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The United States Geological Survey defines the Strait of Juan de Fuca as a channel. It extends east from the Pacific Ocean between Vancuver Island[?], Canada, and the Olympic Peninsula[?], Washington, to Haro Strait[?], San Juan Channel[?], Rosario Strait[?], and Puget Sound. Its Pacific Ocean boundary is formed by a line between Cape Flattery[?] and Tatoosh Island[?], Washington, and Carmanah Point[?] (Vancouver Island), British Columbia. Its northern boundary follows the shoreline of Vancuver Island[?] to Gonzales Point[?], then follows a continuous line east to Seabird Point[?] (Discovery Island[?]), British Columbia, Cattle Point[?] (San Juan Islands), Washington, Iceberg Point[?] (Lopez Island[?]), Point Colville (Lopez Island[?]), and then over Rosario Head[?] (Fidalgo Island[?]). The eastern boundary is a continuous line extending south from Rosario Head along Whidbey Island to Point Partridge[?] and south to Point Wilson[?] (Quimper Peninsula[?]). The Washington mainland forms the southern boundary of the strait.
Counties along the Strait of Juan de Fuca:
Source: United States Geological Survey (http://geonames.usgs.gov/pls/gnis/web-query.gnisprod?f-name=Juan+de+Fuca&variant=N&f-state=&f-cnty=&f-ty=&elev1=&elev2=&cell=&pop1=&pop2=&my-function=Send+Query&last-name=&last-state=&last-cnty=&page-cnt=&record-cnt=&tab=Y)
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