
The Piscataquis River corridor serves as the primary artery through this Central Maine landscape, connecting industrial and rail hubs during the early 1930s. The Bangor and Piscataquis River and Moosehead Lake RR meets the Maine Central RR at Monson Junction, reflecting a period when rail transport was vital to the local economy. In Guilford and Sangerville, the concentration of structures near the riverbanks highlights the historical importance of water power and bridge crossings like Lows Bridge.
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5 editions found
1913 · Skowhegan
USGS Topo · 1:62,500
1930 · Pittsfield
USGS Topo · 1:48,000
1931 · Stetson
USGS Topo · 1:48,000
1932 · Dover-Foxcroft
USGS Topo · 1:48,000
1932 · Pittsfield
USGS Topo · 1:62,500
1933 · Pittsfield
USGS Topo · 1:62,500
1933 · Guilford
USGS Topo · 1:62,500
1935 · Dover-Foxcroft
USGS Topo · 1:62,500
1935 · Stetson
USGS Topo · 1:62,500
1937 · Guilford
USGS Topo · 1:62,500