
Piscataquis River flows eastward through the heart of this landscape, serving as a corridor for the Bangor and Aroostook RR and anchoring the dual settlement of Dover-Foxcroft. In the early 1930s, this region was a network of small mill hamlets and rural school districts. The economy is visible through industrial sites like Dover South Mills, Atkinson Mills, and Rollins Mill, while higher education is represented by the Higgins Classical Institute in Charleston. Numerous small schoolhouses, such as Bear Hill Sch and Hathaway Sch, dot the countryside at nearly every major road intersection, or "corner." The transition from valley floors to elevations like The Pinnacle and Davis Hill reveals a pattern of dispersed upland farming, connected by early routes like State Highway No 100. This survey documents a precise moment when rail sidings like Starbirds Siding still supported local timber and agricultural transport before the full modernization of the state highway system.
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4 editions found
1902 · Bangor
USGS Topo · 1:62,500
1930 · Pittsfield
USGS Topo · 1:48,000
1931 · Stetson
USGS Topo · 1:48,000
1932 · Pittsfield
USGS Topo · 1:62,500
1933 · Boyd Lake
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