This is an old revision of this page, as edited by Backspace (talk | contribs) at 19:01, 11 January 2011 (To correct the name, geocoordinates of major tributary). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
Revision as of 19:01, 11 January 2011 by Backspace (talk | contribs) (To correct the name, geocoordinates of major tributary)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)Template:Geobox The Anaktuvuk River is a river in Alaska's North Slope. One hundred and thirty-five miles long, it flows west from glaciers in the Endicott Mountains changing direction just north of Anaktuvuk Pass to flow north to the Arctic Coastal Plain where it joins the Colville River. Its major tributary is the Nanushuk River, which joins it at 69°18′11″N 150°59′58″W / 69.30306°N 150.99944°W / 69.30306; -150.99944. Its headwaters are formed by runoff from various glaciers in the Gates of the Arctic Wilderness on the slopes of Fan Mountain, Alapah Mountain and Limestack Mountain, the last of which lies on the watershed divide between the Arctic Coastal Plain and the Koyukuk River, and feeds the Anaktuvuk River via Graylime Creek.
"The first geologic transect of the Arctic Slope was conducted during the summer of 1901 by USGS geologist F.C. Schrader and topographer W.J. Peters, who descended the Anaktuvuk River in canoes to its junction with the Colville River."
References
- USGS Geographic Names Information System (GNIS). Anaktuvuk River. Accessed Aug 20, 2007.
- Porter, Stephen C. (1966) Pleistocene geology of Anaktuvuk Pass, Central Brooks Range, Alaska (Arctic Institute of North America Technical Paper #18) Arctic Institute of North America, Washington D.C., page 12, OCLC 17327
- Mull, Charles G. et al. (2004) "Geologic Map of the Umiat Quadrangle, Alaska" Scientific Investigations U.S. Department of the Interior Map 2817–A, United States Geological Survey
See also
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