
The Connecticut River serves as the winding boundary between Vermont and New Hampshire in the mid-1930s, anchoring a landscape defined by its river-and-rail economy. The presence of the Frank D. Comerford Hydro-electric Plant near Monroe highlights the industrial shift toward electrification along the river's edge. This era is characterized by an extensive network of rural education, evidenced by numerous local schoolhouses such as Sugar Hill Sch and North Littleton Sch that once served these upland farming and timber communities.
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4 editions found
1900 · Whitefield
USGS Topo · 1:62,500
1920 · Guildhall
USGS Topo · 1:62,500
1929 · Moosilauke
USGS Topo · 1:62,500
1929 · Franconia
USGS Topo · 1:62,500
1931 · Guildhall
USGS Topo · 1:48,000
1931 · Littleton
USGS Topo · 1:62,500
1931 · Woodsville
USGS Topo · 1:48,000
1932 · Franconia
USGS Topo · 1:62,500
1932 · Littleton
USGS Topo · 1:48,000
1932 · Moosilauke
USGS Topo · 1:62,500