
The Harding Icefield dominates the western interior of this coastal terrain, where massive rivers of ice descend through the Kenai Mountains toward the sea. This 1951 survey, based on 1950 aerial photography, documents the active glacial interface of the Kenai Peninsula before mid-century environmental shifts. The map illustrates a complex coastline defined by deep fjords and maritime hazards, featuring prominent ice-flows like the Bear Glacier and Holgate Glacier.
27 named features on this map. Tap any name to fly to it.
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3 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 · 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
1951 · Seward A-7
USGS Topo · 1:63,360