
Yalik Glacier descends from the high elevations of the Kenai Peninsula Borough toward the deep marine waters of the Gulf of Alaska. This coastline, defined by the massive landmass of Nuka Island and the intricate channels of the Pye Islands, reveals a landscape where maritime access dictated small-scale human activity. Isolated cabins are noted along the western shores of the island, suggesting seasonal use for fishing or trapping during the mid-twentieth century.
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2 editions found
1951 · Seldovia
USGS Topo · 1:250,000
1951 · Seldovia A-3
USGS Topo · 1:63,360
1951 · Seldovia B-3
USGS Topo · 1:63,360
1951 · Seldovia C-3
USGS Topo · 1:63,360
1952 · Seldovia A-3
USGS Topo · 1:63,360
1952 · Seldovia B-3
USGS Topo · 1:63,360
1953 · Seldovia C-3
USGS Topo · 1:63,360
1953 · Seldovia B-1
USGS Topo · 1:63,360
1953 · Seldovia B-2
USGS Topo · 1:63,360
1953 · Seldovia C-2
USGS Topo · 1:63,360