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Revision as of 17:08, 16 September 2013 editFinetooth (talk | contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers123,692 edits added basin size and average discharge, citing Benke← Previous edit Revision as of 17:09, 16 September 2013 edit undoFinetooth (talk | contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers123,692 edits roundingNext edit →
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| length_note = <ref name="gnis"/> | length_note = <ref name="gnis"/>
| watershed_imperial = 5750 | watershed_imperial = 5750
| watershed_round = 0 | watershed_round = -1
| watershed_note = <ref name="Benke">{{cite book|last=Benke|first=Arthur C., ed.|coauthor=Cushing, Colbert E., ed.|title=Rivers of North America|location=Burlington, Massachusetts|publisher=Elsevier Academic Press|year=2005|page=934|isbn=0-12-088253-1}}</ref> | watershed_note = <ref name="Benke">{{cite book|last=Benke|first=Arthur C., ed.|coauthor=Cushing, Colbert E., ed.|title=Rivers of North America|location=Burlington, Massachusetts|publisher=Elsevier Academic Press|year=2005|page=934|isbn=0-12-088253-1}}</ref>
| discharge_location = | discharge_location =
| discharge_imperial = 4700 | discharge_imperial = 4700
| discharge_round = 1 | discharge_round = 0
| discharge_note = <ref name="Benke"/> | discharge_note = <ref name="Benke"/>
| discharge_max_imperial = | discharge_max_imperial =

Revision as of 17:09, 16 September 2013

Template:Geobox

The Sagavanirktok River is a river in Alaska's North Slope. 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

  1. Cite error: The named reference gnis was invoked but never defined (see the help page).
  2. Alaska Atlas & Gazetteer (7th ed.). Yarmouth, Maine: DeLorme. 2010. pp. 135–36. ISBN 978-0-89933-289-5.
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