
The Kuskokwim River defines the southern edge of this remote Interior Alaska landscape, where low-lying wetlands give way to rising upland terrain. In the southwestern corner, the prominent rise of Appel Mtn stands as a significant landmark above the surrounding drainage basins. The area is characterized by a complex network of seasonal watercourses and ponds, most notably the meandering Broken Snowshoe Cr and Grayling Cr. This 2019 survey illustrates the untouched character of the Yukon-Koyukuk region, lacking any established roads or permanent settlements within the quadrangle. The topography suggests a wilderness transition, where the river's influence on the land is countered by the isolated peaks that guide local drainage patterns.
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This is the sole edition of this map. No revisions or reprints were ever made.
1949 · McGrath
USGS Topo · 1:250,000
1950 · Medfra
USGS Topo · 1:250,000
1950 · McGrath
USGS Topo · 1:250,000
1953 · McGrath D-5
USGS Topo · 1:63,360
1954 · Medfra A-6
USGS Topo · 1:63,360
1954 · McGrath D-6
USGS Topo · 1:63,360
1954 · Medfra A-5
USGS Topo · 1:63,360
1958 · McGrath
USGS Topo · 1:250,000
1959 · Medfra
USGS Topo · 1:250,000
2019 · McGrath D-5 NW
USGS Topo · 1:25,000