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The '''Killik River'''{{Pronunciation-needed}} is a {{convert|105|mi|km|adj=on}} tributary of the ] in the ] of ].<ref name="gnis"/> It begins in the northern portion of ] and flows north onto property of the ]. The '''Killik River'''{{Pronunciation-needed}} is a {{convert|105|mi|km|adj=on}} tributary of the ] in the ] of ].<ref name="gnis"/> It begins in the northern portion of ] and flows north onto property of the ].<ref>{{cite web|title=Killik River 1|url=https://www.google.com/search?q=killik+river+alaska&ie=utf-8&oe=utf-8&aq=t&rls=org.mozilla:en-US:official&client=firefox-a#q=killik+river+north+slope+borough&revid=2121644314&rls=org.mozilla:en-US:official|date=June 10, 2008|publisher=Arctic Slope Regional Corporation|accessdate=September 5, 2013}}</ref>


The river begins on the North Slope of the central ] and merges with the Colville River south of Angoyavik Pass. It arises in the ], in the vicinity of Survey Pass at about N 67° 46.5', and flows through a broad, U-shaped valley. The direction of flow initially is to the northwest, then bending approximately 90° to the northeast before heading generally north at about N 68° 56' and W 154° 12'. North of the Park boundary the river's course runs through the foothills of the ] and on to the coastal plain. The river begins on the North Slope of the central ] and merges with the Colville River south of Angoyavik Pass. It arises in the ], in the vicinity of Survey Pass at about N 67° 46.5', and flows through a broad, U-shaped valley. The direction of flow initially is to the northwest, then bending approximately 90° to the northeast before heading generally north at about N 68° 56' and W 154° 12'. North of the Park boundary the river's course runs through the foothills of the ] and on to the coastal plain.

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The Killik River is a 105-mile (169 km) tributary of the Colville River in the U.S. state of Alaska. It begins in the northern portion of Gates of the Arctic National Park and flows north onto property of the Arctic Slope Regional Corporation.

The river begins on the North Slope of the central Brooks Range and merges with the Colville River south of Angoyavik Pass. It arises in the Endicott Mountains, in the vicinity of Survey Pass at about N 67° 46.5', and flows through a broad, U-shaped valley. The direction of flow initially is to the northwest, then bending approximately 90° to the northeast before heading generally north at about N 68° 56' and W 154° 12'. North of the Park boundary the river's course runs through the foothills of the Brooks Range and on to the coastal plain.

Major tributaries of the Killik are April Creek and Easter Creek, both of which approach the Killik from the southeast. North of Easter Creek, tributary streams, such as Aniakvik Creek and Nigaktukvik Creek, flow predominantly through short, narrow, V-shaped valleys. Numerous changes of the river's course within this valley have left behind a large number of lakes, as well as gravelbars and sandbars. The tundra in the Killik valley appears to be dominated by copious stretches of dwarf birch (betula nana), and sedges, with large expanses of sedge bogs and tussocks.

The Killik is fed largely by precipitation and snow melt, and hence its waters are relatively clear of the sediment that characterizes glacial streams.

See also

References

  1. Cite error: The named reference gnis was invoked but never defined (see the help page).
  2. "Killik River 1". Arctic Slope Regional Corporation. June 10, 2008. Retrieved September 5, 2013.


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