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 miles (72 km)) and the South Fork Stillaguamish. The two forks join near Arlington. From there the Stillaguamish River proper flows for 22 miles (35 km) to Puget Sound. The river's watershed drains part of the Cascade Range north of Seattle.

Stillaguamish River
The South Fork of the Stillaguamish River near Verlot
Location of the mouth of the Stillaguamish River in Washington Show map of Washington (state) Stillaguamish River (the United States) Show map of the United States
Location
Country	United States
State	Washington
Physical characteristics
Source	North Cascades
• coordinates	48°12′14″N 122°7′38″W[1]
Mouth	Puget Sound
• location	Port Susan
• coordinates	48°14′18″N 122°22′38″W[1]
• elevation	0 m (0 ft)
Length	67 mi (108 km)[2]
Basin size	700 sq mi (1,800 km2)

Course

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 miles (16 km) 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 miles (48 km)) originates from the northern slopes of Del Campo Peak and Morning Star Peak in central Snohomish County, 20 miles (32 km) 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.[3] 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.[4]

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),[5] and river levels can vary by as much as 13 feet (4.0 m). 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.[6]

History

Variant names for the Stillaguamish River, according to the USGS, include Tuxpam River, Stoh-luk-whahmpsh River, Stillaquamish River, Steilaguamish River, Stalukahamish River, and other similar spellings.

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

See also

• List of Washington rivers

References

External links

Wikimedia Commons has media related to Stillaguamish River.

• Snohomish County, Stillaguamish Watershed

На других языках

[de] Stillaguamish River