
Bendeleben Mountains dominate the southern half of this mid-century survey, rising sharply above a network of waterways that define the Seward Peninsula interior. The northern landscape is characterized by extensive Lava flows, a stark geological feature that contrasts with the meandering path of the Kuzitrin River. This area is preserved within the Bering Land Bridge National Preserve, reflecting its significance in the natural history of the region. Numerous drainages such as Minnie Creek, Ella Creek, and Harris Creek cut through the terrain, illustrating the complex hydrology of this subarctic environment. The presence of the Base Line and the border of the Arctic Borough provide essential cadastral context for the remote wilderness, which remained largely devoid of established roads or permanent settlements during this period of photogrammetric mapping.
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3 editions found
1950 · Bendeleben C-5
USGS Topo · 1:63,360
1950 · Bendeleben B-5
USGS Topo · 1:63,360
1950 · Bendeleben A-4
USGS Topo · 1:63,360
1950 · Bendeleben C-3
USGS Topo · 1:63,360
1950 · Bendeleben A-5
USGS Topo · 1:63,360
1950 · Bendeleben A-3
USGS Topo · 1:63,360
1950 · Bendeleben B-4
USGS Topo · 1:63,360
1950 · Bendeleben C-4
USGS Topo · 1:63,360
1950 · Bendeleben B-3
USGS Topo · 1:63,360
1950 · Bendeleben
USGS Topo · 1:250,000