
The remarkable limestone sinkhole of Grassy Cove dominates this Tennessee landscape, where the valley floor sits hundreds of feet below the surrounding peaks of Brady Mountain and Black Mountain. This geological karst feature is a self-contained basin where water drains into subterranean passages like Saltpeter Cave and Mill Cave rather than surface outlets. The 1946 field examination by the Tennessee Valley Authority records a network of rural life tied to these high-elevation valleys, including the small settlements of Alloway and Jewett.
85 named features on this map. Tap any name to fly to it.
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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 · Pennine
USGS Topo · 1:24,000