
The Cumberland Plateau in the late nineteenth century is characterized by a network of high-elevation settlements and critical gaps through the ridge lines. Pikeville serves as a primary valley hub, while the Nashville Chattanooga and St. Louis R. R. pushes through the hills to reach coal and timber resources near Bon Air. Local industry and community life are evidenced by Hale Mill on the creeks and Sequatchie College to the south. Distinctive landmarks such as the Rock House near Sparta and the Eastland Stand indicate the importance of established waypoints along the plateau trails. The landscape is defined by its difficult passages, including Stevens Gap and Morris Gap, which dictated the flow of trade and travel between the Caney Fork and the valley floor.
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7 editions found
1886 · Cleveland
USGS Topo · 1:125,000
1887 · Kingston
USGS Topo · 1:125,000
1888 · Chattanooga
USGS Topo · 1:125,000
1891 · Kingston
USGS Topo · 1:125,000
1892 · Pikeville
USGS Topo · 1:125,000
1892 · Cleveland
USGS Topo · 1:125,000
1893 · Mc Minnville
USGS Topo · 1:125,000
1893 · Chattanooga
USGS Topo · 1:125,000
1893 · Kingston
USGS Topo · 1:125,000
1895 · Cleveland
USGS Topo · 1:125,000