
Owl Hills and the prominent height of Owl High define this interior Alaskan landscape, characterized by a complex network of wetland basins and low ridges. The presence of John Barleycorn Lakes in the east and Queer Ponds further north suggests the slow drainage patterns typical of this subarctic region, where water moves through seasonal drainages like Owl Cr and Bull Cr. The terrain is marked by significant topographical markers such as Little Dome and Hermit Ridge, which offer perspective over the surrounding Bear Gulch. This 2017 survey provides an exacting record of the township and range lines across a region defined by its hydrography rather than human settlement, serving as a baseline for environmental study and topographical history in the Yukon-Koyukuk Census Area.
13 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1951 · Beaver
USGS Topo · 1:250,000
1956 · Beaver B-2
USGS Topo · 1:63,360
1956 · Beaver B-3
USGS Topo · 1:63,360
1956 · Beaver
USGS Topo · 1:250,000
1964 · Beaver
USGS Topo · 1:250,000
1990 · Beaver C-2
USGS Topo · 1:63,360
1990 · Beaver C-3
USGS Topo · 1:63,360
2017 · Beaver B-3 NW
USGS Topo · 1:25,000
2017 · Beaver B-3 SW
USGS Topo · 1:25,000
2017 · Beaver B-2 NW
USGS Topo · 1:25,000