
The Copper River dominates this landscape, its braided channels weaving through a corridor of high glacial peaks and deep river valleys as they appeared in 1950. Along the eastern bank, an Old Railroad Grade traces the river's edge, serving as a physical reminder of the early 20th-century transportation routes through this corridor. This industrial footprint contrasts with the massive ice fields of the Schwan Glacier and Cleave Creek Glacier, which remain marked by dangerous Crevasses.
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2 editions found
1948 · Cordova
USGS Topo · 1:250,000
1950 · Valdez A-3
USGS Topo · 1:63,360
1950 · Cordova D-3
USGS Topo · 1:63,360
1951 · Cordova
USGS Topo · 1:250,000
1951 · Valdez B-2
USGS Topo · 1:63,360
1951 · Valdez B-3
USGS Topo · 1:63,360
1951 · Valdez B-4
USGS Topo · 1:63,360
1951 · Cordova D-4
USGS Topo · 1:63,360
1951 · Valdez A-2
USGS Topo · 1:63,360
1952 · Valdez
USGS Topo · 1:250,000