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{{Infobox river
{{Geobox|
| name = Koyuk River
<!-- *** Heading *** -->
| name_native = {{native name|mis|Kuuyuk|paren=omit}} (])
| name = Koyuk River
| name_other = Kuyuk
| native_name = Kvyguk River
| other_name = | name_etymology =
<!---------------------- IMAGE & MAP -->
| category_hide =
| image = Serpentine Tors 2007-013 NPS1.jpg
<!-- *** Names **** -->
| image_caption = Part of the ], in the Koyuk River Valley
| etymology = ]
| image_size = 300
| nickname =
| map =
<!-- *** Image *** -->
| map_size = 300
| image =Serpentine Tors 2007-013 NPS1.jpg
| map_caption =
| image_caption =] in the Koyuk River Valley
| pushpin_map = USA Alaska
| image_size =
| pushpin_map_size = 300
<!-- *** Country *** -->
| pushpin_map_caption= Location of the mouth of the Koyuk River in Alaska
| country = {{flag|United States}}
<!---------------------- LOCATION -->
| state = {{flag|Alaska}}
| subdivision_type1 = Country
| region = ]
| subdivision_name1 = ]
<!-- *** Family *** -->
| subdivision_type2 = State
| tributary_left =
| subdivision_name2 = ]
| tributary_right =
| city = | subdivision_type3 =
| city1 = | subdivision_name3 =
| subdivision_type4 = District
| city2 =
| subdivision_name4 = ]
| city3 =
| city4 = | subdivision_type5 =
| subdivision_name5 =
<!-- *** River locations *** -->
<!---------------------- PHYSICAL CHARACTERISTICS -->
| source = ] of western ]
| length = {{convert|115|mi|km|abbr=on}}<ref name="gnis"/>
| source_location =
| width_min =
| source_region =
| width_avg =
| source_country =
| width_max =
| source_elevation_imperial =
| source_lat_d = | depth_min =
| source_lat_m = | depth_avg =
| source_lat_s = | depth_max =
| discharge1_location=
| source_lat_NS =N
| source_long_d = | discharge1_min =
| source_long_m = | discharge1_avg =
| source_long_s = | discharge1_max =
<!---------------------- BASIN FEATURES -->
| source_long_EW =W
| source1 = small lake {{convert|3|mi|km}} north of Kuzitrin Lake
| source_coordinates_note =
| source1_location = ], ]
<!-- *** Mouth *** -->
| source1_coordinates= {{coord|65|25|44|N|163|13|00|W|display=inline}}<ref name="gnis"/>
| mouth = ]
| source1_elevation = {{convert|1526|ft|abbr=on}}<ref>Derived by entering source coordinates in ].</ref>
| mouth_location =
| mouth = ]
| mouth_region =
| mouth_location = ]
| mouth_country =
| mouth_coordinates = {{coord|64|55|45|N|161|08|03|W|display=inline,title}}<ref name="gnis">{{cite web | work = Geographic Names Information System| publisher = United States Geological Survey | date = January 1, 2000| url = {{gnis3|1404983}} | title = Koyuk River| accessdate = September 26, 2013}}</ref>
| mouth_elevation_imperial =
| mouth_elevation = {{convert|0|ft|abbr=on}}<ref name="gnis"/>
| mouth_lat_d = 64
| progression =
| mouth_lat_m = 55
| river_system =
| mouth_lat_s = 45
| basin_size =
| mouth_lat_NS =N
| tributaries_left =
| mouth_long_d = 161
| tributaries_right =
| mouth_long_m = 08
| custom_label =
| mouth_long_s = 03
| mouth_long_EW = W | custom_data =
| extra =
| mouth_coordinates_note =
<!-- *** Dimensions *** -->
| length_imperial =
| length_note =
| watershed_imperial =
| watershed_note =
| discharge_imperial =
| discharge_location =
| discharge_note =
| discharge_max_imperial =
| discharge_min_imperial =
<!-- *** Map section *** -->
| map =
| map_size = 300
| map_caption =
|map_alt =
| map1 = Alaska Locator Map.PNG
| map1_size = 300
| map1_caption = Location of the mouth of the Koyuk River in Alaska
| map1_locator = Alaska
|map1_alt =
}} }}


The '''Koyuk River''' (also spelled, '''Kuyuk''')<ref name=Burch2005 /> is a ] on the ] of western ], US.<ref>USGS Geographic Names Information System (GNIS). Accessed Aug 20, 2007.</ref> The river originates in the interior of the peninsula, at the ] of the ], where it flows southeast towards the mouth of ] on ]. The native village of ] is located at its mouth. The two major tributaries are the Peace and Salmon Rivers; other tributaries include Dime and Sweepstakes.<ref name="Smith1917">{{cite book|last=Smith|first=Sumner Stewart|title=The mining industry in the territory of Alaska during the calendar year 1916|url=http://books.google.com/books?id=fJf3VTPlYtEC&pg=PA56|accessdate=27 March 2013|edition=Public domain|year=1917|publisher=Govt. Print. Off.|pages=56–}} </ref> The '''Koyuk River''' (also spelled, '''Kuyuk''')<ref name=Burch2005 /> (]: ''Kuuyuk''; ]: ''Kuiguk'') is a ] on the ] of western ], in the United States.<ref name="gnis"/> The river originates in the interior of the peninsula, at the ] of the ], where it flows southeast towards the mouth of ] on ]. The native village of ] is located at its mouth. The two major tributaries are the Peace and Salmon rivers; other tributaries include Dime and Sweepstakes.<ref name="Smith1917">{{cite book|last=Smith|first=Sumner Stewart|title=The mining industry in the territory of Alaska during the calendar year 1916|url=https://books.google.com/books?id=fJf3VTPlYtEC&pg=PA56|accessdate=27 March 2013|edition=Public domain|year=1917|publisher=Govt. Print. Off.|pages=56–}} </ref>


==Etymology== ==Etymology==
Its ] named as Tebenkof Eskimos, reported by ] (1852, map 2), IRN, as ''Kvyguk'' or ''Kvieguk''. The Western Union Telegraph Expedition spelled the name ''Koikpak'' ("big river"). The Seward map of 1867 gives ''Koipak'', and later as ''Kayuk'', ''Koyuk'', and ''Kuyuk''. The Kanguksuk is also known as the ''Left Fork of the Kviguk'' (Koyuk). The present spelling comes from ]', 1900 ].<ref name="Bulletin1902">{{cite book|title=Bulletin of the United States Geological Survey|url=http://books.google.com/books?id=WUHwAAAAMAAJ&pg=PA251|accessdate=23 March 2013|edition=Public domain|year=1902|publisher=U.S. Government Printing Office|pages=251–}}</ref><ref name="Baker1902">{{cite book|author=Baker, Marcus |title=Geographic Dictionary of Alaska|url=http://books.google.com/books?id=F2auJ_2ft0kC&pg=PA251|year=1902|publisher=U.S. Government vffice|pages=251–}}</ref> Its ] named as Tebenkof Eskimos, reported by ] (1852, map 2), IRN, as ''Kvyguk'' or ''Kvieguk''. The Western Union Telegraph Expedition spelled the name ''Koikpak'' ("big river"). The Seward map of 1867 gives ''Koipak'', and later as ''Kayuk'', ''Koyuk'', and ''Kuyuk''. The Kanguksuk is also known as the ''Left Fork of the Kviguk'' (Koyuk). The present spelling comes from ]', 1900 ].<ref name="Bulletin1902">{{cite book|title=Bulletin of the United States Geological Survey|url=https://books.google.com/books?id=WUHwAAAAMAAJ&pg=PA251|accessdate=23 March 2013|edition=Public domain|year=1902|publisher=U.S. Government Printing Office|pages=251–}}</ref><ref name="Baker1902">{{cite book|author=Baker, Marcus |title=Geographic Dictionary of Alaska|url=https://books.google.com/books?id=F2auJ_2ft0kC&pg=PA251|year=1902|publisher=U.S. Government vffice|pages=251–}}</ref>


==Geography== ==Geography==
The Koyuk River, one of the largest in the ],<ref name="BrooksAbbe1906">{{cite book|author1=Brooks, Alfred Hulse; Abbe, Cleveland and Goode, Richard Urquhart |title=The Geography and Geology of Alaska: A Summary of Existing Knowledge|url=http://books.google.com/books?id=UF4SAAAAYAAJ&pg=PA93|year=1906|publisher=U.S. Government Printing Office|pages=93–}}</ref><ref name="Bulletin1911">{{cite book|author=Geological Survey (U.S.)|title=Bulletin – United States Geological Survey|url=http://books.google.com/books?id=mh4qAQAAIAAJ&pg=RA1-PA10|accessdate=27 March 2013|edition=Public domain|year=1911|publisher=The Survey|pages=10–}}</ref> originates in a lake (no designated name) bounded on the north by the ], in the upper reaches of the Seaward Island, in Northwest Alaska.<ref name="DeVaughn2011">{{cite book|author=DeVaughn, Melissa |title=Alaska AdventureGuide|url=http://books.google.com/books?id=fqpw0kZuIRgC&pg=PA69|year=2011|publisher=Menasha Ridge Press|isbn=978-0-89732-907-1|pages=69–60}}</ref> The upper reach is also reported as being made up of flat lava fields to the north of the mountains.<ref name="Geological Survey Bulletin">{{cite book|title=Geological Survey Bulletin|url=http://books.google.com/books?id=1pgJO0twQmMC&pg=RA1-PA7|year=1913|publisher=U.S. Government Printing Office|pages=1–}}</ref> The Koyuk River, one of the largest in the ],<ref name="BrooksAbbe1906">{{cite book|author1=Brooks, Alfred Hulse |author2=Abbe, Cleveland |author3=Goode, Richard Urquhart |title=The Geography and Geology of Alaska: A Summary of Existing Knowledge|url=https://books.google.com/books?id=UF4SAAAAYAAJ&pg=PA93|year=1906|publisher=U.S. Government Printing Office|pages=93–}}</ref><ref name="Bulletin1911">{{cite book|author=Geological Survey (U.S.)|title=Bulletin – United States Geological Survey|url=https://archive.org/details/bulletinuniteds09usgoog|accessdate=27 March 2013|edition=Public domain|year=1911|publisher=The Survey|pages=–}}</ref> originates in a lake (no designated name) bounded on the north by the ], in the upper reaches of the ], in Northwest Alaska.<ref name="DeVaughn2011">{{cite book|author=DeVaughn, Melissa |title=Alaska AdventureGuide|url=https://books.google.com/books?id=fqpw0kZuIRgC&pg=PA69|year=2011|publisher=Menasha Ridge Press|isbn=978-0-89732-907-1|pages=69–60}}</ref> The upper reach is also reported as being made up of flat lava fields to the north of the mountains.<ref name="Geological Survey Bulletin">{{cite book|title=Geological Survey Bulletin|url=https://books.google.com/books?id=1pgJO0twQmMC&pg=RA1-PA7|year=1913|publisher=U.S. Government Printing Office|pages=1–}}</ref>


The river joins the ] after flowing for a length of {{convert|150|miles}}; after taking a sharp turn {{convert|25|miles}} before debouching into the tidal estuary of Norton bay subsequent to its confluence with the East Fork Koyuk, near Kuyuk village. The last stretch of the river,<ref name="DeVaughn2011"/> is in a southeasterly direction as it joins the bay,<ref name="Geological Survey Bulletin"/> and flows through the ] ] area. The catchment in the middle and upper reaches has a horse-shoe shape, and the hills surrounding the valley lie in an elevation range of {{convert|2000|-|3000|ft}}; the two prominent mountains are the Bendeleben Mountains and ], the latter named after the granite geological formations. The {{convert|115|mi|km|adj=on}} long river flows southeast for {{convert|90|mi|km}}, then south for another {{convert|25|mi|km}}.<ref name="gnis"/> The river empties into Norton Bay, which it enters via a tidal estuary downstream of the river's confluence with the East Fork Koyuk River near the village of Koyuk. The last stretch of the river,<ref name="DeVaughn2011"/> is in a southeasterly direction as it joins the bay,<ref name="Geological Survey Bulletin"/> and flows through the ] ] area. The catchment in the middle and upper reaches has a horse-shoe shape, and the hills surrounding the valley lie in an elevation range of {{convert|2000|to|3000|ft|m}}; the two prominent mountains are the Bendeleben Mountains and ], the latter named after the granite geological formations.


In its initial reaches, the river has steep slopes with rapids in the upper most reaches having shallow depth of flows. The river widens as it flows down with more flow additions from tributaries which join it and the width of the river attains even {{convert|820|ft|abbr=on}}, with slow moving stretch of the river recording {{convert|5|ft}} depth of water.<ref name="DeVaughn2011"/> On both banks of the river rock exposures derived lava flows are bedded on a horizontal direction; the rockfall from these exposures has filled the river bed with boulders.<ref name="Brooks1901">{{cite book|last1=Brooks|first1=Alfred Hulse|last2=Collier|first2=Arthur James|last3=Mendenhall|first3=Walter Curran|coauthors=George Burr Richardson|editor=Geological Survey (U.S.)|title=Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900|url=http://books.google.com/books?id=DZYRAAAAIAAJ&pg=PA191|accessdate=23 March 2013|edition=Public domain|year=1901|publisher=Government Printing Office|pages=191, 198, 212–}}</ref> While the lava beds were noted in the upper region of the river and also in the valley, geological formations in the valley were mapped by ], the fifth director of the ]. He reported these formations as ] of ] or ] age.<ref name="(U.S.)1902">{{cite book|author=Geological Survey (U.S.)|title=Professional paper – United States Geological Survey|url=http://books.google.com/books?id=AEURAAAAIAAJ&pg=RA1-PA25|year=1902|publisher=The Survey|pages=1–}}</ref> ], ], and radioactive minerals were reported by the ] in 1973, as well as lode and placer claims, along a {{convert|10|miles}} wide stretch of the river.<ref name="Service1980">{{cite book|author=United States. Heritage Conservation and Recreation Service|title=A proposal for protection of eleven Alaskan rivers|url=http://books.google.com/books?id=eVPwAAAAMAAJ|year=1980|publisher=The Service|page=63}}</ref> In its initial reaches, the river has steep slopes with rapids in the upper most reaches having shallow depth of flows. The river widens as it flows down with more flow additions from tributaries which join it and the width of the river attains {{convert|820|ft|m}}, with a slow moving stretch of the river recording a {{convert|5|ft|m|adj=on}} depth of water.<ref name="DeVaughn2011"/> On both banks of the river rock exposures derived lava flows are bedded on a horizontal direction; the rockfall from these exposures has filled the river bed with boulders.<ref name="Brooks1901">{{cite book|last1=Brooks|first1=Alfred Hulse|last2=Collier|first2=Arthur James|last3=Mendenhall|first3=Walter Curran|author4=George Burr Richardson|editor=Geological Survey (U.S.)|title=Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900|url=https://archive.org/details/reconnaissances00mendgoog|accessdate=23 March 2013|edition=Public domain|year=1901|publisher=Government Printing Office|pages=, 198, 212–}}</ref> While the lava beds were noted in the upper region of the river and also in the valley, geological formations in the valley were mapped by ], the fifth director of the ]. He reported these formations as ] of ] or ] age.<ref name="(U.S.)1902">{{cite book|author=Geological Survey (U.S.)|title=Professional paper – United States Geological Survey|url=https://books.google.com/books?id=AEURAAAAIAAJ&pg=RA1-PA25|year=1902|publisher=The Survey|pages=1–}}</ref> ], ], and radioactive minerals were reported by the ] in 1973, as well as lode and placer claims, along a {{convert|10|mi|km|adj=on}} wide stretch of the river.<ref name="Service1980">{{cite book|author=United States. Heritage Conservation and Recreation Service|title=A proposal for protection of eleven Alaskan rivers|url=https://books.google.com/books?id=eVPwAAAAMAAJ|year=1980|publisher=The Service|page=63}}</ref>


;Basin ;Basin
The river becomes a broad estuary subject to tidal effect extending for long stretch upstream forming a flat mud- and sand-filled basin. The basin area measure approximately {{convert|2000|sqmi}}.<ref name="Reclamation1952">{{cite book|author=United States. Bureau of Reclamation|title=Alaska: A Reconnaissance Report on the Potential Development of Water Resources in the Territory of Alaska for Irrigation, Power Production, and Other Beneficial Uses|url=http://books.google.com/books?id=i0_oAAAAMAAJ|year=1952|publisher=U.S. Government Printing Office|page=172}}</ref> The ] is located in the uppermost part of the basin. Its drainage includes southeastern Seward Peninsula through Norton Bay. The river becomes a broad estuary subject to tidal effect extending for long stretch upstream forming a flat mud- and sand-filled basin. The basin area measure approximately {{convert|2000|sqmi}}.<ref name="Reclamation1952">{{cite book|author=United States. Bureau of Reclamation|title=Alaska: A Reconnaissance Report on the Potential Development of Water Resources in the Territory of Alaska for Irrigation, Power Production, and Other Beneficial Uses|url=https://books.google.com/books?id=i0_oAAAAMAAJ|year=1952|publisher=U.S. Government Printing Office|page=172}}</ref> The Bering Land Bridge National Preserve is in the uppermost part of the basin. Its drainage includes southeastern Seward Peninsula through Norton Bay.


==History== ==History==
A study of the archaeological remains at the Lyatayak site, south of ] and south of Koyuk, indicated that the area was inhabited 6000 to 8000 years ago.<ref name="DeVaughn2011"/> The recorded history of Koyuk is traced to Lieutenant L.A. Zagoskin of the ] during the 1840s. In 1865, William Wennis of the ] Telegraph expedition reported that the Koyuk was deserted on account of possibly the ] epidemic wiping out the entire population of the village and that the village had been abandoned for 13 years. The ]-speaking<ref name="Sturtevant1978">{{cite book|last=Sturtevant|first=William C|title=Handbook of North American Indians: Arctic|url=http://books.google.com/books?id=kGWuMa6sRYsC&pg=PA303|year=1978|publisher=Government Printing Office|isbn=978-0-16-004580-6|pages=303–}}</ref> Unali Eskimos and the Melemute Eskimos resettled in Koyuk during the 1860s to take advantage of ] herding. In 1879, a trading post for furs was established at the river's mouth by the ].<ref name="Bockstoce2009">{{cite book|last=Bockstoce|first=John R.|title=Furs and Frontiers In the Far North: The Contest Among Native and Foreign Nations for the Bering Strait Fur Trade|url=http://books.google.com/books?id=HY6LvFMSxxwC&pg=PA306|year=2009|publisher=Yale University Press|isbn=978-0-300-15490-0|pages=306–}}</ref> During the gold rush, there was intense activity in the region but hardly any gold was found though claims had been staked at many places within the Koyuk River valley. By 1900, the village had declined to the level of subsistence economy, depending on fishing and hunting caribou and moose and picking on berries.<ref name="DeVaughn2011"/> A study of the archaeological remains at the Lyatayak site, south of ] and south of Koyuk, indicated that the area was inhabited 6000 to 8000 years ago.<ref name="DeVaughn2011"/> The recorded history of Koyuk is traced to Lieutenant L.A. Zagoskin of the ] during the 1840s. In 1865, William Wennis of the ] Telegraph expedition reported that the Koyuk was deserted on account of possibly the ] epidemic wiping out the entire population of the village and that the village had been abandoned for 13 years. The ]-speaking<ref name="Sturtevant1978">{{cite book|last=Sturtevant|first=William C|title=Handbook of North American Indians: Arctic|url=https://archive.org/details/handbookofnorth010stur|url-access=registration|year=1978|publisher=Government Printing Office|isbn=978-0-16-004580-6|pages=–}}</ref> Unali Eskimos and the Melemute Eskimos resettled in Koyuk during the 1860s to take advantage of ] herding. In 1879, a trading post for furs was established at the river's mouth by the ].<ref name="Bockstoce2009">{{cite book|last=Bockstoce|first=John R.|title=Furs and Frontiers In the Far North: The Contest Among Native and Foreign Nations for the Bering Strait Fur Trade|url=https://books.google.com/books?id=HY6LvFMSxxwC&pg=PA306|year=2009|publisher=Yale University Press|isbn=978-0-300-15490-0|pages=306–}}</ref> During the gold rush, there was intense activity in the region but hardly any gold was found though claims had been staked at many places within the Koyuk River valley. By 1900, the village had declined to the level of subsistence economy, depending on fishing and hunting caribou and moose and picking on berries.<ref name="DeVaughn2011"/>


==Wildlife== ==Wildlife==
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Under the Alaska National Interest Lands Conservation Act (ANILCA) (P.L 96-487) the Koyuk River is categorized as "Freshwater Aquatic Herbaceous" and is one out of 25 nominated as the National Wild and Scenic Rivers. The river and the basin draining it is rich of wild life species, which consists of five fish species, 22 mammals species and 46 bird species.<ref name=Wildlife>{{Cite web|url=https://docs.google.com/viewer?a=v&q=cache:hLfJUv5KFqcJ:www.blm.gov/pgdata/etc/medialib/blm/ak/aktest/ofr.Par.12274.File.dat/OFR%252018.pdf+Koyuk+River&hl=en&gl=in&pid=bl&srcid=ADGEESgeRYsKgrXyP76lNF_rNASVmfDtbjEfGPh8A7n7yXWAoLATAh4jsoYQflmJzGdoyTd2wUlIh1yMcJ3IFo7k0IfAYLN_ele2aJLqeHfA1LAKjjbFh8wFkLRRTLs-5Mp-Erw8zzXr&sig=AHIEtbShn6vRqUMJDURrNKR8Nuc-qn2doA|title=Wildlife of the Koyuk Watershed|accessdate=26 March 2013|publisher=Bureau of Land Management, Alaska}}</ref> Under the Alaska National Interest Lands Conservation Act (ANILCA) (P.L 96-487) the Koyuk River is categorized as "Freshwater Aquatic Herbaceous" and is one out of 25 nominated as the National Wild and Scenic Rivers. The river and the basin draining it is rich of wild life species, which consists of five fish species, 22 mammals species and 46 bird species.<ref name=Wildlife>{{Cite web|url=https://docs.google.com/viewer?a=v&q=cache:hLfJUv5KFqcJ:www.blm.gov/pgdata/etc/medialib/blm/ak/aktest/ofr.Par.12274.File.dat/OFR%252018.pdf+Koyuk+River&hl=en&gl=in&pid=bl&srcid=ADGEESgeRYsKgrXyP76lNF_rNASVmfDtbjEfGPh8A7n7yXWAoLATAh4jsoYQflmJzGdoyTd2wUlIh1yMcJ3IFo7k0IfAYLN_ele2aJLqeHfA1LAKjjbFh8wFkLRRTLs-5Mp-Erw8zzXr&sig=AHIEtbShn6vRqUMJDURrNKR8Nuc-qn2doA|title=Wildlife of the Koyuk Watershed|accessdate=26 March 2013|publisher=Bureau of Land Management, Alaska}}</ref>


The flora of the river watershed, in their descending order of distribution are: closed needleleaf forest dominating the ]; closed tall shrub scrub is also part of the riparian zone, and open-air low shrub scrub with willows and grasses as dominant vegetation. The wet ] herbaceous habitat lies between the river riparian and higher ground. The ] graminoid herbaceous forms the hilly ] tundra.<ref name=Wildlife/> The dominant vegetation in the valley is of tundras, except in the basin area below Knowles Creek, where it consists of tree species of ], ] and ].<ref name="DeVaughn2011"/> The flora of the river watershed, in their descending order of distribution are: closed needleleaf forest dominating the ]; closed tall shrub scrub is also part of the riparian zone, and open-air low shrub scrub with willows and grasses as dominant vegetation. The wet ] herbaceous habitat lies between the river riparian and higher ground. The ] graminoid herbaceous forms the hilly ] tundra.<ref name=Wildlife/> The dominant vegetation in the valley is of tundras, except in the basin area below Knowles Creek, where it consists of tree species of ], ] and ].<ref name="DeVaughn2011"/>


The river is well known for its fishing resources. the fish species reported are ] (''Oncorhynchus tshawytscha''), ] (''Oncorhynchus nerka''), ] (''Oncorhynchus kisutch''), ] (''Oncorhynchus mykiss''), ] (''Salvelinus malma''), ], ] (''Esox lucius''), ] (''Thymallus thymallus''), ] (''Salvelinus malma malma''), ], ] (''Oncorhynchus mykiss'') and ] (''Salvelinus alpinus'').<ref name=Wildlife/><ref name=fish>{{Cite web|url=http://www.alaskansportsman.com/fishing/rivers/Koyuk_River.php|title=Koyuk River Hunting and Fishing...Enjoy One Of The Many Scenic Rivers in Alaska!|accessdate=26 March 2013|publisher= Alaska Fishing and Hunting Guides Directory}}</ref> Some of the important mammals reported in the river basin are ] ('']''), ] (''Ursus arctos horribilis''), ] (''Ursus americanus''), ] (''Rangifer tarandus''), ] (''Canis lupus''), ], ], ], and ] (''Lepus americanus'').<ref name=Wildlife/><ref name=fish/> Some of the important bird species reported in the river watershed are: ]s, ]s, ], ], ], ravens, ], ], ] and ].<ref name=Wildlife/> The river is well known for its fishing resources. the fish species reported are ] (''Oncorhynchus tshawytscha''), ] (''Oncorhynchus nerka''), ] (''Oncorhynchus kisutch''), ] (''Oncorhynchus mykiss''), ] (''Salvelinus malma''), ] (''Esox lucius''), ] (''Thymallus thymallus''), ] (''Salvelinus malma malma''), and ] (''Salvelinus alpinus'').<ref name=Wildlife/><ref name=fish>{{Cite web|url=http://www.alaskansportsman.com/fishing/rivers/Koyuk_River.php|title=Koyuk River Hunting and Fishing...Enjoy One Of The Many Scenic Rivers in Alaska!|accessdate=26 March 2013|publisher=Alaska Fishing and Hunting Guides Directory|archive-url=https://archive.today/20130410122542/http://www.alaskansportsman.com/fishing/rivers/Koyuk_River.php|archive-date=10 April 2013|url-status=dead}}</ref> Some of the important mammals reported in the river basin are ] ('']''), ] (''Ursus arctos horribilis''), ] (''Ursus americanus''), ] (''Rangifer tarandus''), ] (''Canis lupus''), ], ], ], and ] (''Lepus americanus'').<ref name=Wildlife/><ref name=fish/> Some of the important bird species reported in the river watershed are: ]s, ]s, ], ], ], ravens, ], ], ] and ].<ref name=Wildlife/>


==Tourism== ==Tourism==
There are a network of trails in the basin, prominent among these are the Koyuk River-Buckland route and the Koyuk-Kiwalik route.<ref name="Burch2005">{{cite book|first=Ernest S. |last=Burch|title=Alliance and Conflict: The World System of the Inũpiaq Eskimos|url=http://books.google.com/books?id=Wt-FXgSxRCYC&pg=PT296|year=2005|publisher=U of Nebraska Press|isbn=978-0-8032-6238-6|pages=276, 296–}}</ref> The river is also popular for water sports such as ] and ].<ref name=fish/> There are a network of trails in the basin, prominent among these are the Koyuk River-Buckland route and the Koyuk-Kiwalik route.<ref name="Burch2005">{{cite book|first=Ernest S. |last=Burch|title=Alliance and Conflict: The World System of the Inũpiaq Eskimos|url=https://books.google.com/books?id=Wt-FXgSxRCYC&pg=PT296|year=2005|publisher=U of Nebraska Press|isbn=978-0-8032-6238-6|pages=276, 296–}}</ref> The river is also popular for water sports such as ] and ].<ref name=fish/>

==See also==
*]


==References== ==References==
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*{{Source-attribution|U.S. Geological Survey's "Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900" (1901)}} *{{Source-attribution|U.S. Geological Survey's "Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900" (1901)}}
*{{Source-attribution|S.S. Smith's "The mining industry in the territory of Alaska during the calendar year 1916" (1917)}} *{{Source-attribution|S.S. Smith's "The mining industry in the territory of Alaska during the calendar year 1916" (1917)}}
{{reflist}} {{reflist|30em}}


{{authority control}}
==See also==
*]


] ]
] ]
]
]

Latest revision as of 17:59, 29 May 2023

River in Alaska, United States
Koyuk River
Kuyuk
Part of the Bering Land Bridge National Preserve, in the Koyuk River Valley
Koyuk River is located in AlaskaKoyuk RiverLocation of the mouth of the Koyuk River in Alaska
Native nameKuuyuk (Inuit)
Location
CountryUnited States
StateAlaska
DistrictNome Census Area
Physical characteristics
Sourcesmall lake 3 miles (4.8 km) north of Kuzitrin Lake
 • locationBering Land Bridge National Preserve, Seward Peninsula
 • coordinates65°25′44″N 163°13′00″W / 65.42889°N 163.21667°W / 65.42889; -163.21667
 • elevation1,526 ft (465 m)
MouthNorton Bay
 • locationKoyuk
 • coordinates64°55′45″N 161°08′03″W / 64.92917°N 161.13417°W / 64.92917; -161.13417
 • elevation0 ft (0 m)
Length115 mi (185 km)

The Koyuk River (also spelled, Kuyuk) (Inupiaq: Kuuyuk; Yup'ik: Kuiguk) is a river on the Seward Peninsula of western Alaska, in the United States. The river originates in the interior of the peninsula, at the Lost Jim Lava Flow of the Bering Land Bridge National Preserve, where it flows southeast towards the mouth of Norton Bay on Norton Sound. The native village of Koyuk is located at its mouth. The two major tributaries are the Peace and Salmon rivers; other tributaries include Dime and Sweepstakes.

Etymology

Its Inuit named as Tebenkof Eskimos, reported by Captain Tebenkov (1852, map 2), IRN, as Kvyguk or Kvieguk. The Western Union Telegraph Expedition spelled the name Koikpak ("big river"). The Seward map of 1867 gives Koipak, and later as Kayuk, Koyuk, and Kuyuk. The Kanguksuk is also known as the Left Fork of the Kviguk (Koyuk). The present spelling comes from Alfred Hulse Brooks', 1900 United States Geological Survey.

Geography

The Koyuk River, one of the largest in the Seward Peninsula, originates in a lake (no designated name) bounded on the north by the Bendeleben Mountains, in the upper reaches of the Bering Land Bridge National Preserve, in Northwest Alaska. The upper reach is also reported as being made up of flat lava fields to the north of the mountains.

The 115-mile (185 km) long river flows southeast for 90 miles (140 km), then south for another 25 miles (40 km). The river empties into Norton Bay, which it enters via a tidal estuary downstream of the river's confluence with the East Fork Koyuk River near the village of Koyuk. The last stretch of the river, is in a southeasterly direction as it joins the bay, and flows through the tundra wetland area. The catchment in the middle and upper reaches has a horse-shoe shape, and the hills surrounding the valley lie in an elevation range of 2,000 to 3,000 feet (610 to 910 m); the two prominent mountains are the Bendeleben Mountains and Domes of Granite Mountain, the latter named after the granite geological formations.

In its initial reaches, the river has steep slopes with rapids in the upper most reaches having shallow depth of flows. The river widens as it flows down with more flow additions from tributaries which join it and the width of the river attains 820 feet (250 m), with a slow moving stretch of the river recording a 5-foot (1.5 m) depth of water. On both banks of the river rock exposures derived lava flows are bedded on a horizontal direction; the rockfall from these exposures has filled the river bed with boulders. While the lava beds were noted in the upper region of the river and also in the valley, geological formations in the valley were mapped by Walter Curran Mendenhall, the fifth director of the US Geological Survey. He reported these formations as basalts of Pleistocene or Late Pleistocene age. Gold, platinum, and radioactive minerals were reported by the U.S. Bureau of Mines in 1973, as well as lode and placer claims, along a 10-mile (16 km) wide stretch of the river.

Basin

The river becomes a broad estuary subject to tidal effect extending for long stretch upstream forming a flat mud- and sand-filled basin. The basin area measure approximately 2,000 square miles (5,200 km). The Bering Land Bridge National Preserve is in the uppermost part of the basin. Its drainage includes southeastern Seward Peninsula through Norton Bay.

History

A study of the archaeological remains at the Lyatayak site, south of Cape Denbigh and south of Koyuk, indicated that the area was inhabited 6000 to 8000 years ago. The recorded history of Koyuk is traced to Lieutenant L.A. Zagoskin of the Imperial Russian Navy during the 1840s. In 1865, William Wennis of the Western Union Telegraph expedition reported that the Koyuk was deserted on account of possibly the smallpox epidemic wiping out the entire population of the village and that the village had been abandoned for 13 years. The Yupik-speaking Unali Eskimos and the Melemute Eskimos resettled in Koyuk during the 1860s to take advantage of caribou herding. In 1879, a trading post for furs was established at the river's mouth by the Alaska Commercial Company. During the gold rush, there was intense activity in the region but hardly any gold was found though claims had been staked at many places within the Koyuk River valley. By 1900, the village had declined to the level of subsistence economy, depending on fishing and hunting caribou and moose and picking on berries.

Wildlife

Caribou reindeer

Under the Alaska National Interest Lands Conservation Act (ANILCA) (P.L 96-487) the Koyuk River is categorized as "Freshwater Aquatic Herbaceous" and is one out of 25 nominated as the National Wild and Scenic Rivers. The river and the basin draining it is rich of wild life species, which consists of five fish species, 22 mammals species and 46 bird species.

The flora of the river watershed, in their descending order of distribution are: closed needleleaf forest dominating the riparian zone; closed tall shrub scrub is also part of the riparian zone, and open-air low shrub scrub with willows and grasses as dominant vegetation. The wet graminoid herbaceous habitat lies between the river riparian and higher ground. The mesic graminoid herbaceous forms the hilly tussock tundra. The dominant vegetation in the valley is of tundras, except in the basin area below Knowles Creek, where it consists of tree species of willows, spruce and birch.

The river is well known for its fishing resources. the fish species reported are Chinook salmon (Oncorhynchus tshawytscha), sockeye salmon (Oncorhynchus nerka), coho salmon (Oncorhynchus kisutch), steelhead/rainbow trout (Oncorhynchus mykiss), Dolly Varden trout (Salvelinus malma), northern pike (Esox lucius), grayling (Thymallus thymallus), Dolly Varden trout (Salvelinus malma malma), and Arctic char (Salvelinus alpinus). Some of the important mammals reported in the river basin are moose (Alces alces), grizzly bear (Ursus arctos horribilis), black bear (Ursus americanus), caribou (Rangifer tarandus), wolves (Canis lupus), lynx, red fox, beaver, and snowshoe hare (Lepus americanus). Some of the important bird species reported in the river watershed are: bald eagles, glaucous gulls, spruce grouse, northern flying squirrel, song birds, ravens, waterfowl, lesser golden-plover, whimbrel and Lapland longspur.

Tourism

There are a network of trails in the basin, prominent among these are the Koyuk River-Buckland route and the Koyuk-Kiwalik route. The river is also popular for water sports such as kayaking and rafting.

See also

References

  • Public Domain This article incorporates text from this source, which is in the public domain: U.S. Government's Printing Office's "Bulletin of the United States Geological Survey" (1902)
  • Public Domain This article incorporates text from this source, which is in the public domain: U.S. Geological Survey's "Bulletin – United States Geological Survey" (1911)
  • Public Domain This article incorporates text from this source, which is in the public domain: U.S. Geological Survey's "Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900" (1901)
  • Public Domain This article incorporates text from this source, which is in the public domain: S.S. Smith's "The mining industry in the territory of Alaska during the calendar year 1916" (1917)
  1. ^ "Koyuk River". Geographic Names Information System. United States Geological Survey. January 1, 2000. Retrieved September 26, 2013.
  2. Derived by entering source coordinates in Google Earth.
  3. ^ Burch, Ernest S. (2005). Alliance and Conflict: The World System of the Inũpiaq Eskimos. U of Nebraska Press. pp. 276, 296–. ISBN 978-0-8032-6238-6.
  4. Smith, Sumner Stewart (1917). The mining industry in the territory of Alaska during the calendar year 1916 (Public domain ed.). Govt. Print. Off. pp. 56–. Retrieved 27 March 2013. full text
  5. Bulletin of the United States Geological Survey (Public domain ed.). U.S. Government Printing Office. 1902. pp. 251–. Retrieved 23 March 2013.
  6. Baker, Marcus (1902). Geographic Dictionary of Alaska. U.S. Government vffice. pp. 251–.
  7. Brooks, Alfred Hulse; Abbe, Cleveland; Goode, Richard Urquhart (1906). The Geography and Geology of Alaska: A Summary of Existing Knowledge. U.S. Government Printing Office. pp. 93–.
  8. Geological Survey (U.S.) (1911). Bulletin – United States Geological Survey (Public domain ed.). The Survey. pp. 10–. Retrieved 27 March 2013.
  9. ^ DeVaughn, Melissa (2011). Alaska AdventureGuide. Menasha Ridge Press. pp. 69–60. ISBN 978-0-89732-907-1.
  10. ^ Geological Survey Bulletin. U.S. Government Printing Office. 1913. pp. 1–.
  11. Brooks, Alfred Hulse; Collier, Arthur James; Mendenhall, Walter Curran; George Burr Richardson (1901). Geological Survey (U.S.) (ed.). Reconnaissances in the Cape Nome and Norton Bay regions, Alaska, in 1900 (Public domain ed.). Government Printing Office. pp. 191, 198, 212–. Retrieved 23 March 2013.
  12. Geological Survey (U.S.) (1902). Professional paper – United States Geological Survey. The Survey. pp. 1–.
  13. United States. Heritage Conservation and Recreation Service (1980). A proposal for protection of eleven Alaskan rivers. The Service. p. 63.
  14. United States. Bureau of Reclamation (1952). Alaska: A Reconnaissance Report on the Potential Development of Water Resources in the Territory of Alaska for Irrigation, Power Production, and Other Beneficial Uses. U.S. Government Printing Office. p. 172.
  15. Sturtevant, William C (1978). Handbook of North American Indians: Arctic. Government Printing Office. pp. 303–. ISBN 978-0-16-004580-6.
  16. Bockstoce, John R. (2009). Furs and Frontiers In the Far North: The Contest Among Native and Foreign Nations for the Bering Strait Fur Trade. Yale University Press. pp. 306–. ISBN 978-0-300-15490-0.
  17. ^ "Wildlife of the Koyuk Watershed". Bureau of Land Management, Alaska. Retrieved 26 March 2013.
  18. ^ "Koyuk River Hunting and Fishing...Enjoy One Of The Many Scenic Rivers in Alaska!". Alaska Fishing and Hunting Guides Directory. Archived from the original on 10 April 2013. Retrieved 26 March 2013.
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