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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.
Since 1995 when Snohomish County acquired the first phase of Robe Canyon, volunteers have maintained the Old Robe Trail. In 2002, volunteers continued the tradition, led by Volunteers for Outdoor Washington, performing annual maintenance, installing log-railings, and relocating a section of trail lost to the river's winter rampages.
The city limits are defined to the north by the Stillaguamish River, to the east by Iron Mountain, to the south by the Pilchuck River, and to the west by 174th Avenue Northeast. [22] According to the United States Census Bureau , the city has a total area of 2.20 square miles (5.70 km 2 ), of which, 2.18 square miles (5.65 km 2 ) is land and 0. ...
Oso is located along the Stillaguamish River North Fork, which forms a valley between several arms of the Cascade Range. [6] The community is accessible via State Route 530, which continues 12 miles (19 km) west to Arlington and 16 miles (26 km) east to Darrington.
The Stillaguamish River empties into the northern end of Port Susan. To the south, Port Susan connects with the rest of Puget Sound via Possession Sound and Saratoga Passage. A swampy waterway connects the northern end of Port Susan with Skagit Bay. This waterway also separates Camano Island from the mainland.
The Mark Clark Bridge is a girder bridge that carried a State Route 532 across the Stillaguamish River between Stanwood, Washington, and Camano Island. It is the only form of road access to Camano Island from 1950 until 2010, when it is demolished. The bridge is named for Mark W. Clark, a decorated Army officer who spent time on Camano Island ...
Boxcar Rapids is very heavily traveled compared to other rapids, especially from whitewater rafting tours from Maupin. The rapids are turbulent and have large waves, and a small but noticeable drop. There is also a small ledge drop that leads to a hole on the left side.
Like the larger Florence Island, Leque is part of the Stillaguamish river delta. The island is formed where the Old Stillaguamish River Channel bifurcates at Leque's Point, with the South Pass flowing into Port Susan and the West Pass emptying into the southern end of Skagit Bay. Leque is separated from Camano to the west by Davis Slough. [1]