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Fife branch of the Pierce County Library system. Fife is a city in Pierce County, Washington, United States and a suburb of Tacoma. The population was 10,999 at the 2020 census. [4] Fife is contained within the Puyallup Indian Reservation and bisected by Interstate 5. It is east of Tacoma and the Port of Tacoma.
Hylebos Creek is a stream located in the U.S. state of Washington near Tacoma and emptying into Commencement Bay, part of Puget Sound.It flows through southern King County and northern Pierce County, through the cities of Tacoma, Federal Way, Milton, and Fife, as well as the Puyallup Indian Reservation.
Location of Kitsap County in Washington. This is a list of the National Register of Historic Places listings in Kitsap County, Washington. This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Kitsap County, Washington, United States. Latitude and longitude coordinates are provided ...
The museum has 165,000 square feet (1.53 ha) of exhibit space, [1] and contains a 350-car gallery showing cars notable for their speed, technology and design, as well as their importance to car culture. The building also contains gift shops, restoration shops, lecture halls, galleries, a banquet room, and a café.
Fife Heights is a census-designated place (CDP) in Pierce County, Washington, United States. The population was 1,919 at the 2020 census. The community is bordered by Federal Way on the north, Milton on the east, Fife on the south, and Tacoma on the west. [2] It is contained within the Puyallup Indian Reservation.
SR 509 traveling across the Thea Foss Waterway on the cable-stayed 21st Street Bridge within Tacoma, connecting downtown to the Port of Tacoma.. SR 509 begins as South 21st Street at a single-point urban interchange with I-705 in downtown Tacoma in Pierce County, [3] providing access to the Tacoma campus of the University of Washington and the Tacoma Link light rail line on Pacific Avenue.
Fifes Peaks are located east of the Cascade crest. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.As fronts approach, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snow onto the Cascades.