J.R. Randolph, Ruth G. Deike
1966, Water Supply Paper 1863
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Page 2526, results 63126 - 63150
Publication Extents
Not all publications have extents, not all extents are completely accurateN.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...
Philip J. Carpenter, David H. Appel
1966, Open-File Report 67-37
This investigation was undertaken as a part of the cooperative program with the Iowa Institute of Hydraulic Research, the City of Des Moines, and the U.S. Geological Survey. The purpose of this report is twofold: 1. To present water-surface profiles and rating curves for existing channel conditions in the 4-mile reach...
Fred Kunkel, Walter Hofman
1966, Open-File Report 66-75
Ladies and gentlemen, it is a pleasure to be invited to attend this Irrigation Institute conference and to describe the Geological Survey's program of ground-water studies in the San Joaquin Valley. The U.S. Geological Survey has been making water-resources studies in cooperation with the State of California and other agencies...
R. E. Evenson
1966, Open-File Report 66-42
Hydrologic data collected during the climatically near-average 6-year period of inventory 1957-62 provide the basis for making estimates of supply to and demand from the Lompoc subarea of the Santa Ynez River basin and changes in the quantity of water stored in the deposits of the basin. The hydrologic inventory...
W.H. Espey Jr.
1966, Open-File Report 66-41
No abstract available....
Morris Deutsch, J.C. Wallace
1966, Open-File Report 66-23
William B. Bull
1966, Open-File Report 66-13
Near-surface subsidence results chiefly from the compaction of deposits by an overburden load as the clay bond supporting the deposits is weakened by water percolating through the deposits for the first time since burial. About 100 square miles of alluvial-fan deposits in western Fresno County, California, have been affected by...
William Charles Rasmussen, John W. Odell, Norman Howard Beamer
1966, Water Supply Paper 1767
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...
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...
Frederick H. Ruggles Jr.
1966, Open-File Report 66-119
The first streamflow station in Texas was established on the Rio Grande at El Paso on May 10, 1889. Sip,ce that time the systematic collection of streamflow data. has expanded. In 1915 the Texas Board of Water Engineers (now the Texas Water Development Board) entered into a cooperative agreement with...
Harold E. McGovern, Edward D. Jenkins
1966, Hydrologic Atlas 236
R.N. Doolittle
1966, Open-File Report 66-26
Frederick H. Ruggles
1966, Hydrologic Atlas 240
This report presents hydrologic data that enable the user to define areas susceptible to flooding and to evaluate the flood hazard along Bachman Branch and Joes Creek. The data provide a technical basis for making sound decisions concerning the use of flood-plain lands. The report will be useful for preparing...
Water Resources Division, U.S. Geological Survey
1966, Bulletin 1232
William J. Shampine, Leslie J. Crain, Richard C. Shipley, James B. Hood Jr.
1966, Open-File Report 66-122
This report contains a tabulation of data collection sites established by the U.S. Geological Survey in the Western Oswego River basin. Information on the types of data collected at each site is also provided. Statistical summaries are furnished for selected stream-gaging stations in the form of duration, flood frequency, and low-flow...
S. G. Robson
1966, Open-File Report 66-114
P. R. Speer, M. S. Hines, M.E. Janson, H. G. Jeffery
1966, Professional Paper 448-F
No abstract available....
T. William Lambert
1966, Hydrologic Atlas 165
No abstract available....
R. W. Davis
1966, Hydrologic Atlas 169
Water Resources Division, U.S. Geological Survey
1966, IMAP 489
Harold A. Whitcomb, T. Ray Cummings, Richard A. McCullough
1966, Water Supply Paper 1806
Northern and central Johnson County, Wyo., is an area of about 2,600 square miles that lies principally in the western part of the Powder River structural basin but also includes the east flank of the Bighorn Mountains. Sedimentary rocks exposed range in age from Cambrian to Recent and have an...
Henry A. Hansen (compiler), Mildred R. Hudgins
1966, Special Scientific Report - Wildlife 99
Water Resources Division, U.S. Geological Survey
1966, Water Data Report MN-65-1-2