Deblois anchors the northeastern corner of this coastal Maine interior, where the West Branch Narraguagus River winds through a complex landscape of heaths and granite ridges. The topography is dominated by a series of prominent elevations, including the significant massif of Tunk Mtn and nearby Spring River Mtn. These peaks rise above a network of isolated water bodies such as Myrick Lake, Anderson Pond, and Tilden Pond, illustrating the post-glacial drainage patterns characteristic of the Downeast region.
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1902 · Cherryfield
USGS Topo · 1:62,500
1904 · Cherryfield
USGS Topo · 1:62,500
1929 · Lead Mountain
USGS Topo · 1:48,000
1930 · Tunk Lake
USGS Topo · 1:48,000
1932 · Tunk Lake
USGS Topo · 1:62,500
1932 · Lead Mountain
USGS Topo · 1:62,500
1941 · Tug Mountain
USGS Topo · 1:62,500
1942 · Cherryfield
USGS Topo · 1:62,500
1942 · Tunk Lake
USGS Topo · 1:62,500
1943 · Tug Mountain
USGS Topo · 1:62,500