
Pennellville and Gilbert Mills anchor this central New York landscape, where the terrain is defined by a dense network of slow-moving waterways and wetland areas. The Oswego River cuts through the southwestern corner near Hinmansville, while the interior is characterized by the broad Beaver Meadow and the extensive Peter Scott Swamp to the south. These features, combined with the presence of Great Bear Spring, suggest a region long-shaped by its high water table and glacial drainage patterns.
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This is the sole edition of this map. No revisions or reprints were ever made.
1895 · Syracuse
USGS Topo · 1:62,500
1898 · Syracuse
USGS Topo · 1:62,500
1900 · Baldwinsville
USGS Topo · 1:62,500
1900 · Fulton
USGS Topo · 1:62,500
1905 · Mexico
USGS Topo · 1:62,500
1940 · Brewerton
USGS Topo · 1:24,000
1943 · Oswego East
USGS Topo · 1:31,680
1943 · Lysander
USGS Topo · 1:31,680
1943 · New Haven
USGS Topo · 1:31,680
1943 · Brewerton
USGS Topo · 1:31,680