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| The '''Sagavanirktok River'''{{Pronunciation-needed}} is a stream in the ] of the ] of ].<ref name="gnis"/> It is about {{convert|180|mi|km}} long and originates on the north slope of the ], flowing north to the ] near ]. The ] and ] roughly parallel it from ] to ].<ref name="DeLorme">{{cite book|title=Alaska Atlas & Gazetteer|publisher=DeLorme|location=Yarmouth, Maine|pages=135–36|edition=7th|year=2010|isbn=978-0-89933-289-5}}</ref> Also, a glaciation happened approximately at the same time as the ] of central North America at the Sagavanirktok River.{{Citation needed|date=August 2007}} | The '''Sagavanirktok River'''{{Pronunciation-needed}} or '''Sag River''' is a stream in the ] of the ] of ].<ref name="gnis"/> It is about {{convert|180|mi|km}} long and originates on the north slope of the ], flowing north to the ] near ]. The ] and ] roughly parallel it from ] to ].<ref name="DeLorme">{{cite book|title=Alaska Atlas & Gazetteer|publisher=DeLorme|location=Yarmouth, Maine|pages=135–36|edition=7th|year=2010|isbn=978-0-89933-289-5}}</ref> Also, a glaciation happened approximately at the same time as the ] of central North America at the Sagavanirktok River.{{Citation needed|date=August 2007}} | ||
| ==See also== | ==See also== | ||
Revision as of 16:41, 29 November 2015
The Sagavanirktok River or Sag River is a stream in the North Slope Borough of the U.S. state of Alaska. It is about 180 miles (290 km) 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. Also, a glaciation happened approximately at the same time as the Illinoian Stage of central North America at the Sagavanirktok River.
See also
References
- Cite error: The named reference
gniswas invoked but never defined (see the help page). - Alaska Atlas & Gazetteer (7th ed.). Yarmouth, Maine: DeLorme. 2010. pp. 135–36. ISBN 978-0-89933-289-5.
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