Kenai National Wildlife Refuge dominates this section of the Kenai Peninsula, showcasing a landscape defined by dramatic glacial activity and alpine hydrology. The ice fields of Chernof Glacier and Dinglestadt Glacier serve as the primary geographical anchors, illustrating the ongoing process of glacial movement and melt that shapes the surrounding valleys. Below the ice, Glacier Lake collects the runoff in a high-elevation basin, typical of the transitional drainage patterns found in this wilderness. This 2017 survey by the U.S. Geological Survey provides a precise topographic record of these shifting ice masses and remote water bodies within the Kenai Peninsula Borough, capturing the exact extent of the ice and the complex contouring of the high peaks during the early 21st century.
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This is the sole edition of this map. No revisions or reprints were ever made.
1950 · Seldovia D-2
USGS Topo · 1:63,360
1951 · Seldovia
USGS Topo · 1:250,000
1951 · Seldovia D-1
USGS Topo · 1:63,360
1953 · Seldovia C-2
USGS Topo · 1:63,360
1953 · Seldovia D-2
USGS Topo · 1:63,360
1953 · Seldovia C-1
USGS Topo · 1:63,360
1953 · Seldovia D-1
USGS Topo · 1:63,360
1963 · Seldovia
USGS Topo · 1:250,000
2017 · Seldovia C-2 NE
USGS Topo · 1:25,000
2017 · Seldovia D-2 NE
USGS Topo · 1:25,000