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The Snohomish River is a river in Snohomish County, Washington, formed by the confluence of the Skykomish and Snoqualmie rivers near Monroe. It flows northwest entering Port Gardner Bay, part of Puget Sound, between Everett and Marysville. The Pilchuck River is its main tributary and joins the river at Snohomish. The river system drains the west side of the Cascade Mountains from Snoqualmie Pass to north of Stevens Pass.

Snohomish River
Snohomish River at Snohomish
Map of the Snohomish River and tributaries
Mouth of the Snohomish River in Washington
Snohomish River (the United States)
Location
CountryUnited States
StateWashington
CountySnohomish
Physical characteristics
SourceConfluence of the Skykomish River and the Snoqualmie River
  locationMonroe
  coordinates47°49′48″N 122°2′47″W[1]
MouthPuget Sound
  location
Port Gardner
  coordinates
48°1′16″N 122°12′30″W[1]
  elevation
0 m (0 ft)
Length20 mi (32 km)[2]
Basin size1,856 sq mi (4,810 km2)[3]
Discharge 
  locationNear Monroe[4]
  average9,511 cu ft/s (269.3 m3/s)[4]
  minimum763 cu ft/s (21.6 m3/s)
  maximum150,000 cu ft/s (4,200 m3/s)

Measured at Monroe, the Snohomish River has an average annual flow of 9,500 cubic feet per second (270 m3/s).[2] In comparison, the Columbia River, Washington's largest river, has an average flow of about 265,000 cubic feet per second (7,500 m3/s).[5]

Route 9 bridge, with downtown Snohomish behind
Route 9 bridge, with downtown Snohomish behind
Debris in the  November 2006 flood is swept under the Airport Way Bridge in Snohomish.
Debris in the November 2006 flood is swept under the Airport Way Bridge in Snohomish.

Course


The Snohomish River forms at the confluence of the Snoqualmie and Skykomish Rivers just west of Monroe. Both of these rivers originate in the Cascades and drain the west slopes of the mountains in southeastern Snohomish County and northeastern King County. The Snohomish River flows generally northwestward from the confluence, passing under state route 522 and flowing alongside Lord Hill Regional Park before reaching downtown Snohomish. Here, it is joined by the Pilchuck River, its main tributary, and flows under state route 9. From Snohomish, the river continues northwestward through a broad floodplain, forming the eastern boundary of the city of Everett. The final few miles of the river in Everett form the Snohomish River estuary, a river delta that features wetlands and tideflats spread out across various islands and arms of the river.[6] Several bridges carry U.S. 2, Interstate 5, and state route 529 across the delta. The river then empties into Possession Sound, which is part of Puget Sound, between Everett and Marysville.

Panoramic view of the Snohomish River from downtown Snohomish

See also



References


  1. U.S. Geological Survey Geographic Names Information System: Snohomish River
  2. Snohomish River Watershed Draft Initial Assessment Archived 2006-10-04 at the Wayback Machine
  3. Surface Water Management Division: Snohomish River Salmon Recovery
  4. USGS Snohomish River gauge near Monroe
  5. Kammerer, J.C. (May 1990). "Largest Rivers in the United States". U.S. Geological Survey. Retrieved 2008-04-01.
  6. Brennick, Charles. "Snohomish River Estuary Recreation Guide". Snohomish County Estuary. Snohomish County government. Retrieved 11 July 2019.





На других языках


[de] Snohomish River

Der Snohomish River ist ein Fluss im US-Bundesstaat Washington, welcher seinen Namen beim Zusammenfluss des Skykomish River und des Snoqualmie River in der Nähe Monroes erhält. Er fließt nordwestlicher Richtung, bis er zwischen Everett und Marysville in die Port Gardner Bay, Teil des Puget Sound, fließt. Der Pilchuck River ist sein größter Nebenfluss und mündet bei Snohomish in ihn ein. Der Snohomish River entwässert die Westseite der Kaskadenkette vom Snoqualmie Pass bis zum nördlich gelegenen Stevens Pass.
- [en] Snohomish River

[ru] Снохомиш (река)

Снохомиш (англ. Snohomish River) — река на северо-западе центральной части штата Вашингтон, США. Образуется при слиянии рек Скайкомиш и Сноукуони близ города Монро. Течёт преимущественно в северо-западном направлении и впадает в залив Порт-Гарднер (часть залива Пьюджет) близ города Эверетт. Крупнейший приток — Пилчак, текущий с севера и впадающий в реку в городе Снохомиш. Бассейн реки включает западные склоны Каскадных гор от перевала Сноукуони до местности севернее перевала Стивенс.



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