
The Ohio River flows along the northwestern edge of this Kentucky-Illinois borderland, defining a landscape where river bottomlands meet the rising topography of the Dyer Hills. In the early 1950s, the region's rural character is marked by a network of small churches that served as local anchors, including Zion Ch, Spring Grove Ch, and Mt Olive Ch. The Illinois Central railroad cuts through the southern terrain, connecting the settlement at Grove Center to the wider region. Systematic drainage is evident through the Goose Pond Ditch, which reclaimed land near the riverbank. Scattered Oil Wells across the eastern hills point to the era's active resource extraction, while landmarks like The Rocks and Bald Hill provide distinct navigational points above the river's normal pool elevation.
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1905 · New Haven
USGS Topo · 1:62,500
1906 · New Haven
USGS Topo · 1:62,500
1907 · Morganfield
USGS Topo · 1:62,500
1916 · Shawneetown
USGS Topo · 1:62,500
1917 · Uniontown
USGS Topo · 1:62,500
1949 · Paducah
USGS Topo · 1:250,000
1949 · New Haven
USGS Topo · 1:62,500
1949 · Morganfield
USGS Topo · 1:24,000
1950 · Paducah
USGS Topo · 1:250,000
1951 · Sturgis
USGS Topo · 1:24,000