The Ted Stevens Icefield anchors this high-altitude landscape in the Chugach Mountains, where ice and rock define the terrain. Glacial movement is central to the local geography, with the Stephens Glacier and Klutina Glacier serving as the primary sources for the area's drainage systems. Meltwater from these expansive ice bodies feeds into the Klutina River and Stephens Creek, illustrating the transition from frozen icefields to alpine waterways. Rising above the glacial basins are several prominent summits, including Garrett Peak, Mt Ourand, and Mt Evans, which mark the highest points of the local ridges. This map captures the unorganized territory at a time when surveying was conducted through a collaboration between the U.S. Geological Survey and agencies such as the Alaska Dept. of Transportation, providing a detailed look at the ice-to-water cycle in the Alaska wilderness.
14 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Valdez C-6
USGS Topo · 1:63,360
1951 · Valdez B-6
USGS Topo · 1:63,360
1952 · Valdez
USGS Topo · 1:250,000
1953 · Valdez C-6
USGS Topo · 1:63,360
1953 · Valdez B-6
USGS Topo · 1:63,360
1960 · Valdez B-7
USGS Topo · 1:63,360
1960 · Valdez C-7
USGS Topo · 1:63,360
1960 · Valdez
USGS Topo · 1:250,000
1993 · Valdez C-6
USGS Topo · 1:63,360
1993 · Valdez C-7
USGS Topo · 1:63,360