
Three-Day-Slough dominates this remote Alaskan landscape, winding through a complex network of wetlands and meanders. The slough's intricate path illustrates the dynamic hydrology of the region, where water levels and shifting channels are the primary architects of the terrain. To the south, Tachanlowa Lake sits within a low-lying basin, while the Koyukuk River cuts through the southeastern corner of the survey. A prominent landform known as Colville Bend highlights a significant turn in the waterway, marking a point of geological interest for those studying the fluvial processes of the Yukon-Koyukuk interior. This 2016 survey documents the precise configuration of these vital water bodies before the inevitable shifts caused by seasonal flooding and permafrost changes.
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.
1951 · Kateel River
USGS Topo · 1:250,000
1952 · Kateel River B-3
USGS Topo · 1:63,360
1952 · Kateel River B-2
USGS Topo · 1:63,360
1954 · Kateel River C-2
USGS Topo · 1:63,360
1954 · Kateel River C-3
USGS Topo · 1:63,360
1955 · Kateel River
USGS Topo · 1:250,000
2015 · Kateel River C-3 SW
USGS Topo · 1:25,000
2015 · Kateel River C-3 NW
USGS Topo · 1:25,000
2015 · Kateel River B-3 NW
USGS Topo · 1:25,000
2015 · Kateel River B-3 NE
USGS Topo · 1:25,000