Skip to content
Surf Wiki
Save to docs
general/rivers-of-washington-state

From Surf Wiki (app.surf) — the open knowledge base

Stillaguamish River

River in Washington, United States

Stillaguamish River

River in Washington, United States

FieldValue
nameStillaguamish River
imageStillaguamish River 39160.JPG
image_captionThe South Fork of the Stillaguamish River near Verlot
image_size300
pushpin_mapWashington#USA
pushpin_map_size300
pushpin_map_captionLocation of the mouth of the Stillaguamish River in Washington
subdivision_type1Country
subdivision_name1United States
subdivision_type2State
subdivision_name2Washington
length67 mi
source1North Cascades
source1_coordinates
mouthPuget Sound
mouth_locationPort Susan
mouth_coordinates
mouth_elevation0 m
basin_size700 sqmi

The Stillaguamish River is a river in the northwestern region of the U.S. state of Washington. It is mainly composed of two forks, the longer North Fork Stillaguamish (45 mi) and the South Fork Stillaguamish. The two forks join near Arlington. From there the Stillaguamish River proper flows for 22 mi to Puget Sound. The river's watershed drains part of the Cascade Range north of Seattle.

Name

The Stillaguamish River's name is derived from the Stillaguamish people, the Lushootseed-speaking people who had several villages along the river's course. Their name, Stillaguamish, is derived from their Lushootseed endonym, , meaning "river people."

Variant spellings of the Stillaguamish River, according to the USGS, include Stoh-luk-whahmpsh River, Steilaguamish River, and Stalukahamish River.

Course

North Fork Valley west of Darrington

The Stillaguamish River is formed from the confluence of the North and South Forks, both of which rise in the Cascades. Between the North and South forks there is a portion of the Mount Baker-Snoqualmie National Forest called the Boulder River Wilderness.

The North Fork rises as several branches in a remote area of Skagit County near Finney Peak, approximately 10 mi north of Darrington. Collecting many tributary creeks, the river flows south, then west through the foothills along the Skagit-Snohomish county line. Tributaries of the North Fork Stillaguamish River include Boulder River and Deer Creek.

The South Fork (30 mi) originates from the northern slopes of Del Campo Peak and Morning Star Peak in central Snohomish County, 20 mi south of Darrington, and flows west and northwest by Silverton, Verlot, and Granite Falls.

The two forks unite at Arlington in northwestern Snohomish County. The combined stream flows west before it briefly splits again to encircle the town of Silvana.

The Stillaguamish bifurcates at its delta to form Florence Island before entering Puget Sound. Hatt Slough flows southwest and is now the primary distributary of the Stillaguamish waters into Port Susan, having been diverted in the early twentieth century. The Old Stillaguamish River Channel flows northwest towards Florence and then Stanwood on an 8-mile meandering course. Near the Camano Island bridge this channel again splits, forming Leque Island, with the South Pass flowing into Port Susan and the West Pass emptying into the southern end of Skagit Bay.

Natural history

The Stillaguamish River and its tributaries are known for their salmon runs. Eight salmonid species use the streams for spawning, including Chinook, coho, chum, pink, and sockeye salmon, steelhead trout, sea-run cutthroat, and bull trout.

Hydrology

The north fork of the Stillaguamish river level is monitored by gauges operated by the United States Geological Survey (USGS), and river levels can vary by as much as 13 ft. The river level rises and falls very quickly, with the average north fork flood duration of eight hours. Of the five highest north fork flood levels on record, three have occurred since 2009.

History

The Stillaguamish River is the center of Stillaguamish territory. For centuries, the Stillaguamish have fished and hunted and gathered all along its extent. The Stillaguamish had at least ten villages along its course, from its mouth to as far upriver as Hazel and Mt. Higgins (). Other Indigenous peoples historically traveled to the Stillaguamish River to fish as well, including the Sauk, the Snohomish, and the Duwamish.

The 2014 Oso landslide occurred on the North Fork of the Stillaguamish.

On December 5, 2023, the river crested at 21.34 ft near Arlington and set a new record amid regional floods.

References

References

  1. Including North Fork
  2. {{GNIS. 1508743. Stillaguamish River
  3. (1994). "Lushootseed Dictionary". [[University of Washington Press]].
  4. (1906). "An Illustrated History of Skagit and Snohomish Counties". Interstate Publishing Company.
  5. (October 2005). "Old Stillaguamish River Channel Diel Surveys". Washington State Department of Ecology.
  6. "National Weather Service Advanced Hydrologic Prediction Service".
  7. "Historical Crests for North Fork Stillaguamish River near Arlington".
  8. Lane, Barbara. (1973). "Anthropological Report on the Identity, Treaty Status and Fisheries of the Stillaguamish Indians".
  9. Baldwin, Garth L.. (2023-03-21). "A Cultural Resources Assessment of the Amber Grove Development (TPN 31051400101800), Arlington, Snohomish County, Washington". Drayton Archaeology.
  10. Oakley, Janet. (December 31, 2007). "Arlington — Thumbnail History". [[HistoryLink]].
  11. (December 5, 2023). "Stillaguamish River flood breaks record after 6 inches of rain". [[The Everett Herald]].
  12. Zhou, Amanda. (December 7, 2023). "In tiny Silvana, flooding is a way of life. It's getting worse". [[The Seattle Times]].
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

Want to explore this topic further?

Ask Mako anything about Stillaguamish River — get instant answers, deeper analysis, and related topics.

Research with Mako

Free with your Surf account

Content sourced from Wikipedia, available under CC BY-SA 4.0.

This content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.

Report