
The Penobscot River serves as the primary corridor for commerce and transport in this part of Maine, with the Maine Central and Canadian Pacific railroads flanking its banks. This 1916 survey reveals a landscape of established mill towns and interconnected waterways, where the river's Sebonibus Rapids and several large islands like Snow Island and Hersey Island dictate the movement of timber and goods. Settlements such as Winn, Chester, and Lincoln follow the rail lines, while the interior is dominated by a dense network of ponds, including Mattanawcook Pond, Madagascal Pond, and Mattakeunk Pond. These water bodies, connected by systems like Dead Stream and Rocky Brook, highlight the region's reliance on hydraulic resources for industry. Higher elevations like Bagley Mtn, Jefferson Mtn, and Twombly Ridge provide a topographical backdrop to the logging and farming communities of Webster Plantation and Lee.
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5 editions found
1917 · Passadumkeag
USGS Topo · 1:62,500
1920 · Winn
USGS Topo · 1:62,500
1931 · Springfield
USGS Topo · 1:48,000
1931 · Saponac
USGS Topo · 1:48,000
1932 · Nicatous Lake
USGS Topo · 1:48,000
1934 · Saponac
USGS Topo · 1:62,500
1934 · Nicatous Lake
USGS Topo · 1:62,500
1934 · Springfield
USGS Topo · 1:62,500
1940 · Mattawamkeag
USGS Topo · 1:62,500
1941 · Wytopitlock
USGS Topo · 1:62,500