
Dover and the surrounding borderlands of New Hampshire and Maine are defined by a complex network of tidal rivers and early rail infrastructure in the late 19th century. The confluence of the Cocheco River and Salmon Falls River forms the Piscataqua River, a vital waterway that separates Eliot, Maine, from Newington and Rollinsford. This survey captures the height of the railroad era, showing the Boston and Maine Railroad and its various divisions as they connect industrial hubs like Rochester and Somersworth to coastal ports.
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5 editions found
1888 · Newburyport
USGS Topo · 1:62,500
1888 · Haverhill
USGS Topo · 1:62,500
1890 · Haverhill
USGS Topo · 1:62,500
1890 · Newburyport
USGS Topo · 1:62,500
1891 · Berwick
USGS Topo · 1:62,500
1891 · Kennebunk
USGS Topo · 1:62,500
1893 · Kennebunk
USGS Topo · 1:62,500
1893 · Dover
USGS Topo · 1:62,500
1893 · Berwick
USGS Topo · 1:62,500
1893 · York
USGS Topo · 1:62,500