Bear Island Lake sits at the northern edge of this interior landscape, which is defined by an intricate network of waterways draining toward the southwest. This 2019 survey captures the hydrological complexity of the Unorganized Borough, where meandering channels like Tonclohukna Cr and Telidaside Cr carve through low-lying terrain. The drainage pattern is further characterized by the convergence of Middle Cr and the larger Slow Fork, illustrating the natural transition of the subarctic watershed before it reaches more prominent river systems. The map reflects a region dominated by raw natural geography, devoid of established roads or permanent settlements, where the terrain is segmented only by the formal boundaries of the Public Land Survey System.
11 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Medfra
USGS Topo · 1:250,000
1958 · Medfra A-2
USGS Topo · 1:63,360
1958 · Medfra B-2
USGS Topo · 1:63,360
1958 · Medfra A-1
USGS Topo · 1:63,360
1958 · Medfra B-1
USGS Topo · 1:63,360
1959 · Medfra
USGS Topo · 1:250,000
2019 · Medfra A-2 NE
USGS Topo · 1:25,000
2019 · Medfra B-1 SE
USGS Topo · 1:25,000
2019 · Medfra B-1 NW
USGS Topo · 1:25,000
2019 · Medfra B-1 NE
USGS Topo · 1:25,000