The Whitewater River valley running north-south through eastern Indiana and southwestern Ohio was created by the Late Wisconsin Glaciation ending 13,600 years ago. Fayette County was at the southern fringe of the glaciation at that time. The Ice Age was punctuated by several prolonged warm periods during which the glaciers disappeared entirely from the temperate latitudes and a climate similar to modern times or even warmer prevailed. The flood waters produced resulted in lakes; breaching of the lakes resulted in rivers and streams carving its hills and valleys.
The Whitewater River valley running north-south through eastern Indiana and southwestern Ohio was created by the Late Wisconsin Glaciation ending 13,600 years ago Fayette County was at the southern fringe of the glaciation at that time. The Ice Age was punctuated by several prolonged warm periods during which the glaciers disappeared entirely from the temperate latitudes and a climate similar to modern times or even warmer prevailed. The flood waters produced resulted in lakes; breaching of the lakes resulted in rivers .and streams carving its hills and valleys.