
Stuyahok River winds through the northern portion of this Alaskan interior landscape, a region defined by complex drainage patterns and low-lying wetlands. The Stuyahok Hills rise as the primary topographic prominence in the northeast, providing a rare break in the expanse of small lakes and unnamed ponds that cover much of the terrain. Mapped primarily through aerial photography from the mid-1950s, the area is characterized by an absence of roads or established settlements, reflecting the remote nature of the Dillingham district during the mid-twentieth century. The intricate web of water bodies suggests a dynamic hydrological environment where land and water constantly intermingle, a typical feature of the region's subarctic geography.
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3 editions found
1950 · Taylor Mountains
USGS Topo · 1:250,000
1951 · Taylor Mountains
USGS Topo · 1:250,000
1951 · Dillingham
USGS Topo · 1:250,000
1954 · Taylor Mountains
USGS Topo · 1:250,000
1954 · Dillingham
USGS Topo · 1:250,000
1954 · Dillingham C-3
USGS Topo · 1:63,360
1954 · Dillingham D-2
USGS Topo · 1:63,360
1954 · Dillingham C-1
USGS Topo · 1:63,360
1954 · Dillingham D-3
USGS Topo · 1:63,360
1954 · Dillingham C-2
USGS Topo · 1:63,360