
Robinson Mountains define the interior of this Alaskan landscape, where glacial activity and hydraulic systems dominate the terrain. This 2016 survey, produced by the U.S. Geological Survey, illustrates the complex geography of the Bering Glacier as it feeds into the surrounding environment. The massive scale of the Bering Glacier in the northwest is countered by the Leeper Glacier in the southeast, framing the central topographic reliefs. Between these ice-bound regions, the Duktoth River carves a path through the valley, reflecting the dynamic hydrologic patterns of the Yakutat region. The map provides a detailed view of the township and range boundaries, including t18s r17e and t19s r18e, offering a precise look at the land division in this glaciated wilderness.
8 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.
1948 · Bering Glacier A-4
USGS Topo · 1:63,360
1950 · Bering Glacier
USGS Topo · 1:250,000
1951 · Bering Glacier
USGS Topo · 1:250,000
1951 · Bering Glacier A-4
USGS Topo · 1:63,360
1959 · Bering Glacier
USGS Topo · 1:250,000
1959 · Bering Glacier A-4
USGS Topo · 1:63,360
1984 · Bering Glacier A-5
USGS Topo · 1:63,360
1984 · Bering Glacier A-4
USGS Topo · 1:63,360
1985 · Bering Glacier B-5
USGS Topo · 1:63,360
1985 · Bering Glacier B-4
USGS Topo · 1:63,360