
The Deerfield River and its numerous tributaries, including Cold Brook and Binney Brook, define the settlement patterns of this southern Vermont landscape. In the late 19th century, the Hoosac Tunnel and Wilmington R.R. followed the river's winding path south toward Readsboro, providing a vital rail link through the mountainous terrain. The map captures established mountain communities such as Wilmington, Jacksonville, and Whitingham before significant 20th-century hydrological changes altered the valley floors. High elevations are marked by prominent peaks like Haystack Mountain and Hogback Mountain, while local industry and agriculture are situated near water sources like Sadawga Pond and Ray Pond. The proximity of Davis Bridge and various mills along the river branches reflects a period of peak rural activity in Windham and Bennington Counties.
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7 editions found
1886 · Greylock
USGS Topo · 1:62,500
1886 · Hawley
USGS Topo · 1:62,500
1889 · Wilmington
USGS Topo · 1:62,500
1890 · Hawley
USGS Topo · 1:62,500
1890 · Greenfield
USGS Topo · 1:62,500
1891 · Wilmington
USGS Topo · 1:62,500
1891 · Greylock
USGS Topo · 1:62,500
1891 · Brattleboro
USGS Topo · 1:62,500
1893 · Brattleboro
USGS Topo · 1:62,500
1893 · Greylock
USGS Topo · 1:62,500