
Brandy Pond and its surrounding wetlands form a central hydrological hub for this area on the Penobscot and Hancock County line. The terrain is defined by a series of prominent elevations, including Passadumkeag Mtn in the north and Spaulding Ridge to the southwest, which dictate the complex drainage patterns of the region. Numerous watercourses such as Guagus Stream, Buffalo Stream, and Dead Stream weave through the lowlands between these heights. This modern survey reflects a landscape primarily characterized by timber management and natural water bodies, with a network of access routes like Brandy Pond Rd and numbered forestry roads such as 24-00-0 providing the only terrestrial transit through the dense interior.
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This is the sole edition of this map. No revisions or reprints were ever made.
1929 · Great Pond
USGS Topo · 1:48,000
1929 · Lead Mountain
USGS Topo · 1:48,000
1931 · Saponac
USGS Topo · 1:48,000
1932 · Nicatous Lake
USGS Topo · 1:48,000
1932 · Lead Mountain
USGS Topo · 1:62,500
1932 · Great Pond
USGS Topo · 1:62,500
1934 · Saponac
USGS Topo · 1:62,500
1934 · Nicatous Lake
USGS Topo · 1:62,500
1948 · Bangor
USGS Topo · 1:250,000
1954 · Millinocket
USGS Topo · 1:250,000