
Chitanatala Mountains define the southern landscape of this remote Yukon-Koyukuk interior, providing a dramatic vertical contrast to the winding path of the Cosna River. The river traverses the eastern sections of the quadrangle, carving a serpentine route through the lowlands as it flows northward. This 2017 edition illustrates the complex hydrography of the Alaskan interior, showing how the drainage patterns are strictly governed by the proximity of the mountains. Beyond the primary waterway, the terrain is marked by a network of smaller drainages and shifting elevations across the township and range boundaries of t1n r20w, t1s r21w, and t2s r20w. This specific survey offers a detailed view of an area shaped by glacial and fluvial processes, where the presence of the Cosna River indicates a dynamic landscape of seasonally changing water levels and wilderness navigation.
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This is the sole edition of this map. No revisions or reprints were ever made.
1948 · Kantishna River
USGS Topo · 1:250,000
1951 · Kantishna River
USGS Topo · 1:250,000
1952 · Kantishna River
USGS Topo · 1:250,000
1952 · Kantishna River D-3
USGS Topo · 1:63,360
1952 · Kantishna River C-3
USGS Topo · 1:63,360
1952 · Kantishna River C-4
USGS Topo · 1:63,360
1953 · Kantishna River D-4
USGS Topo · 1:63,360
1954 · Kantishna River D-3
USGS Topo · 1:63,360
1954 · Kantishna River D-4
USGS Topo · 1:63,360
1954 · Kantishna River C-3
USGS Topo · 1:63,360