
The Susquehanna River dominates this landscape at the end of the nineteenth century, serving as a primary corridor for transportation and settlement between Snyder, Northumberland, and Dauphin counties. The eastern bank is heavily influenced by the industrial infrastructure of the Northern Central RR and the Summit Branch RR, which connected the river towns to the interior coal regions. Parallel to the river, the remnant of the Pennsylvania Canal is visible near McKee Half Falls and Liverpool, tracing a path that predates the rail dominance. The topography is defined by the sharp, linear ridges of Berrys Mountain and Mahantango Mountain, which hem in valleys where farming communities like Elizabethville and Berrysburg are situated. Large river islands such as Hoover Id. and Zeigler Id. underscore the river's dynamic nature before modern controls altered the Susquehanna's traditional flow and navigation patterns.
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7 editions found
1892 · Lykens
USGS Topo · 1:62,500
1892 · Hummelstown
USGS Topo · 1:62,500
1892 · Shamokin
USGS Topo · 1:62,500
1892 · Harrisburg
USGS Topo · 1:62,500
1893 · Sunbury
USGS Topo · 1:62,500
1893 · Lykens
USGS Topo · 1:62,500
1893 · Shamokin
USGS Topo · 1:62,500
1893 · Millersburg
USGS Topo · 1:62,500
1899 · Harrisburg
USGS Topo · 1:62,500
1907 · New Bloomfield
USGS Topo · 1:62,500