Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin
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...
Delaware water
William Charles Rasmussen, John W. Odell, Norman Howard Beamer
1966, Water Supply Paper 1767
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...
Sedimentation in Brownell Creek subwatershed No. 1, Nebraska
J. C. Mundorff
1966, Water Supply Paper 1798-C
Water-quality characteristics of New Jersey streams
Peter W. Anderson, John R. George
1966, Water Supply Paper 1819-G
No abstract available....
Record low tide of December 31, 1962 on the Delaware River
A.C. Lendo
1966, Water Supply Paper 1586-E
Bibliography of hydrology of the United States 1963
J.R. Randolph, Ruth G. Deike
1966, Water Supply Paper 1863
Laboratory study of aquifer properties and well design for an Artificial-Recharge site
A.I. Johnson, R.P. Moston, S.F. Versaw
1966, Water Supply Paper 1615-H
The occurrence, chemical quality and use of ground water in the Tabulbah area, Tunisia
L.C. Dutcher, H. E. Thomas
1966, Water Supply Paper 1757-E
Sedimentation and chemical quality of surface water in the Heart River drainage basin, North Dakota
Marion L. Maderak
1966, Water Supply Paper 1823
The Heart River drainage basin of southwestern North Dakota comprises an area of 3,365 square miles and lies within the Missouri Plateau of the Great Plains province. Streamflow of the Heart River and its tributaries during 1949-58 was directly proportional to .the drainage area. After the construction of Heart Butte...
Free-surface instability correlations, and Roughness-concentration effects on flow over hydrodynamically rough surfaces
Herman John Koloseus, Jacob Davidian
1966, Water Supply Paper 1592-C,D
Ground-water resources of Sheridan County, Wyoming
Marlin E. Lowry, T. Ray Cummings
1966, Water Supply Paper 1807
Sheridan County is in the north-central part of Wyoming and is an area of about 2,500 square miles. The western part of the county is in the Bighorn Mountains, and the eastern part is in the Powder River structural basin. Principal streams are the Powder and Tongue Rivers, which are...
Magnitude and frequency of floods in the United States; part 2-B. South Atlantic slope and Eastern Gulf of Mexico basins, Ogeechee River to Pearl River
Harry H. Barnes, Harold G. Golden
1966, Water Supply Paper 1674
No abstract available....
Reconnaissance of the geology and ground-water resources in the Aurora area, St. Louis county, Minnesota
Robert W. Maclay
1966, Water Supply Paper 1809-U
The Aurora area is a glaciated upland of drift-mantled slopes, channels, swamps, and glacial-lake plains. It covers about 24 square miles of the eastern part of the Mesabi Iron Range in northeastern Minnesota. A deep narrow channel along the Embarrass River, the principal outlet of a former large glacial lake...
Water resources of Fort Huachuca Military Reservation, southeastern Arizona
S. G. Brown, E. S. Davidson, L. R. Kister, B. W. Thomsen
1966, Water Supply Paper 1819-D
The Fort Huachuca Military Reservation, on the northeast flank of the Huachuca Mountains, is in the southern part of the San Pedro River drainage in the Basin and Range physiographic province in Arizona. The main sources of water available in the reservation area are ground water stored in two unconsolidated...
Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin
Water Resources Division, U.S. Geological Survey
1966, Water Supply Paper 1645
Salt-water encroachment in southern Nassau and southeastern Queens Counties, Long Island, New York
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...
Hydrology of the cavernous limestones of the Mammoth Cave area, Kentucky
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...
Gunpowder Falls, Maryland : uses of a water resource today and tomorrow
Deric O’Bryan, Russell Lonnie McAvoy
1966, Water Supply Paper 1815
Hydrology of the alluvial deposits in the Ohio River valley in Kentucky
John T. Gallaher, William Evans Price
1966, Water Supply Paper 1818
Organic acids in naturally colored surface waters
William L. Lamar, D.F. Goerlitz
1966, Water Supply Paper 1817-A
Most of the organic matter in naturally colored surface waters consists of a mixture of carboxylic acids or salts of these acids. Many of the acids color the water yellow to brown; however, not all of the acids are colored. These acids range from simple to complex, but predominantly they...
Water in the Humboldt River Valley near Winnemucca, Nevada
Philip M. Cohen
1966, Water Supply Paper 1816
Most of the work of the interagency Humboldt River Research Project in the Winnemucca reach of the Humboldt River valley has been completed. More than a dozen State and Federal agencies and several private organizations and individuals participated in the study. The major objective of the project, which began in...
Ground-water resources of the Dayton area, Ohio
Stanley Eugene Norris, Andrew Maute Spieker
1966, Water Supply Paper 1808
The principal aquifers of the Dayton area are sand and gravel layers in the 150- to 250-foot thick glacial deposits filling the river valleys (Miami River and its tributaries), which were originally cut in bedrock by preglacial streams. The upper and lower aquifers are separated by a poorly permeable till-rich...
Salinity of the ground water in western Pinal County, Arizona
Lester Ray Kister, W. F. Hardt
1966, Water Supply Paper 1819-E
The chemical quality of the ground water in western Pinal County is nonuniform areally and stratigraphically. The main areas of highly mineralized water are near Casa Grande and near Coolidge. Striking differences have been noted in the quality of water from different depths in the same well. Water from one...
Hydrology of the Upper Capibaribe Basin, Pernambuco, Brazil - A reconnaissance in an Area of Crystalline Rocks
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...
