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The 1940 Tacoma Narrows Bridge, the first bridge at this location, was a suspension bridge in the U.S. state of Washington that spanned the Tacoma Narrows strait of Puget Sound between Tacoma and the Kitsap Peninsula. It opened to traffic on July 1, 1940, and dramatically collapsed into Puget Sound on November 7 of the same year. [1]
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List of Washington State bridge failures (PDF), Washington State Department of Transportation (WSDOT), c. 2009, archived from the original (PDF) on 2015-02-05 – via The Seattle Times "I-5 bridge collapses over Skagit River, no fatalities". Seattle: KING-TV. Associated Press. May 23, 2013. Archived from the original on June 7, 2013
A major landslide occurred 4 miles (6.4 km) east of Oso, Washington, United States, on March 22, 2014, at 10:37 a.m. local time.A portion of an unstable hill collapsed, sending mud and debris to the south across the North Fork of the Stillaguamish River, engulfing a rural neighborhood, and covering an area of approximately 1 square mile (2.6 km 2).
The Tacoma Narrows Bridge is a pair of twin suspension bridges that span the Tacoma Narrows strait of Puget Sound in Pierce County, Washington. The bridges connect the city of Tacoma with the Kitsap Peninsula and carry State Route 16 (known as Primary State Highway 14 until 1964) over the strait. Historically, the name "Tacoma Narrows Bridge ...
The Astoria–Megler Bridge is a steel cantilever through- truss bridge in the Pacific Northwest region of the United States that spans the lower Columbia River. It carries a section of U.S. Route 101 from Astoria, Oregon, to Point Ellice near Megler, Washington. Opened in 1966, it is the longest continuous truss bridge in North America.
The bridge before the collapse. The bridge carries a section of Interstate 5 (I-5) over the Skagit River between Mount Vernon and Burlington, in Washington state, about 60 miles (97 km) north of Seattle. I-5 is the primary highway between the metropolitan areas of Seattle and Vancouver, British Columbia. Before the collapse, approximately ...
Channeled Scablands. The Channeled Scablands are a relatively barren and soil-free region of interconnected relict and dry flood channels, coulees and cataracts eroded into Palouse loess and the typically flat-lying basalt flows that remain after cataclysmic floods within the southeastern part of Washington state. [1][2] The Channeled Scablands ...