
The Pequannock River corridor serves as the primary artery through this Highland landscape, where the New York Susquehanna and Western RR parallels its course through Newfoundland. The 1954 culture revision reveals a region defined by its significant water infrastructure, featuring the Canistear Reservoir, Clinton Reservoir, and Echo Lake. These water bodies are flanked by the steep ridges of Bearfort Mountain and Kanouse Mountain, which constrained settlement to the valleys and plateaus.
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6 editions found
1888 · Franklin
USGS Topo · 1:62,500
1888 · Morristown
USGS Topo · 1:62,500
1888 · Lake Hopatcong
USGS Topo · 1:62,500
1891 · Greenwood Lake
USGS Topo · 1:62,500
1893 · Greenwood Lake
USGS Topo · 1:62,500
1894 · Morristown
USGS Topo · 1:62,500
1894 · Lake Hopatcong
USGS Topo · 1:62,500
1894 · Franklin
USGS Topo · 1:62,500
1897 · Franklin
USGS Topo · 1:62,500
1898 · Lake Hopatcong
USGS Topo · 1:62,500