
Mt Bendeleben dominates the central landscape of this portion of the Seward Peninsula, marking the high point of the Bendeleben Mountains. This 2017 survey by the U.S. Geological Survey traces the high-altitude drainage patterns that define this subarctic environment, where the headwaters of the Niukluk River and Libby River descend from steep slopes into the surrounding valleys. The terrain is characterized by intense topographic relief, with the Belt Cr cutting through the northern sections of the map. This area is defined by its lack of permanent modern infrastructure, emphasizing a landscape shaped by natural processes and geological time. The survey provides a clear view of the mountain range's structure, reflecting the remote character of the Nome Census Area and the physical barriers that historically influenced travel and exploration in the Alaskan interior.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Bendeleben B-5
USGS Topo · 1:63,360
1950 · Bendeleben A-4
USGS Topo · 1:63,360
1950 · Bendeleben A-5
USGS Topo · 1:63,360
1950 · Bendeleben B-4
USGS Topo · 1:63,360
1950 · Bendeleben
USGS Topo · 1:250,000
1951 · Bendeleben
USGS Topo · 1:250,000
1964 · Bendeleben
USGS Topo · 1:250,000
1970 · Bendeleben A-4
USGS Topo · 1:63,360
2017 · Bendeleben B-5 SW
USGS Topo · 1:25,000
2017 · Bendeleben A-5 SW
USGS Topo · 1:25,000