
The Ozark plateau along the Current River is a landscape defined by its karst geology and timber history in the late 1940s. Natural landmarks such as Round Spring Caverns, Pulltite Spr, and Whaley Cave Spr highlight a topography rich in subterranean drainage and massive spring-fed systems. The presence of the Shannondale Fire Tower and various mills, including Falk Mill and Mansers Mill, reflects an economy tied to the forest and the river long before modern development transformed these hills.
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1915 · Eminence
USGS Topo · 1:62,500
1917 · Eminence
USGS Topo · 1:62,500
1928 · Cardareva
USGS Topo · 1:62,500
1932 · Cedar Grove
USGS Topo · 1:48,000
1941 · Salem
USGS Topo · 1:62,500
1941 · Stone Hill
USGS Topo · 1:62,500
1943 · Boss
USGS Topo · 1:62,500
1944 · Corridon
USGS Topo · 1:62,500
1945 · Salem
USGS Topo · 1:62,500
1945 · Stone Hill
USGS Topo · 1:62,500