
The Cumberland Escarpment defines the dramatic transition between the high plateau of Walden Ridge and the lower Tennessee Valley. This landscape is marked by steep ravines and waterfalls, most notably Stinging Fork Falls and the headwaters of the Piney River. Small settlements such as Pennine and Milo sit near the edges of these topographical shifts, while the town of Spring City occupies the more level terrain to the east.
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This is the sole edition of this map. No revisions or reprints were ever made.
1887 · Kingston
USGS Topo · 1:125,000
1891 · Kingston
USGS Topo · 1:125,000
1892 · Pikeville
USGS Topo · 1:125,000
1893 · Kingston
USGS Topo · 1:125,000
1895 · Pikeville
USGS Topo · 1:125,000
1909 · Sequatchie Valley
USGS Topo · 1:62,500
1910 · Pikeville
USGS Topo · 1:62,500
1912 · Crossville
USGS Topo · 1:62,500
1935 · Melvine
USGS Topo · 1:24,000
1935 · Morgan Springs
USGS Topo · 1:24,000