
Gates Of The Arctic National Park encompasses the northern portion of this landscape, where the North Fork Koyukuk River winds through the interior before it eventually meets the Middle Fork Koyukuk River to the south. The terrain is characterized by the prominent elevations of the Jack White Range, which rises above the river valleys. This 2017 survey documents a wilderness largely defined by its drainage systems, including Florence Cr in the northwest corner. The absence of roads or permanent structures reflects the preserved status of this subarctic environment, emphasizing the natural corridors formed by the braided river channels that have historically guided travel through the Yukon-Koyukuk region.
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1951 · Bettles
USGS Topo · 1:250,000
1951 · Wiseman
USGS Topo · 1:250,000
1956 · Bettles
USGS Topo · 1:250,000
1956 · Wiseman
USGS Topo · 1:250,000
1964 · Wiseman
USGS Topo · 1:250,000
1970 · Wiseman A-3
USGS Topo · 1:63,360
1970 · Wiseman A-2
USGS Topo · 1:63,360
1970 · Bettles D-3
USGS Topo · 1:63,360
1970 · Bettles D-2
USGS Topo · 1:63,360
2016 · Wiseman A-3 NE
USGS Topo · 1:25,000