Bradley Lake sits at the southern edge of this Kenai Peninsula landscape, serving as a primary hydrological basin for the glacial runoff and mountain streams of the region. The drainage patterns are defined by the Bradley River, which winds westward through the center of the sheet, while the northern reaches are marked by the braided channels of the Fox River and the meandering flow of Sheep Creek. This 2017 survey illustrates the complex relationship between the high alpine contours and the sprawling wetlands of the valley floors. Unlike coastal maps that show human infrastructure, this section of the Seldovia quadrangle focuses on the raw hydrology of the Alaska wilderness, where river systems like the Bradley River shift through wide alluvial plains before reaching the deeper waters of the lake.
10 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.
1950 · Seldovia D-2
USGS Topo · 1:63,360
1951 · Seldovia
USGS Topo · 1:250,000
1951 · Seldovia D-3
USGS Topo · 1:63,360
1951 · Seldovia C-3
USGS Topo · 1:63,360
1953 · Seldovia C-3
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 D-3
USGS Topo · 1:63,360
1963 · Seldovia
USGS Topo · 1:250,000
1987 · Seldovia D-3 SW
USGS Topo · 1:25,000