
Scammon Bay serves as the primary coastal anchor on this western Alaska landscape, situated where the lowland marshes meet the rising topography. The terrain is sharply divided between the northern marshlands, characterized by a dense network of lakes and the winding Kun River, and the southern heights of the As Kinuk Mountains. This 1952 study captures the area's vital waterways, including the Bar River and Kalomak River, which provide natural corridors through the delta.
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2 editions found
1951 · Hooper Bay
USGS Topo · 1:250,000
1951 · Black
USGS Topo · 1:250,000
1952 · Black A-2
USGS Topo · 1:63,360
1952 · Black A-1
USGS Topo · 1:63,360
1952 · Hooper Bay C-3
USGS Topo · 1:63,360
1952 · Hooper Bay D-1
USGS Topo · 1:63,360
1952 · Hooper Bay C-1
USGS Topo · 1:63,360
1953 · Hooper Bay
USGS Topo · 1:250,000
1953 · Hooper Bay C-2
USGS Topo · 1:63,360
1953 · Hooper Bay D-3
USGS Topo · 1:63,360