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The Project Gutenberg EBook of Fishes of the Wakarusa River in Kansas, by James E. Deacon and Artie L. Metcalf This eBook is for the use of anyone anywhere at no cost and with almost no restrictions whatsoever. You may copy it, give it away or re-use it under the terms of the Project Gutenberg License included with this eBook or online at www.gutenberg.net Title: Fishes of the Wakarusa River in Kansas Author: James E. Deacon Artie L. Metcalf Release Date: March 5, 2010 [EBook #31513] Language: English Character set encoding: ASCII *** START OF THIS PROJECT GUTENBERG EBOOK FISHES--WAKARUSA RIVER--KANSAS *** Produced by Chris Curnow, Joseph Cooper and the Online Distributed Proofreading Team at http://www.pgdp.net UNIVERSITY OF KANSAS PUBLICATIONS MUSEUM OF NATURAL HISTORY Volume 13, No. 6, pp. 309-322, 1 fig. February 10, 1961 Fishes of the Wakarusa River in Kansas BY JAMES E. DEACON AND ARTIE L. METCALF (Contribution from The State Biological Survey, and from the Department of Zoology of The University of Kansas) UNIVERSITY OF KANSAS LAWRENCE 1961 UNIVERSITY OF KANSAS PUBLICATIONS, MUSEUM OF NATURAL HISTORY Editors: E. Raymond Hall, Chairman, Henry S. Fitch, Robert W. Wilson Vol. 13, No. 6, pp. 309-322, 1 fig. Published February 10, 1961 UNIVERSITY OF KANSAS Lawrence, Kansas PRINTED IN THE STATE PRINTING PLANT TOPEKA, KANSAS 1961 28-5872 Fishes of the Wakarusa River in Kansas BY JAMES E. DEACON AND ARTIE L. METCALF (Contribution from The State Biological Survey, and The Department of Zoology of The University of Kansas) _Introduction_ The Wakarusa River rises in the eastern edge of the Flint Hills and flows approximately 50 miles in an easterly direction and empties into the Kansas River near Eudora; with its tributaries, the Wakarusa drains 458 square miles in parts of Wabaunsee, Shawnee, Osage, and Douglas counties of northeastern Kansas (Fig. 1). The average gradient is 6.3 feet per mile. Turbidity is consistently more than 100 ppm in the lower portions of the mainstream and major tributaries, but is usually lower in the upper portions of tributaries. The channel of the mainstream is intrenched in its own alluvium (Dufford, 1958:36) and has high, muddy banks and mud- or sand-bottom; the upper parts of tributaries have lower banks and bottoms of gravel, rubble, or bedrock, although a few (
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