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The first Tacoma Narrows Bridge opened to traffic on July 1, 1940. Its main span collapsed into the Tacoma Narrows four months later on November 7, 1940, at 11:00 AM (Pacific time) due to a physical phenomenon known as [[aeroelasticity#Flutter|aeroelastic flutter]] caused by a {{convert|67|km/h}} wind. The bridge collapse had lasting effects on science and engineering. In many undergraduate physics texts the event is presented as an example of elementary forced resonance with the wind providing an external periodic frequency that matched the natural structural frequency (even though the real cause of the bridge's failure was aeroelastic flutter<ref name="BillahScanlan91">{{cite journal|last=Billah|first=K.|coauthors=[[Robert H. Scanlan|R. Scanlan]]|year=1991|title=Resonance, Tacoma Narrows Bridge Failure, and Undergraduate Physics Textbooks|journal=American Journal of Physics|volume=59|issue=2|pages=118–124|url=http://www.ketchum.org/billah/Billah-Scanlan.pdf|format=PDF|doi=10.1119/1.16590}}</ref>). Its failure also boosted research in the field of bridge aerodynamics/aeroelastics which have themselves influenced the designs of all the world's great long-span bridges built since 1940.
No human life was lost in the collapse of the bridge. However, a
Dismantling of the towers and side spans—which survived the collapse of the main span but were damaged beyond repair—began shortly after the collapse and continued into May 1943. The United States' participation in [[World War II]] as well as engineering and finance issues delayed plans to replace the bridge.
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