
The Harding Icefield dominates the southern reaches of this mid-century survey, a frozen expanse that serves as the source for several massive glacial systems. Situated within the Kenai Mountains, this frozen landscape is marked by deep crevasses and dramatic ice movement, transitioning into the Bear Glacier and Lowell Glacier as the ice flows toward the coast. To the north and east, the ice gives way to more defined drainages like Cottonwood Creek and Placer Creek, which feed into the Resurrection River.
13 named features on this map. Tap any name to fly to it.
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4 editions found
1944 · Kenai
USGS Topo · 1:250,000
1946 · Blying Sound
USGS Topo · 1:250,000
1950 · Kenai
USGS Topo · 1:250,000
1950 · Kenai B-1
USGS Topo · 1:63,360
1950 · Seward A-8
USGS Topo · 1:63,360
1950 · Blying Sound D-7
USGS Topo · 1:63,360
1950 · Seward A-7
USGS Topo · 1:63,360
1951 · Blying Sound
USGS Topo · 1:250,000
1951 · Seward
USGS Topo · 1:250,000
1951 · Seldovia
USGS Topo · 1:250,000