
The Suckling Hills rise as a prominent landform above the coastal lowlands in this remote stretch of the Alaskan shoreline. The landscape is defined by a complex network of glacial meltwater channels and tidewater influences, most notably where the Okalee River, Seal River, and Kiklukh River wind through shifting flats toward the Gulf of Alaska. The presence of Vitus Lake in the northeastern corner suggests a dynamic glacial environment, as its waters are traditionally fed by the nearby Bering Glacier system.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Bering Glacier
USGS Topo · 1:250,000
1950 · Icy Bay
USGS Topo · 1:250,000
1951 · Icy Bay
USGS Topo · 1:250,000
1951 · Bering Glacier
USGS Topo · 1:250,000
1959 · Bering Glacier
USGS Topo · 1:250,000
1961 · Icy Bay
USGS Topo · 1:250,000
1984 · Bering Glacier A-8
USGS Topo · 1:63,360
1984 · Bering Glacier A-7
USGS Topo · 1:63,360
2014 · Bering Glacier A-8 NW
USGS Topo · 1:25,000
2014 · Bering Glacier A-8 SW
USGS Topo · 1:25,000