
The Black River snakes through the expansive marshlands and river deltas of the Kusilvak Census Area, defining the wet, low-lying geography of this Alaskan interior. While much of the landscape is dominated by water and shifting riverbanks, the terrain rises sharply in the east toward the Kusilvak Mountains and the distinct Ulokat Hills. These high points provide a stark vertical contrast to the surrounding tundra and the numerous interconnected water bodies, such as Nunavakonuk Lake. Hydrological patterns are further established by the Taslaktoli River and Kun River, which together illustrate the complex drainage systems typical of the Yukon-Kuskokwim Delta region. This survey highlights a wilderness where geography is governed almost entirely by seasonal water cycles and prominent geological uplifts.
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This is the sole edition of this map. No revisions or reprints were ever made.
1951 · Marshall
USGS Topo · 1:250,000
1952 · Kwiguk
USGS Topo · 1:250,000
1952 · Kwiguk A-6
USGS Topo · 1:63,360
1952 · Marshall D-7
USGS Topo · 1:63,360
1952 · Marshall D-8
USGS Topo · 1:63,360
1954 · Marshall
USGS Topo · 1:250,000
2020 · Marshall D-8 SW
USGS Topo · 1:25,000
2020 · Marshall D-7 NW
USGS Topo · 1:25,000
2020 · Marshall D-8 SE
USGS Topo · 1:25,000
2020 · Marshall D-8 NW
USGS Topo · 1:25,000