
The Sandy River and Rangeley Lakes RR winds through the river valleys of the Maine interior, anchoring a landscape of small milling communities and rural schools as it appeared in the early 1930s. At the confluence of the Carrabassett River and Stanley Stream, the town of Kingfield stands as a primary hub of activity. Further south, the Sandy River bypasses Soule Mill and South Strong, while a network of rural schoolhouses, including the Millay Sch and Parsons Sch, reflects the distributed settlement pattern of the era.
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4 editions found
1894 · Norridgewock
USGS Topo · 1:62,500
1898 · Norridgewock
USGS Topo · 1:62,500
1903 · Bingham
USGS Topo · 1:62,500
1904 · Anson
USGS Topo · 1:62,500
1905 · Bingham
USGS Topo · 1:62,500
1924 · Farmington
USGS Topo · 1:62,500
1926 · Dixfield
USGS Topo · 1:62,500
1928 · Dead River
USGS Topo · 1:62,500
1928 · Stratton
USGS Topo · 1:48,000
1929 · Phillips
USGS Topo · 1:48,000