Tunk Lake dominates this Downeast Maine landscape, a deep water body surrounded by a rugged collection of granite peaks including Catherine Mtn, Caribou Mtn, and Black Mtn. The 2014 survey reveals a transition from these high summits down to the low-lying wetlands and coastal bogs of the south. Evidence of the region's rail and timber history appears at Goodwin Siding, while a dense network of smaller waters like Wizard Pond, Spring River Lake, and Flanders Pond are connected by drainages such as Tunk Stream and Whitten Parritt Stream. The map details the remote character of the Hancock and Washington County border, where isolated routes like Me-182 and Black Mountain Rd provide the only access to these glacial ponds and ridges.
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This is the sole edition of this map. No revisions or reprints were ever made.
1902 · Cherryfield
USGS Topo · 1:62,500
1904 · Cherryfield
USGS Topo · 1:62,500
1904 · Bar Harbor
USGS Topo · 1:62,500
1904 · Petit Manan
USGS Topo · 1:62,500
1930 · Tunk Lake
USGS Topo · 1:48,000
1932 · Tunk Lake
USGS Topo · 1:62,500
1942 · Bar Harbor
USGS Topo · 1:62,500
1942 · Cherryfield
USGS Topo · 1:62,500
1942 · Tunk Lake
USGS Topo · 1:62,500
1948 · Bangor
USGS Topo · 1:250,000