Kuskokwim River

Kuskokwim River
Shoreline of the Kuskokwim River at Aniak
Name origin: from the Yup'ik, kusquqviim[1]
Country United States
State Alaska
District Bethel Census Area, Yukon–Koyukuk Census Area
Source confluence of the river's east and north forks
 - location near Medfra, Yukon–Koyukuk Census Area
 - elevation 3,655 ft (1,114 m) [2]
 - coordinates 63°05′16″N 154°38′33″W / 63.08778°N 154.64250°W / 63.08778; -154.64250 [3]
Mouth Kuskokwim Bay
 - location near Eek, Bethel Census Area
 - elevation 0 ft (0 m) [3]
 - coordinates 60°04′59″N 162°20′02″W / 60.08306°N 162.33389°W / 60.08306; -162.33389Coordinates: 60°04′59″N 162°20′02″W / 60.08306°N 162.33389°W / 60.08306; -162.33389 [3]
Length 702 mi (1,130 km) [4]
Basin 48,000 sq mi (124,319 km2) [5]
Discharge for mouth
 - average 67,000 cu ft/s (1,897 m3/s) [5]
Watershed of the Kuskokwim River in Alaska

The Kuskokwim River or Kusko River (Kusquqvak in Yup'ik) is a river, 702 miles (1,130 km) long, in Southwest Alaska in the United States.[4] It is the ninth largest river in the United States by average discharge volume at its mouth and seventeenth largest by basin drainage area.[6]

The river provides the principal drainage for an area of the remote Alaska Interior on the north and west side of the Alaska Range, flowing southwest into Kuskokwim Bay on the Bering Sea. The highest point in its watershed is Mount Russell. Except for its headwaters in the mountains, the river is broad and flat for its entire course, making it a useful transportation route for many types of watercraft, as well as road vehicles during the winter when it is frozen over.[7] It is the longest free flowing river in the United States.

Kuskokwim is a loose transliteration of a Yup'ik word. It is a compound word meaning big slow moving thing.

The Alaska Natives of Kuskokwim are Yup'ik Eskimo on the lower Kuskokwim, Deg Hit'an Athabaskan on the middle Kuskokwim, Upper Kuskokwim Athabaskan on the upper Kuskokwim, and Koyukon Athabaskan on the North Fork, Lake Minchumina.

Name

The river's name comes from the Yup'ik, kusquqviim, recorded by a Russian sailor in 1826.[1] An obsolete Tanana (Athabaskan) name for the river was Chin-ana.[3] Upper Kuskokwim (Kolchan) is often used to mean the people of the upper parts of the river, while Yup'ik people live along the lower river.[1]

Course

Yup'ik at Moravian Mission Station at Kuskokwim River in the year 1900

The river is formed by the confluence of East Fork Kuskokwim River and North Fork Kuskokwim River, 5 miles (8 km) east of Medfra. From there it flows southwest to Kuskokwim Bay and the Bering Sea.[3]

The Kuskokwim is fed by several forks in central and south-central Alaska. The North Fork (250 mi/400 km) rises in the Kuskokwim Mountains approximately 200 miles (320 km) WSW of Fairbanks and flows southwest in a broad valley. The South Fork (200 mi/320 km) rises in the southwestern end of the Alaska Range west of Mount Gerdine and flows north-northwest through the mountains, past Nikolai, receiving other streams that descend from the Alaska Range northwest of Denali. The two forks join near Medfra, and from there the main stem of the Kuskokwim flows southwest, past McGrath, in a remote valley between the Kuskokwim Mountains to the north and the Alaska Range to the south.

In southwest Alaska the river emerges from the Kuskokwim Mountains in a vast lake-studded alluvial plain south of the Yukon River, surrounded by vast spruce forests. It passes a series of Yup'ik villages, including Aniak, and approaches within 50 mi (80 km) of the Yukon before diverging southwest. Southwest of Bethel, the largest community on the river, it broadens into a wide marshy delta that enters Kuskokwim Bay approximately 50 mi (80 km) SSW of Bethel. The lower river below Aniak is located within the Yukon Delta National Wildlife Refuge.

The river receives the Big River from the south approximately 20 miles (32 km) southwest of Medfra. It receives the Swift, Stony, and Holitna rivers from the south at the southern end of the Kuskokwim Mountains before emerging on the coastal plain. It receives the Aniak River from the south at Aniak. Approximately 20 miles (32 km) upstream from Bethel it receives the Kisaralik and Kwethluk rivers from the south. It receives the Eek River from the east at Eek near its mouth on Kuskokwim Bay.

History

The principal economic activities along the river have historically been fur trapping and fishing. Subsistence fishing for salmon and whitefish provides a staple of the Yup'ik diet along the river. Economic deposits of placer gold were discovered in 1901 near Aniak.[8] Mineral production in the region has mainly been from scattered placer gold deposits that through 2004 had produced a total of 3.5 million troy ounces of gold.[9] The primary route of the Iditarod Trail follows the South Fork Kuskokwim River out of the Alaska Range and crosses the main stem of the river near McGrath.[10]

See also

References

  1. 1 2 3 Bright, p. 243
  2. ↑ Source elevation derived from Google Earth search using source coordinates.
  3. 1 2 3 4 5 "Kuskokwim River". Geographic Names Information System. United States Geological Survey. January 1, 2000. Retrieved May 2, 2011.
  4. 1 2 Benke and Cushing, p. 741
  5. 1 2 Benke and Cushing, p. 764
  6. ↑ Kammerer, J.C. (1990). "Largest Rivers in the United States". United States Geological Survey. Retrieved May 2, 2011.
  7. ↑ Johnson, Kirk (May 28, 2013). "Health Care Is Spread Thin on Alaskan Frontier". New York Times. Retrieved 3 June 2013.
  8. ↑ Bundtzen, T.K.; Miller, M.L. (1997). "Monograph 9: Mineral Deposits of Alaska, Precious Metals Associated with Late Cretaceous-Early Tertiary Igneous Rocks of Southwestern Alaska" (PDF). Economic Geology: 242–286.
  9. ↑ Goldfarb, Richard J.; et al. (June–July 2004). "The Late Cretaceous Donlin Creek Gold Deposit, Southwestern Alaska: Controls on Epizonal Ore Formation" (PDF). Economic Geology. 99 (4): 644. doi:10.2113/gsecongeo.99.4.643. Retrieved May 2, 2011.
  10. ↑ "Iditarod National Historic Trail Map". Bureau of Land Management. September 3, 2009. Retrieved May 2, 2011.

Works cited

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