
Glacier Bay National Park dominates this terrain, revealing a landscape defined by dramatic glacial activity and tidal waters. The topography centers on the intersection of ancient ice and the sea, where the Carroll Glacier moves through the western reaches while the Bruce Hills rise to the south. This area serves as a primary study in post-glacial landscape evolution, as the massive ice sheets that once covered these peaks continue to recede and reshape the coastline. The waters of Muir Inlet penetrate the northeastern corner of the map, providing a glimpse into the intricate network of fjords that characterize this protected wilderness. In a region where the land is literally rising due to isostatic rebound, the map documents the precise contours of these transitioning elevations, from the sea-level inlets to the high ridges of the interior.
8 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.
1948 · Mount Fairweather D-1
USGS Topo · 1:63,360
1948 · Mount Fairweather D-2
USGS Topo · 1:63,360
1950 · Mount Fairweather D-2
USGS Topo · 1:63,360
1951 · Mt Fairweather
USGS Topo · 1:250,000
1952 · Skagway
USGS Topo · 1:250,000
1954 · Mount Fairweather D-1
USGS Topo · 1:63,360
1961 · Skagway A-4
USGS Topo · 1:63,360
1961 · Skagway A-5
USGS Topo · 1:63,360
1961 · Mt Fairweather
USGS Topo · 1:250,000
1961 · Skagway
USGS Topo · 1:250,000