
The Keowee River and Seneca River define the hydraulic character of this late 19th-century landscape, which was surveyed by C.M. Yeates in the mid-1880s. The region is marked by a transition from the mountainous heights of Rocky Bald Mt. and Cedar Rock Mt. in the north to the industrializing corridors of the Richmond and Danville Railroad in the south. This era captures the area before modern inundation, showing historic river crossings like Cherry Ferry, Shallow Ford, and Ravenee Bridge in their original contexts.
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