
Johns Creek snakes through the heart of this Appalachian landscape, serving as the primary drainage for a dense network of hollows and branches in the mid-1950s. The settlement of Thomas and its Thomas PO anchor the valley, while smaller communities like McCombs, Gulnare, and Jackson are tucked along the tributary waters of Brushy Fork and Sycamore Creek. This era reveals a localized rural infrastructure of education and faith, evidenced by the distribution of the Wolf Creek Sch, Banyan Sch, and the Freewill Ch. The terrain is characterized by steep ridges such as Spring Knob and Chestnut Knob, which separate the various forks of the watershed. Notable industrial activity is indicated by a heavy concentration of gas and oil wells throughout the hills, reflecting the region's mid-century energy production. Much of the lower valley land along the main creek is identified as subject to inundation from the Dewey Reservoir spillway.
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3 editions found
1886 · Prestonsburg
USGS Topo · 1:125,000
1887 · Warfield
USGS Topo · 1:125,000
1891 · Warfield
USGS Topo · 1:125,000
1892 · Prestonsburg
USGS Topo · 1:125,000
1910 · Naugatuck
USGS Topo · 1:48,000
1912 · Naugatuck
USGS Topo · 1:62,500
1914 · Laynesville
USGS Topo · 1:48,000
1914 · Inez
USGS Topo · 1:48,000
1915 · Williamson
USGS Topo · 1:48,000
1915 · Naugatuck
USGS Topo · 1:48,000