William A. Fischer, Dan A. Davis, Theresa M. Sousa
1966, Hydrologic Atlas 218
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Publication Extents
Not all publications have extents, not all extents are completely accurateC.D. Albert, G.J. Stramel
1966, Water Supply Paper 1798-B
Characteristics and transport of sediment in the Little Arkansas River basin in south-central Kansas were studied to determine if the water from the river could be used as a supplemental source for municipal supply or would provide adequate recharge to aquifers that are sources of municipal and agricultural water supplies....
Harry Hulsing, Winchell Smith, Ernest D. Cobb
1966, Water Supply Paper 1869-C
Donald L. Coffin, Edward J. Jenkins
1966, Open-File Report 66-15
R. H. Dale, James J. French, G. V. Gordon
1966, Open-File Report 66-21
The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the 700,000 acre-feet per year flow of...
Harry H. Barnes, Harold G. Golden
1966, Water Supply Paper 1674
No abstract available....
F. W. Giessner, S. G. Robson
1966, Open-File Report 66-48
J.F. Turner Jr.
1966, Professional Paper 272-G
The mass-transfer and water-budget techniques of calibrating a reservoir for evaporation were evaluated through a study of Lake Michie, N.C. The techniques appear adequate for estimation of lake evaporation and net seepage in humid regions where lake storage is affected by streamflow and ground-water seepage, under conditions no more adverse...
John R. Dyni
1966, Open-File Report 66-38
No abstract available....
James L. Patterson, William P. Somers
1966, Water Supply Paper 1683
This report outlines methods by which the magnitude and frequency of expected floods of any recurrence interval from 1.1 to 50 years can be determined at most points in the Colorado River basin.Composite frequency curves were drawn showing the relation of the mean annual flood to floods having recurrence intervals...
E. H. Cordes, J. R. Wall, Joe A. Moreland
1966, Open-File Report 66-19
J. R. Dyni
1966, Oil and Gas Investigation Map 216
No abstract available....
Robert H. Tschudy
1966, Open-File Report 66-132
Harlan H. Schwob
1966, Open-File Report 67-196
Highway engineers and many others use flood stages and discharges in the design of bridges and other structures or operations on the flood plain of a stream. These data are provided in the form of gaging-station and other flood records and as flood profiles. Flood-frequency data are used to compute...
Gerald Meyer, Granville G. Wyrick
1966, Circular 533
Between the towns of Macon and Taylorville in central Illinois lies a ridge that is part of a system of ridges and knolls largely composed of sand and gravel. This ridge contains an important aquifer. An extensive electrical earth resistivity survey was conducted over the ridged-drift aquifer. Inversion of the...
P. W. Philbin, C. W. Smith
1966, Geophysical Investigations Map 594
No abstract available....
Arnold Leslie Brokaw, John Rodgers, D. F. Kent, Robert A. Laurence, C. H. Behre Jr.
1966, Bulletin 1222-C
No abstract available....
Thomas Seward Lovering
1966, Bulletin 1222-F
Bureau Of Sport Fisheries And Wildlife, University Of Alaska
1966, Resource Publication 16
No abstract available....
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...
N.J. Lusczynski, Wolfgang V. Swarzenski
1966, Water Supply Paper 1613-F
Test drilling, extraction of water from cores, electric logging, water sampling, and water-level measurements from 1958 to 1961 provided a suitable basis for a substantial refinement in the definition of the positions, chloride concentrations, and rates of movement of salty water in the intermediate and deep deposits of southern Nassau...
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...
K. V. Wilson
1966, Open-File Report 66-155
George L. Snyder
1966, Open-File Report 66-126
No abstract available....
William Charles Rasmussen, John W. Odell, Norman Howard Beamer
1966, Water Supply Paper 1767