Johnson Glacier dominates the northwestern corner of this high-altitude landscape in the Unorganized Borough, where ice and rock meet at the crest of the Alaska Range. Mapping by the U.S. Geological Survey reveals a complex vertical environment defined by dramatic elevation changes, with glacial flows carving deep into the surrounding peaks. The absence of roads or human settlements underscores the primitive state of this terrain, which is organized strictly by the public land survey system through townships such as t18s r15e and t19s r15e. This survey serves as a vital record of glacial extent and alpine topography in a region where the natural environment remains the primary architect of the land.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Mount Hayes
USGS Topo · 1:250,000
1950 · Mount Hayes A-3
USGS Topo · 1:63,360
1951 · Mount Hayes
USGS Topo · 1:250,000
1952 · Mount Hayes A-3
USGS Topo · 1:63,360
1954 · Mount Hayes A-3
USGS Topo · 1:63,360
1955 · Mount Hayes A-2
USGS Topo · 1:63,360
1955 · Mount Hayes B-3
USGS Topo · 1:63,360
1955 · Mount Hayes B-2
USGS Topo · 1:63,360
1955 · Mount Hayes
USGS Topo · 1:250,000
2016 · Mount Hayes B-3 NE
USGS Topo · 1:25,000