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The '''Sagavanirktok River''' is a ] in ]'s ].<ref>USGS Geographic Names Information System (GNIS). Accessed Aug 20, 2007.</ref> It is approximately 180 miles long, and originates on the north slope of the ], flowing north to the ] near ]. The ] and ] roughly parallel it from ] to ]. Also, a glaciation happened approximately at the same time as the ] of central North America at the Sagavanirktok River.{{ |
The '''Sagavanirktok River''' is a ] in ]'s ].<ref>USGS Geographic Names Information System (GNIS). Accessed Aug 20, 2007.</ref> It is approximately 180 miles long, and originates on the north slope of the ], flowing north to the ] near ]. The ] and ] roughly parallel it from ] to ]. Also, a glaciation happened approximately at the same time as the ] of central North America at the Sagavanirktok River.{{Citation needed|date=August 2007}} | ||
==References== | ==References== | ||
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{{NorthSlopeAK-geo-stub}} | {{NorthSlopeAK-geo-stub}} |
Revision as of 04:37, 18 March 2011
The Sagavanirktok River is a river in Alaska's North Slope. It is approximately 180 miles long, and originates on the north slope of the Brooks Range, flowing north to the Beaufort Sea near Prudhoe Bay. The Trans-Alaska Pipeline System and Dalton Highway roughly parallel it from Atigun Pass to Deadhorse, Alaska. Also, a glaciation happened approximately at the same time as the Illinoian Stage of central North America at the Sagavanirktok River.
References
- USGS Geographic Names Information System (GNIS). Sagavanirktok River. Accessed Aug 20, 2007.
See also
70°19′15″N 148°02′10″W / 70.32083°N 148.03611°W / 70.32083; -148.03611
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