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Where the "deep stage" is crossed by the Mississinewa moraine, the maximum thickness of drift is 410 feet.
The present course of the Wabash River originated in late Tazewell time.
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The Eel River valley train occupies an interlobate position, and the Wabash Valley bears evidence of its roles as a sluiceway and as an outlet for glacial Lake Maumee in late Cary time.
Three topographic areas comprise the upland part of Wabash County: the Tipton till plain, the Mississinewa terminal moraine, and the Packerton interlobate moraine.
Marl is restricted to the area of the Packerton moraine.
Sand and gravel occur in the Packerton moraine, in abundance along the Eel and Mississinewa valley trains, and along the Wabash and Salamonie Valleys where they cross preglacial and interglacial valleys.
Buried valleys, particularly the Teays and Eel, contain large potential supplies of ground water.