
The Harding Icefield dominates the southern landscape of this 1951 survey, a glacial expanse punctuated by numerous crevasses that illustrate the dynamic nature of the Kenai Peninsula's interior. This high-altitude wilderness transitions from the frozen plateau into the jagged Kenai Mountains, where the massive Lowell Glacier descends toward the coast. The mapping of the Seward Base Line across this difficult terrain highlights the surveyor's efforts to establish a grid in a region largely defined by ice and rock.
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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