was prepared by the Water Resources Division of the U.S. Geological Survey at the request of the U.S. Corps of Engineers, Tulsa District, for inclusion in the Corps' overall report on the water resources of the basin. The report is...
Geologic evaluation of radar imagery, Caliente and Temblor Ranges, southern California
Edward W. Wolfe
1966, Open-File Report 69-321
Rapid modal analysis of some felsic rocks from calibrated X-ray diffraction patterns
Donald Bruce Tatlock
1966, Bulletin 1209
Surficial geology of the Athol quadrangle, Worcester and Franklin Counties, Massachusetts
Donald F. Eschman
1966, Bulletin 1163-C
Geology of the Adam Weiss Peak quadrangle, Hot Springs and Park Counties, Wyoming
Willis L. Rohrer
1966, Bulletin 1241-A
Water resources of the Ipswich River basin, Massachusetts
Edward A. Sammel, John Augustus Baker, Richard A. Brackley
1966, Water Supply Paper 1826
Water resources of the Ipswich River basin are at resent {1960) used principally for municipal supply to about 379,000 person's in 16 towns and cities in or near the river basin. By the year 2000 municipal use of water in this region will probably be more than twice the current...
Borden Formation (Mississippian) in south- and southeast-central Kentucky
Gordon Whitney Weir, James Louis Gualtieri, Seymour O. Schlanger
1966, Bulletin 1224-F
No abstract available....
Outcrop/geologic maps of the Nuka-Etivluk region, northern Alaska
I.L. Tailleur, B.H. Kent Jr., H. N. Reiser
1966, Open-File Report 66-128
Water resources of the Big Stone Lake Watershed, West-central Minnesota
R. D. Cotter, L. E. Bidwell, E.L. Oakes, G.H. Hollenstein
1966, Hydrologic Atlas 213
No abstract available....
Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska
Samuel J. Tuthill, Wilson M. Laird
1966, Professional Paper 543-B
The Alaska earthquake of March 27, 1964, caused widespread geomorphic changes in the Martin-Bering Rivers area-900 square miles of uninhabited mountains, alluvial flatlands, and marshes north of the Gulf of Alaska, and east of the Copper River. This area is at lat 60°30’ N. and long 144°22’ W., 32 miles...
