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Publication Extents

Not all publications have extents, not all extents are completely accurate
Floods in Oklahoma: magnitude and frequency
A.O. Westfall, J.L. Patterson
1964, Open-File Report 64-170
This report presents methods by which the magnitude and frequency of expected floods for most streams in Oklahoma can be determined. Flood data were used to define flood-frequency curves applicable to the State. Composite frequency curves were drawn showing the relation of mean annual floods to floods having recurrence intervals...
Ground-water geology of the Dickson, Lawrenceburg, and Waverly areas in the western Highland Rim, Tennessee
Melvin V. Marcher, Roy H. Bingham, Richard Edwin Lounsbury
1964, Water Supply Paper 1764
Ground-water supplies in the Dickson, Lawrenceburg, and Waverly areas are obtained from wells and springs in limestone and chert formations of Missisippian age. In the Dickson area most of the wells and springs are in Warsaw Limestone. In the Lawrenceburg and Waverly areas, ground-water supplies are obtained from Fort Payne...
Evaluation of hydrogeology and hydrogeochemistry of Truckee Meadows area, Washoe County, Nevada
Philip M. Cohen, Omar J. Loeltz
1964, Water Supply Paper 1779-S
Practically all the ground water of economic importance in the Truckee Meadows area, an alluviated intermontane basin in western Nevada is in the valley fill, which consists of unconsolidated and partially consolidated sedimentary deposits. The Mesozoic and Cenozoic consolidated rocks of the mountains bordering the valley contain some water in...
Chemical quality of surface waters in the Brazos River basin in Texas
Burdge Irelan, H.B. Mendieta
1964, Water Supply Paper 1779-K
The Brazos River basin, which makes up 15 percent of the land area of Texas, extends from the High Plains, where altitudes reach 4,200 feet and the average precipitation ranges from 15 to 20 inches a year, to the Gulf of Mexico where the annual rainfall is 45-^50 inches. Large...