
The Delaware River serves as the central artery of this region, carved by the natural flow of the Pequest River and Beaver Brook toward the county seat of Belvidere. This 1955 survey captures the transition from old rail corridors to modern transit, featuring the Conrail line and remnants like the Old RR Grade near Manunka Chunk. The topography is dominated by the steep slopes of Jenny Jump Mountain and Scotts Mountain, which define the settlement patterns in the valleys below.
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6 editions found
1888 · Hackettstown
USGS Topo · 1:62,500
1890 · Easton
USGS Topo · 1:62,500
1890 · High Bridge
USGS Topo · 1:62,500
1891 · Easton
USGS Topo · 1:62,500
1891 · Delaware Water Gap
USGS Topo · 1:62,500
1893 · Delaware Water Gap
USGS Topo · 1:62,500
1894 · Hackettstown
USGS Topo · 1:62,500
1898 · Hackettstown
USGS Topo · 1:62,500
1898 · High Bridge
USGS Topo · 1:62,500
1900 · Raritan
USGS Topo · 1:125,000