
The Caney Fork and Smith Fork Creek converge in this dissected plateau region, where the intricate network of hollows and ridges dictates the placement of long-standing rural communities. Settlements like Chestnut Mound and Buffalo Valley are positioned along high ground and valley floors, connected by a winding road system that follows the natural topography of places such as Opossum Valley and Ditty Hollow. The northern boundary is defined by the expansive Cordell Hull Reservoir, which transformed the local drainage patterns of Hurricane Cr and Martin Cr.
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