Wrangell-Saint Elias National Park encompasses this high-altitude Alaskan landscape, where massive ice fields shape the topography of the Wrangell Mountains. The glacial movement here is a dominant force, visible through the expansive Nabesna Glacier in the north and the Root Glacier and Kennicott Glacier in the south. The convergence of these ice flows creates a dynamic environment of moraines and high ridges, punctuated by the W Fork Glacier to the east. This 2017 survey documents the precise contours of the ice and rock during a period of modern glacial study. The map serves as a detailed record of wilderness boundaries and hydrography, showing how the massive frozen rivers interact with the land near the headwaters of major drainage systems.
11 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.
1951 · McCarthy
USGS Topo · 1:250,000
1959 · McCarthy C-5
USGS Topo · 1:63,360
1959 · McCarthy C-6
USGS Topo · 1:63,360
1960 · McCarthy D-6
USGS Topo · 1:63,360
1960 · McCarthy D-5
USGS Topo · 1:63,360
1960 · McCarthy
USGS Topo · 1:250,000
1993 · McCarthy C-6
USGS Topo · 1:63,360
1993 · McCarthy C-5
USGS Topo · 1:63,360
2017 · McCarthy C-5 SW
USGS Topo · 1:25,000
2017 · McCarthy C-6 NW
USGS Topo · 1:25,000