Farmington Falls sits at a critical bend in the Sandy River, where local roads converge near the northern edge of the Franklin and Kennebec county lines. This central Maine landscape is defined by its glacial heritage, characterized by numerous water bodies like Parker Pond, Norcross Pond, and Crowell Pond interspersed among prominent elevations such as Vienna Mountain and Cape Cod Hill. The distribution of small settlements like North Chesterville and Knowltons Corner reflects a traditional rural layout, with development concentrated along established routes like Vienna Rd and Farmington Falls Rd.
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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