Stannard serves as a central point in this northern Vermont landscape, surrounded by high-elevation landmarks such as Wheelock Mountain and Stannard Mountain. The terrain is defined by a dense network of mountain brooks, including Morrison Brook and Fall Brook, which feed into larger bodies of water like Coles Pond and the Lamoille River. The settlement pattern reflects a deeply rooted local history, with small clusters like Sheffield Square and Fairbanks Mills connected by winding routes like the Pellegrini Pike.
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1928 · Hardwick
USGS Topo · 1:62,500
1934 · Hardwick
USGS Topo · 1:48,000
1935 · Lyndonville
USGS Topo · 1:48,000
1938 · Hardwick
USGS Topo · 1:62,500
1938 · St. Johnsbury
USGS Topo · 1:48,000
1939 · Lyndonville
USGS Topo · 1:62,500
1939 · Plainfield
USGS Topo · 1:48,000
1940 · Plainfield
USGS Topo · 1:62,500
1943 · Plainfield
USGS Topo · 1:62,500
1943 · St. Johnsbury
USGS Topo · 1:62,500