
Maclaren Glacier dominates the eastern edge of this mid-century topographic record, feeding the south-flowing Maclaren River through a high-altitude wilderness. The drainage network is clearly defined by the East Fork Susitna River and the West Fork Maclaren River, revealing a landscape shaped by ice and water. Evidence of human activity in this remote region is sparse but significant, centered on a lone Cabin and Landing Strips situated near the riverbanks. Geodetic control points like VABM East Fork and VABM Coal indicate the primary survey work conducted by the U.S. Geological Survey and the Bureau of Land Management. The presence of numerous Crevasses across the high snowfields underscores the dynamic and unstable nature of the glacial terrain during the early 1950s.
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2 editions found
1949 · Healy A-1
USGS Topo · 1:63,360
1949 · Mount Hayes A-5
USGS Topo · 1:63,360
1950 · Mount Hayes
USGS Topo · 1:250,000
1950 · Healy B-1
USGS Topo · 1:63,360
1950 · Mount Hayes A-6
USGS Topo · 1:63,360
1951 · Healy
USGS Topo · 1:250,000
1951 · Mount Hayes
USGS Topo · 1:250,000
1951 · Healy C-1
USGS Topo · 1:63,360
1951 · Mount Hayes C-5
USGS Topo · 1:63,360
1951 · Mt. Hayes B-5
USGS Topo · 1:63,360