
Chilkoot Lake and the surrounding Takshanuk Mountains define this coastal landscape near the head of the Lynn Canal. In the mid-1950s, the area's geography was a complex network of glacial melt and tidal inlets, with the Chilkat River and Takhin River creating a braided delta system in the southwest. Local infrastructure was concentrated along the Haines Highway and a prominent Pipeline corridor, reflecting the strategic and industrial transit needs of the era.
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4 editions found
1948 · Skagway C-3
USGS Topo · 1:63,360
1948 · Skagway C-2
USGS Topo · 1:63,360
1948 · Skagway A-1
USGS Topo · 1:63,360
1948 · Skagway C-1
USGS Topo · 1:63,360
1949 · Skagway B-1
USGS Topo · 1:63,360
1951 · Skagway A-1
USGS Topo · 1:63,360
1951 · Skagway C-1
USGS Topo · 1:63,360
1951 · Skagway B-1
USGS Topo · 1:63,360
1951 · Skagway C-2
USGS Topo · 1:63,360
1952 · Skagway
USGS Topo · 1:250,000