
Georgetown sits at the prominent confluence where the George River meets the winding Kuskokwim River, serving as a central point of settlement in this interior landscape. This mid-century survey captures a river-dependent geography defined by isolated outposts and clearings, including several instances of a Cabin and identified Ruins along the water's edge. The presence of a Cem near the riverbank suggests a long-standing human connection to this specific stretch of the Kuskokwim. Away from the main river channels, the terrain is carved by numerous tributaries such as Steamboat Creek, California Creek, and Downey Creek. High points are meticulously marked by triangulation stations like VABM Downey 1804 and VABM Tundra 1954, providing a rare look at the established survey network in a region with no roads or trails indicated at the time of mapping.
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2 editions found
1950 · Sleetmute
USGS Topo · 1:250,000
1951 · Iditarod
USGS Topo · 1:250,000
1954 · Sleetmute C-4
USGS Topo · 1:63,360
1954 · Sleetmute D-4
USGS Topo · 1:63,360
1954 · Sleetmute D-6
USGS Topo · 1:63,360
1954 · Iditarod A-4
USGS Topo · 1:63,360
1954 · Iditarod A-3
USGS Topo · 1:63,360
1954 · Sleetmute C-6
USGS Topo · 1:63,360
1954 · Sleetmute C-5
USGS Topo · 1:63,360
1954 · Sleetmute
USGS Topo · 1:250,000