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Page 6005, results 150101 - 150125

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Surface waters of Elk Creek basin in southwestern Oklahoma
A.O. Westfall
1963, Open-File Report 63-138
The purpose of this study is to (1) determine the average discharge during a period that is representative of average streamflow conditions, (2) determine the range of discharge, and (3) determine the storage required to supplement natural flows during drought periods. Elk Creek drains 587 square miles of the North Fork...
Ground-water and related geology of Joshua Tree National Monument, California
J. E. Weir Jr., J. S. Bader
1963, Open-File Report 63-137
Joshua Tree National Monument is in a mountainous part of the desert region of southern California. The geographic center of the monument is about 130 miles east of Los Angeles, Calif.; the area Investigated, covering almost 1,000 square miles in area, is included between 115?20' and 116?28' west longitude, and...
Geology and ground-water features of salt springs, seeps, and plains in the Arkansas and Red River basins of western Oklahoma and adjacent parts of Kansas and Texas
P.E. Ward
1963, Open-File Report 63-132
The salt springs, seeps, and plains described in this report are in the Arkansas and Red River basins in western Oklahoma and adjacent areas in Kansas and Texas. The springs and seeps contribute significantly to the generally poor water quality of the rivers by bringing salt (NaCl) to the surface...
Reconnaissance geology and hydrology on the Nett Lake Indian Reservation, Minnesota
R.F. Norvitch
1963, Open-File Report 63-104
The Nett Lake Indian Reservation is in northern Minnesota, about 210 miles north of Minneapolis and St. Paul. The village of Nett Lake (population about 300) is the only community on the reservation. This report is the result of an investigation made to provide a central water source for the...
The hydrologic laboratory
A.I. Johnson
1963, Open-File Report 63-62
The knowledge of soil and rock testing, including the application of the test or analysis data to field problems, is still in its infancy. By learning more about the basic laws and principles of nature we can more accurately predict hydrologic phenomena of the future, as well as solve more...
Chemical character of streams in the Delaware River basin
Peter W. Anderson, Leo T. McCarthy Jr.
1963, Open-File Report 63-2
The water chemistry of streams in the Delaware River basin falls into eight general groups, when mapped according to the prevalent dissolved-solids content and the predominant ions normally found in the water. The approximate regions representing each of these iso-chemical quality groups are shown on the accompanying base map of the drainage basin....