Sandy River and Wilson Stream converge at the northern edge of this landscape, defining the settlement pattern around Farmington Falls. This area of central Maine is characterized by a series of north-south running ridges and narrow stream valleys that shaped the development of local roads and farmsteads. In the central part of the quadrangle, Chesterville sits near the Mercer Dam on the Little Norridgewock Stream, illustrating how early residents utilized local waterpower.
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This is the sole edition of this map. No revisions or reprints were ever made.
1892 · Augusta
USGS Topo · 1:62,500
1894 · Norridgewock
USGS Topo · 1:62,500
1898 · Norridgewock
USGS Topo · 1:62,500
1910 · Livermore
USGS Topo · 1:62,500
1912 · Livermore
USGS Topo · 1:62,500
1924 · Farmington
USGS Topo · 1:62,500
1941 · Livermore
USGS Topo · 1:62,500
1941 · Augusta
USGS Topo · 1:62,500
1943 · Augusta
USGS Topo · 1:62,500
1943 · Norridgewock
USGS Topo · 1:62,500