Lake Washington is the second largest natural lake in state of Washington (after Lake Chelan) and the largest lake in King County. It is bordered by the cities of Seattle on the west, Bellevue and Kirkland on the east, Renton on the south and Kenmore on the north, and surrounds Mercer Island. It is fed by the Sammamish River at its north end and the Cedar River at its south.
Welcome to CWAnswers
CWAnswers is your guide to the sprawling world wide web. The directory aims to provide a useful guide made by users. You can share your knowledge as well - simply sign up and edit your first entry. For questions just contact the team at support - at - cwanswers.com.
Weblinks for Lake Washington
Top 10 for Lake Washington
Things about Lake Washington you find nowhere else.
Select content modules
Lake Washington is the second largest natural lake in state of Washington (after Lake Chelan) and the largest lake in King County. It is bordered by the cities of Seattle on the west, Bellevue and Kirkland on the east, Renton on the south and Kenmore on the north, and surrounds Mercer Island. It is fed by the Sammamish River at its north end and the Cedar River at its south.
Lake Washington received its present name in 1854 after Thomas Mercer suggested it be named after George Washington, as the new Washington Territory had been named the year before. The Duwamish called it "Lake Xacuabš" (Lushootseed: literally great-amount-of-water). Kenmore Air operates passenger seaplane service at Kenmore Air Harbor at the northern end of the lake.
Geography
Lake Washington is a ribbon lake, which are long, narrow and finger-like. Ribbon lakes were formed thousands of years ago during the ice age through glaciation: as the glacier bulldozed through a valley (glacial trough), it met bands of harder and softer rock. Erosion (mainly through abrasion: the process of rocks simply being scraped across the bedrock) was greater at the soft rock than the hard rock and so a dip was created. When the glacier melted the lake filled with the meltwater, which was held in by moraine (rock material) deposited by the glacier. A dam can also be created by the bands of harder rock either side of the softer rock. There is usually a river at both ends of a ribbon lake, one being the inflow, and the other, the outfow - though in the case of present day Lake Washington, both serve as inflow rivers.
Creeks and rivers
In addition to the Cedar and Sammamish Rivers, numerous small creeks and rivers feed the lake, including:
- Ravenna Creek
- Thornton Creek
- Kelsey Creek
- Juanita Creek
- Coal Creek
Canals and bridges
Before construction of the Lake Washington Ship Canal in 1916, Lake Washington's outlet was the Black River, which joined the Duwamish River and emptied into Elliott Bay. When the canal was opened the level of the lake dropped nearly nine feet (3 m). The canal to the Puget Sound became the lake's sole outlet, causing the Black River to dry up and disappear.
Concrete floating bridges were employed to span the lake because Lake Washington's depth and muddy bottom prevented the emplacement of the pilings or towers necessary for the construction of a causeway or suspension bridge. The bridges consist of hollow concrete pontoons that float atop the lake, anchored with cables to each other and to weights on the lake bottom. The roadway is constructed atop these concrete pontoons. Three floating bridges cross Lake Washington: the Evergreen Point Floating Bridge (officially the Governor Albert D. Rosellini Bridge - Evergreen Point) carries State Route 520 from Seattle's Montlake neighborhood to Medina while the Lacey V. Murrow Memorial Bridge and the Third Lake Washington Bridge (officially the Homer M. Hadley Memorial Bridge) carry Interstate 90 from Seattle's Mount Baker neighborhood to Mercer Island. The East Channel Bridge carries Interstate 90 from Mercer Island to Bellevue. The Evergreen Point, Lacey V. Murrow, and Third Lake Washington bridges are the longest, second longest, and fifth longest floating bridges in the world, respectively.

























