
Cumberland Plateau heights drop sharply into the Sequatchie Valley on this study of the Tennessee landscape. The physical geography is dominated by the Tennessee Valley Divide, which separates the drainage systems of the region, while gaps like Billingsley Gap and Rankins Gap provide natural passages through the escarpment. Settlement patterns follow the valley floor and the plateau summits, with small communities such as Cold Spring and Mount Crest established near reliable water sources and agricultural land.
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1892 · Pikeville
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
1935 · Brockdell
USGS Topo · 1:24,000
1935 · Billingsley Gap
USGS Topo · 1:24,000
1935 · Vandever
USGS Topo · 1:24,000