
The Yukon River cuts across the southern reach of this landscape, serving as a primary geographic anchor in the Yukon-Koyukuk region. In the southwest corner, modern infrastructure intersects the wilderness where the Dalton Highway and the Alaska Pipeline run parallel through the terrain. These corridors represent critical transportation and energy arteries for the state, carved into a topography defined by the Fort Hamlin Hills to the north and the prominence of Smoothface Mtn. Drainage patterns are visible through seasonal flows like Woodcamp Cr, which meanders through the central interior. This 2017 survey reflects the enduring spatial relationship between the massive scale of the northern interior and the concentrated industrial footprints required to navigate and utilize it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1945 · Livengood
USGS Topo · 1:250,000
1951 · Livengood
USGS Topo · 1:250,000
1951 · Beaver
USGS Topo · 1:250,000
1952 · Livengood D-5
USGS Topo · 1:63,360
1956 · Beaver A-5
USGS Topo · 1:63,360
1956 · Beaver
USGS Topo · 1:250,000
1956 · Livengood D-6
USGS Topo · 1:63,360
1956 · Livengood
USGS Topo · 1:250,000
1964 · Beaver
USGS Topo · 1:250,000
1964 · Livengood
USGS Topo · 1:250,000