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Page 5223, results 130551 - 130575

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Flood investigations in Nevada through 1977 water year
Otto Moosburner
1978, Open-File Report 78-610
Maximum annual discharges, gage heights, and probable flood dates for 127 sites are compiled for Nevada streams. Data have been collected in cooperation with the Nevada Department of Highways at most of the sites (108).Also included in the report are the peak discharges, gage heights, and flood dates for the...
Two-dimensional and three-dimensional digital flow models of the Salinas Valley ground-water basin, California
T. J. Durbin, G.W. Kapple, J. R. Freckleton
1978, Water-Resources Investigations Report 78-113
The Salinas Valley ground-water basin is in central coastal California. The ground-water basin extends from Monterey Bay southeastward along the Salinas River to San Ardo, a distance of about 70 miles, and has a maximum thickness of about 2,000 feet. Annual recharge to the ground-water basin, which is derived mostly...
Stratigraphic test well, Nantucket Island, Massachusetts
David W. Folger, J.C. Hathaway, R. A. Christopher, P. C. Valentine, C. W. Poag
1978, Circular 773
The U.S. Geological Survey, in cooperation with the Massachusetts Water Resources Commission and the Nantucket Conservation Foundation, continuously cored 514 m of sediment and volcanic rock in a stratigraphic and water-quality test near the geographic center of Nantucket Island. Stratified sediments were divided texturally into three zones: the upper zone...
Pillar Mountain Landslide, Kodiak, Alaska
Reuben Kachadoorian, Willard H. Slater
1978, Open-File Report 78-217
Pillar Mountain landslide on the southeast face of Pillar Mountain is about 915 m (3,000 ft) southwest of the city of Kodiak, Alaska. The landslide is about 520 m (1,700 ft) wide at its base and extends approximately from sea level to an altitude of about 343 m (1,125 ft)....
Low-flow and flow duration of Tennessee streams
Robert L. Gold
1978, Open-File Report 78-807
Low-flow frequency and duration data are presented to define variations of the low flow of Tennessee streams both in time and place. Analysis has been made of 204 continuous record stations, both regulated and unregulated and 651 partial-record stations operated either by the U.S. Geological Survey or Tennessee Valley Authority...
Geologic map of the New Windsor Quadrangle, Carroll County, Maryland
G.W. Fisher
1978, IMAP 1037
The pattern of rock units in the geologic map of the New Windsor quadrangle has been affected by three distinguishable generations of folds; following the usage of Tobisch and Fleuty (1969) and Higgins (1973), the fold generations are named for localities where they are well displayed....