C. M. Bunker, H.C. Hamontre
1959, Bulletin 1052-G
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Publication Extents
Not all publications have extents, not all extents are completely accurateR.F. Carter
1959, Open-File Report 59-17
No abstract available....
I.G. Grossman
1959, Open-File Report 59-45
L.L. Laine
1959, Open-File Report 59-76
The estimated runoff from the Illinois River basin of 1,660 square miles has averaged 1,160,000 acre-feet per year during the water years 1938-56, equivalent to an average annual runoff depth of 13.1 inches. About 47 percent of the streamflow is contributed from drainage in Arkansas, where an average of 550,000...
Clyde P. Ross
1959, Professional Paper 296
This report summarizes available data on two adjacent and partly overlapping regions in northwestern Montana. The first of these is Glacier National Park plus small areas east and west of the park. The second is here called, for convenience, the Flathead region; it embraces the mountains from the southern tip...
L.C. Dutcher
1959, Open-File Report 59-135
F. N. Houser, F. G. Poole
1959, Open-File Report 59-68
John Isbister
1959, Open-File Report 59-69
Luna Bergere Leopold
1959, Circular 410
The literature on probability techniques applicable to problems in hydrology is abundant but scattered through scientific journals of both hydrology and statistics. Important administrative and judicial decisions presently face water-compact commissions, courts, and water-planning committees. These and other groups might find useful, a brief and simplified discussion of how statistical...
A.V. Heyl Jr., A.F. Agnew, E.J. Lyons, C. H. Behre Jr.
1959, Open-File Report 59-53
Verl Richard Wilmarth, D.L. Healey, Alfred Clebsch Jr., I.J. Winograd, Isadore Zietz, H. W. Oliver
1959, Trace Elements Investigations 358
This report summarizes an interpretation of the geology of Yucca Valley to depths of about 2,300 feet below the surface, the characteristics features of ground water in Yucca and Frenchman Valleys, and the seismic, gravity, and magnetic data for these valleys. Compilation of data, preparation of illustrations, and writing of...
William C. Peterson
1959, Open-File Report 59-134
This report is the eighth in a continuing series of progress reports giving the results of discharge measurements made at selected springs and streams in the Tecolote Tunnel area of the Santa Ynez Mountains. The measurement program was begun on its present scale in the latter part of 1948 by...
Roland L. Wigley
1959, Fishery Bulletin of the U.S. Fish and Wildlife Service 561-617
A life history study of the sea lamprey, Petromyson marinus Linnaeus, in Cayuga Lake, N.Y., was conducted during 1950, 1951, and 1952. One of the major objectives was to obtain biological data concerning this endemic stock of sea lampreys for comparison with the newly established stocks in the Great Lakes....
John G. Connor, C.G. Mitchell
1958, Technical Publication 10
An accelerated use of water resulting from a growing population, industrial expansion, and irrigation has brought into focus the importance of the quality as well as the quantity of this natural resource in Utah. As new demands are made on the existing supply, a search goes on for new sources...
J.B. DeWitt
1958, Arborist's News (24) 25-29
Brief, factual review of information on effect of DDT and other insecticides on birds. One program for control of elm disease caused 22% decrease in number of adult birds and 56% mortality of nestlings. Quail fed 3 oz. of DDT per ton of food had 16% reduction in young...
E. L. Atwood
1958, Biometrics (14) 132-146
Response bias errors are studied by comparing questionnaire responses from waterfowl hunters using four large public hunting areas with actual hunting data from these areas during two hunting seasons. To the extent that the data permit, the sources of the error in the responses were studied and the contribution...
Raymond L. Nace, Arthur Van’t Hul, I.S. McQueen
1958, Water Supply Paper 1463
Many springs and seeps discharge water from the north wall of the valley of the Snake River between Milner and Bliss, Idaho. These are fed by a large ground-water body lying east and north of the river, beneath the Snake River Plain. Much ground water is pumped on the plain, many irrigation wells...
Sulo Werner Wiitala, Karl R. Jetter, Alan J. Sommerville
1958, Open-File Report 58-109
The valid incentives compelling occupation of the flood plain, up to and even into the stream channel, undoubtedly have contributed greatly to the development of the country. But the result has been a heritage of flood disaster, suffering, and enormous costs.Flood destruction awakened a consciousness toward reduction and elimination of...
Harold Meisler
1958, Open-File Report 58-67
The investigation in the Bonanza Lake area of northwestern Power and southeastern Blaine Counties was made to determine the direction of ground-water movement and to ascertain the relation of the regional ground-water body to the Snake River. The surface of the area is nearly flat to gently rolling, and slopes...
J. S. Bader, W. R. Moyle Jr.
1958, Open-File Report 58-7
Warren S. Daniels, Malcolm D. Hale
1958, Water Supply Paper 1370-B
The floods of October 9-11, 1954 in the Chicago area of Illinois and Indiana were the greatest in the history of the region. The 24-hour rainfall of 5.63 inches on October 9-10 and the 48-hour total rainfall of 6.72 inches were the greatest recorded at the Chicago Weather Bureau station...
J. S. Bader, R. W. Page, L.C. Dutcher
1958, Open-File Report 58-8
Robert S. Sigafoos
1958, Bulletin 1061-E
F. M. Robinson, H. R. Bergquist
1958, Professional Paper 305-E
No abstract available....
Elwood R. Leeson
1958, Open-File Report 58-62
Through its Water Resources Division, the United States Geological Survey has become the major water-resources historian for the nation. The Geological Survey's collection of streamflow records in Kansas began on a very small scale in 1895 in response to some early irrigation interest, Since that time the program has grown,...