
Harding Icefield dominates the western interior of this coastal survey, where massive ice flows descend through the Kenai Mountains toward the deep fjords of the Kenai Peninsula. In the early 1950s, this landscape was defined by the raw movement of ice and water, captured here through aerial photogrammetry. Tidal inlets like Aialik Bay and Holgate Arm show a complex shoreline where the Aialik Glacier and Holgate Glacier meet the sea.
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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