Baskahegan Stream winds through this interior Maine landscape, defining the drainage patterns of a region dominated by low-lying wetlands and isolated peaks. The terrain is anchored by the modest elevations of Dill Hill and Horse Hill, which rise above a network of smaller tributaries including Pleasant Brook, Horsehill Brook, and Lindsey Brook. This 2011 survey reflects a sparsely populated area where the human footprint is limited to a handful of gravel roads and rural tracks, such as Atlas Rd and Schillinger Rd. Significant water bodies like Dipper Pond and the edge of Trout Lake provide essential landmarks in a territory where natural hydrography dictated early access and land use. The presence of Dipper Pond Rd suggests localized recreational or logging access, characteristic of northern Penobscot County's timberlands.
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This is the sole edition of this map. No revisions or reprints were ever made.
1931 · Springfield
USGS Topo · 1:48,000
1934 · Springfield
USGS Topo · 1:62,500
1940 · Danforth
USGS Topo · 1:62,500
1941 · Danforth
USGS Topo · 1:62,500
1941 · Scraggly Lake
USGS Topo · 1:62,500
1941 · Wytopitlock
USGS Topo · 1:62,500
1943 · Danforth
USGS Topo · 1:62,500
1943 · Wytopitlock
USGS Topo · 1:62,500
1944 · Scraggly Lake
USGS Topo · 1:62,500
1954 · Millinocket
USGS Topo · 1:250,000