Distribution of the Middle Ordovician Copenhagen formation and its trilobites in Nevada
Reuben James Ross Jr., Frederick C. Shaw
1972, Professional Paper 749
Mesozoic stratigraphy of the Patagonia Mountains and adjoining areas, Santa Cruz County, Arizona
Frank S. Simons
1972, Professional Paper 658-E
Ground-Water Hydraulics
Stanley William Lohman
1972, Professional Paper 708
A Lagrangian method of predicting pollutant dispersion in Bolinas Lagoon, Marin County, California
Hugo B. Fischer
1972, Professional Paper 582-B
Stratigraphy, morphology, and paleoecology of a fossil peccary herd from western Kentucky
Warren Irvin Finch, Frank C. Whitmore Jr., John D. Sims
1972, Professional Paper 790
Geochemical anomalies and alteration in the Moenkopi Formation, Skull Creek, Moffat County, Colorado
Robert Allen Cadigan
1972, Professional Paper 761
Fossils from the Ordovician bioherm at Meiklejohn Peak, Nevada
Reuben James Ross Jr.
1972, Professional Paper 685
Mineral resource evaluation of the U.S. Forest Service Sierra Demonstration Project area, Sierra National Forest, California
John P. Lockwood, Paul Charles Bateman, John Samuel Sullivan
1972, Professional Paper 714
No abstract available....
The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data
Jack James Rowe, George Washington Morey, C.S. Zen
1972, Professional Paper 741
Stratigraphy and ammonite fauna of the Graneros Shale and Greenhorn Limestone near Pueblo, Colorado
William Aubrey Cobban, G. R. Scott
1972, Professional Paper 645
No abstract available....
Sedimentary petrology and paleocurrents of the Harebell Formation, Pinyon Conglomerate, and associated coarse clastic deposits, northwestern Wyoming
David A. Lindsey
1972, Professional Paper 734-B
Soil-moisture and energy relationships associated with riparian vegetation near San Carlos, Arizona
Irel S. McQueen, Reuben Frederick Miller
1972, Professional Paper 655-E
Geology and ground-water characteristics of the Hanford Reservation of the U.S. Atomic Energy Commission, Washington
Reuben Clair Newcomb, J.R. Strand, F. J. Frank
1972, Professional Paper 717
Availability of water in Kalamazoo County, southwestern Michigan
William Burrows Allen, John B. Miller, Warren W. Wood
1972, Water Supply Paper 1973
Kalamazoo County comprises an area of 572 square miles in the southwestern part of Michigan. It includes parts of the Kalamazoo, St. Joseph, and Paw Paw River basins, which drain into Lake Michigan. The northern two-thirds of the county is drained by the Kalamazoo River and its tributaries. A small...
Accuracy of low-flow characteristics estimated by correlation of base-flow measurements
Clayton H. Hardison, Marshall E. Moss
1972, Water Supply Paper 1542-B
Chemical quality of the water in the Tucson basin, Arizona
R. L. Laney
1972, Water Supply Paper 1939-D
The Tucson basin is a broad mountain-rimmed area of about 1,000 square miles in the Basin and Range physiographic province in southeastern Arizona. The altitude ranges from 2,000 feet in the basin to as much as 8,000 feat in the mountains. The major streams in the area are the Santa...
Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana
Joseph W. Lang
1972, Water Supply Paper 1899-M
Fresh water in abundance is contained in large artesian reservoirs in sand and gravel deposits of Tertiary and Quaternary ages in the Pearl River basin, a watershed of 8,760 square miles. Shallow, water-table reservoirs occur in Quarternary deposits (Pleistocene and Holocene) that blanket most of the uplands in .the southern...
The hydrology of four streams in western Washington as related to several Pacific salmon species
Michael R. Collings, Ronald W. Smith, G.T. Higgins
1972, Water Supply Paper 1968
Enhancement-or possibly even preservation-of the Pacific salmon hinges on the careful planning and proper management of the streamflow upon which they depend for spawning. Most spawning activity occurs on reaches of streams where specific hydraulic conditions exist and where stream-channel characteristics and water-quality criteria are met. The present report is...
Ground-water levels in the United States, 1966-70, Southwestern states
Water Resources Division, U.S. Geological Survey
1972, Water Supply Paper 2010
Geology and ground water of the Molalla-Salem slope area, northern Willamette Valley, Oregon
E. R. Hampton
1972, Water Supply Paper 1997
No abstract available....
Sediment transport in the western tributaries of the Sacramento River, California
Benjamin L. Jones, N.L. Hawley, John R. Crippen
1972, Water Supply Paper 1798-J
Measurement of salt-wedge excursion distance in the Duwamish River Estuary, Seattle, Washington, by means of the dissolved-oxygen gradient
William A. Dawson, L. J. Tilley
1972, Water Supply Paper 1873-D
The Duwamish River estuary has been the object of a series of comprehensive studies undertaken to predict the effects of the changing character of waste-water inputs on the water quality of the estuary. This report discusses the fresh- and salt-water relations of the estuary. The distance that the salt-water wedge...
Surface water supply of the United States, 1966-70, Part 14, Pacific Slope basins in Oregon and lower Columbia River basin
Water Resources Division, U.S. Geological Survey
1972, Water Supply Paper 2135
Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina
E. F. Hubbard, William G. Stamper
1972, Water Supply Paper 1873-E
This report presents the results of a fluorescent-dye-tracing study to determine the concentrations of a pollutant that would be present in the Northeast Cape Fear Estuary at various rates of continuous waste injection and freshwater inflow. Rhodamine WT dye was introduced into the estuary at a constant rate over a...
Geology and water resources of the Bitterroot Valley, southwestern Montana, with a section on chemical quality of water
R. G. McMurtrey, Richard L. Konizeski, M. V. Johnson, John H. Bartells, H. A. Swenson
1972, Water Supply Paper 1889
The Bitterroot Valley is a Late Cretaceous structural basin that was partly filled at its deepest point by more than 1,640 feet of Tertiary sediments. These sediments grade valleyward from coarse colluvial deposits along the edges of the valley to fine-grained deposits and then to coarse channel deposits of the...