Klutina Lake dominates this glacial landscape, filling a deep, narrow trough between high mountain ridges. The terrain reflects the massive scale of the interior, with the waters fed by high-altitude drainages such as Saint Anne Cr to the north. These features illustrate the natural hydrology of the Copper River basin before any significant human development, where the shoreline remains largely untouched. On either side of the lake, the topography rises sharply to prominent summits including Powell Peak in the northwest and Marshall Mtn to the east. The steep descent of Curtis Gulch highlights the dramatic vertical relief of the Chugach Mountains, where drainage patterns are dictated by the underlying geology of the Unorganized Borough.
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This is the sole edition of this map. No revisions or reprints were ever made.
1948 · Valdez D-5
USGS Topo · 1:63,360
1949 · Valdez D-6
USGS Topo · 1:63,360
1950 · Valdez C-6
USGS Topo · 1:63,360
1951 · Valdez D-5
USGS Topo · 1:63,360
1951 · Valdez D-6
USGS Topo · 1:63,360
1951 · Valdez C-5
USGS Topo · 1:63,360
1952 · Valdez
USGS Topo · 1:250,000
1953 · Valdez C-6
USGS Topo · 1:63,360
1953 · Valdez C-5
USGS Topo · 1:63,360
1960 · Valdez
USGS Topo · 1:250,000