Abstract

and Neosho River Valley, Kansas' WILLIAM J. SEEVERS and WILLIAM L. JUNGMANN In southeastern Kansas, in the area bounded to the west by the Flint Hills and to the north by the Marais des Cygnes drainage basin, Neogene terraces in the valleys of the Neosho and Marais des Cygnes Rivers have been studied in great detail (Fig. 1). Along both valleys, remnants of alluvial terrace deposits of Illinoisan and Kansan ages and a complex of alluvial gravel deposits ranging from pre-Kansan to Pliocene (?) occur in step-like progression above the Recent flood plain. Sedi-

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