
Brandy Pond serves as a central anchor for this northern interior landscape, situated within the administrative boundaries of Great Pond (Plantation No 33). The terrain is defined by a dense network of waterways, including Buffalo Stream, Guagus Stream, and Main Stream, which navigate between prominent elevations like Passadumkeag Mountain and Lord Mountain. This 1980s-era topographic representation reveals the characteristic topography of the Penobscot and Hancock county line, where the land transitions between steep ridges such as Spaulding Ridge and lower marshy basins. The presence of a Gravel Pit near the southern boundary suggests local resource extraction, while the surrounding hills like Buffalo Hill and Baker Hill remain largely undeveloped, punctuated only by a handful of unimproved roads and trails that traverse the township lines of T 39 M D and T 3 N D.
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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