Wrangell-Saint Elias National Park encompasses this high-altitude landscape in the Alaska-Valdez-Cordova Census Area. The terrain is defined by massive ice flows and glacial tributaries, most notably the Chitina Glacier and Walsh Glacier, which converge and feed into the wider basin. These frozen rivers carve deep paths through the land, with the Logan Glacier contributing to the complex hydrological network that eventually meets the Chitina River. The map provides a precise record of these glacial boundaries and elevations as they stood in 2017. This survey serves as a vital document for understanding the glacial extent in one of the most remote sections of the American wilderness, where the lack of any man-made infrastructure highlights the sheer scale of the natural environment.
9 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 · Bering Glacier
USGS Topo · 1:250,000
1951 · McCarthy
USGS Topo · 1:250,000
1951 · Bering Glacier
USGS Topo · 1:250,000
1959 · McCarthy A-2
USGS Topo · 1:63,360
1959 · McCarthy A-1
USGS Topo · 1:63,360
1959 · Bering Glacier
USGS Topo · 1:250,000
1960 · McCarthy
USGS Topo · 1:250,000
1984 · Bering Glacier D-2
USGS Topo · 1:63,360
1984 · Bering Glacier D-1
USGS Topo · 1:63,360
2017 · Bering Glacier D-2 SW
USGS Topo · 1:25,000