M. S. Bedinger, C. G. Stone, D.R. Albin, M. S. Hines, J.H. Hubble
1966, Open-File Report 66-4
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Publication Extents
Not all publications have extents, not all extents are completely accurateL.M. MacCary, R. W. Davis
1966, Hydrologic Atlas 166
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...
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...
T. William Lambert
1966, Hydrologic Atlas 173
A. E. Scheidegger, W. B. Langbein
1966, Professional Paper 500-C
John S. Havens
1966, Water Supply Paper 1819-F
The area described in this report is that part of the southern High Plains principally within northern Lea County, N. Mex. ; it comprises about 1,400,000 acres. Hydrologic boundaries isolate the main aquifer of the area, the Ogallala Formation, from outside sources of natural recharge other than precipitation on the...
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...
C.J. Robinove
1966, Open-File Report 67-189
J.R. Randolph, Ruth G. Deike
1966, Water Supply Paper 1863
1966, Water Supply Paper 1822
Increasing world activity in water-resources development has created an interest in techniques for conducting investigations in the field. In the United States, the Geological Survey has the responsibility for extensive and intensive hydrologic studies, and the Survey places considerable emphasis on discovering better ways to carry out its responsibility. For...
Frank Walter Kennon
1966, Water Supply Paper 1839-C
Charles Butler Hunt, T. W. Robinson, W.A. Bowles, A.L. Washburn
1966, Professional Paper 494-B
No abstract available....
John Henry Frederick Feth, D.A. Barker, L.G. Moore, Randy J. Brown, C.E. Veirs
1966, Professional Paper 518
A cooperative investigation to determine the geology of the Weber Delta district, with emphasis on the occurrence and chemical quality of ground water, was made by the U.S. Geological Survey and the U.S. Bureau of Reclamation with the later assistance of the Utah State Engineer in the final preparation of...
Ralph C. Heath, B. L. Foxworthy, Philip M. Cohen
1966, Circular 524
Ground-water development on Long Island has followed a pattern that has reflected changing population trends, attendant changes in the use and disposal of water, and the response of the hydrologic system to these changes. The historic pattern of development has ranged from individually owned shallow wells tapping glacial deposits to...
Harry H. Tanaka, Jerrald R. Hollowell, John Joseph Murphy
1966, Water Supply Paper 1809-T
Edwin Allen Bell
1966, Water Supply Paper 1819-C
Water problems and their solutions have been associated with the growth and development of the Louisville area for more than a century. Many hydrologic data that aided water users in the past can be applied to present water problems and will be helpful for solving many similar problems in the...
A. G. Hely, G.H. Hughes, Burdge Irelan
1966, Professional Paper 486-C
D. E. Burkham
1966, Water Supply Paper 1831
The collection of runoff and sediment data was the primary objective of the 10-year (1951-60) study in the Cornfield Wash basin, which has an area of 21.3 square miles. However, reconnaissance investigations also were made of (1) precipitation; (2) the effects of reservoirs on runoff, erosion, and sediment yield; (3)...
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...
Wallace De Laguna
1966, Bulletin 1156-E
Richmond F. Brown
1966, Water Supply Paper 1837
The Mammoth Cave National Park in central Kentucky offers a unique opportunity to study the occurrence of ground water in limestone under natural conditions. Ground water occurs as perched and semiperched bodies in alternate sandstone, shale, and limestone formations and under water-table conditions at the approximate level of the Green...
John T. Gallaher, William Evans Price
1966, Water Supply Paper 1818
Luiz Goncalves Chada Filho, Mario Dias Pessoa, William C. Sinclair
1966, Water Supply Paper 1663-E
The upper Capibaribe basin is the western three-fourths, approximately, of the valley of the river that empties into the Atlantic Ocean at Recife, the capital of the State of Pernambuco, Brazil. It is the part of the drainage basin that is within the Drought Polygon of northeast Brazil, and it...
Allen W. Noehre, Roman T. Mycyk
1966, Hydrologic Atlas 145