
Glacier Bay National Park encompasses this wilderness landscape where glacial retreat continues to reshape the coastline and mountain terrain. The dynamic environment is dominated by the flow of Morse Glacier in the north and the deep waters of the Tidal Inlet to the west. Landforms such as Oberlin Ridge and Pyramid Peak rise sharply from the water's edge, illustrating the dramatic elevation changes characteristic of this portion of the Alaska panhandle. Along the southeastern shore, Tlingit Point and Sebree Cove provide geographic markers for maritime navigation within Glacier Bay. This 2017 study documents the modern contours of Ice Valley and the surrounding peaks, reflecting contemporary shorelines and ice positions that are critical for understanding the region's environmental evolution.
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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
1948 · Mount Fairweather C-1
USGS Topo · 1:63,360
1948 · Mount Fairweather C-2
USGS Topo · 1:63,360
1949 · Mount Fairweather C-1
USGS Topo · 1:63,360
1950 · Mount Fairweather D-2
USGS Topo · 1:63,360
1950 · Mount Fairweather C-2
USGS Topo · 1:63,360
1951 · Mt Fairweather
USGS Topo · 1:250,000
1954 · Mount Fairweather D-1
USGS Topo · 1:63,360
1961 · Mt Fairweather
USGS Topo · 1:250,000