
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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1925 · Gainesboro
USGS Topo · 1:62,500
1928 · Gordonsville
USGS Topo · 1:62,500
1929 · Gainesboro
USGS Topo · 1:62,500
1932 · Carthage
USGS Topo · 1:62,500
1942 · Statesville
USGS Topo · 1:100,000
1943 · Cookeville
USGS Topo · 1:100,000
1944 · Cookeville
USGS Topo · 1:100,000
1955 · Baxter
USGS Topo · 1:24,000
1956 · Silver Point
USGS Topo · 1:24,000
1956 · Corbin
USGS Topo · 1:250,000