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Ground water in alluvial deposits in Oklahoma

January 1, 1951

Alluvium along main streams in Oklahoma has long been recognized as a generally dependable aquifer. Pumping tests made in recent years afford a means of comparing one area with another. They indicate coefficients of transmissibility on the order of 70,000 gallons per day per foot in the Arkansas River alluvium near Fort Gibson, and 60,000 in the North Canadian River alluvium near Oklahoma City and El Reno.

Publication Year 1951
Title Ground water in alluvial deposits in Oklahoma
DOI 10.2113/gsecongeo.46.1.76
Authors S.L. Schoff, E.W. Reed
Publication Type Article
Publication Subtype Journal Article
Series Title Economic Geology
Index ID 70221630
Record Source USGS Publications Warehouse