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165309 results.

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Page 6078, results 151926 - 151950

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Floods in Pennsylvania, frequency and magnitude
W. F. Busch, E.C. Shaw
1961, Open-File Report 61-28
This report outlines a method of determining the magnitude of floods having frequencies up to 50 years for any stream in Pennsylvania except regulated streams and streams whose drainage basins are smaller than 10 square miles. On the main stems of the Schuylkill, Delaware, Susquehanna, and Chemung Rivers the magnitude...
Floods in Wisconsin: Magnitude and frequency
D.W. Ericson
1961, Open-File Report 61-44
Flood data from gaging stations on Wisconsin rivers and streams are listed in this report. From these data, composite frequency curves were defined which express the ratio of floods of various recurrence intervals to the mean annual flood. Multiple correlation techniques were used to obtain formulas that relate the basin...
Data on wells at Ladd Air Force Base, Alaska
Alvin J. Feulner
1961, Open-File Report 61-50
Ladd Air Force Base, in central Alaska, obtains its water supply from wells. A tabulation of 104 wells gives available data on depth, diameter, yield, and depth of permafrost encountered. Also given are 23 well logs and 21 chemical analyses of well waters and treated waters from Ladd Air Force...
Ground water in the alluvium of Beaver Creek basin, Oklahoma
D.L. Hart Jr.
1961, Open-File Report 61-59
Beaver Creek is an 857 square-mile area in south-central Oklahoma. The tributaries head at an altitude as high as 1,400 feet and the mouth of Beaver Creek is at an altitude of 804 feet. Alluvial material has been deposited along all the major streams in the basin. The alluvium contains...
Ground water in the alluvium of Elk Creek basin, Oklahoma
J.R. Hollowell
1961, Open-File Report 61-65
Elk Creek basin comprises 584 square miles in Washita, Beckman, and Kiowa Counties. The basin is typical of southwestern Oklahoma with nearly level plains broken by gentle rolling hills and low escarpments, except for the extreme southern part, where seven granite and gabbroic knobs and ridges of the Wichita Mountains...
Ground water in the vicinity of Roosevelt, Oklahoma
J.R. Hollowell
1961, Open-File Report 61-67
The principal source of additional ground-water supply in the Roosevelt area of west-central Kiowa County is from alluvial deposits. Ground water can be obtained in varying amounts from the red beds of Permian age, but yields of wells are small and the water is of poor quality at most places. Roosevelt's...