
The Colville River carves a massive course along the eastern edge of this Arctic landscape, defining the hydrologic character of the North Slope. Meandering tributaries such as the Kogosukruk River and Ingaluat Cr thread through the tundra, revealing the intricate drainage patterns of this permafrost-underlain region. The lack of built infrastructure or settlements highlights the isolation of this Arctic environment, where the land is primarily characterized by subtle topographic shifts and the seasonal flow of its river systems. Researchers can observe the complex braided channels and oxbow formations where Kikak Cr approaches the primary river valley, illustrating the geomorphology of a landscape largely untouched by permanent development.
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This is the sole edition of this map. No revisions or reprints were ever made.
1952 · Umiat
USGS Topo · 1:250,000
1955 · Umiat C-4
USGS Topo · 1:63,360
1955 · Umiat D-3
USGS Topo · 1:63,360
1955 · Umiat D-4
USGS Topo · 1:63,360
1955 · Umiat C-3
USGS Topo · 1:63,360
1956 · Umiat
USGS Topo · 1:250,000
1964 · Umiat
USGS Topo · 1:250,000
2013 · Umiat C-4 SE
USGS Topo · 1:25,000
2013 · Umiat D-3 SW
USGS Topo · 1:25,000
2013 · Umiat D-4 SE
USGS Topo · 1:25,000