Lake Tacoma

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Lake Tacoma
02 Lake Tacoma, Nisqually, Russell (1913) fig 10.jpg
Glacial lakes Lake Tacoma, Lake Nisqually, & Lake Russell
USA Washington relief location map.jpg
Red pog.svg
Lake Tacoma
Location Puyallup River
Pierce County, Washington
Coordinates 47°17′00″N122°26′58″W / 47.283283°N 122.449330°W / 47.283283; -122.449330
Lake type Glacial lake (former)
Primary inflows Vashon Glacier
Primary outflows Ohop channel
Basin  countries United States
Max. length25 miles (40 km)
Max. width18 miles (29 km)
Max. depth256 feet (78 m)
Residence time ca 200 years
Surface elevation350 m (1,150 ft)
References [1]

Lake Tacoma is the name given the freshwater lake in the basin of the Puyallup River and the Green River (Duwamish River) at the point in time that the Vashon Glacier had receded northward into Commencement Bay. Prior to this, it was referred to as the Lake Puyallup. The bluff on which this city is built is used as the landmark where Lake Puyallup ceased and it became Lake Tacoma. [1]

See also

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Lake Nisqually is used to identify the freshwater lake formed in the Puget Sound trough, west of Tacoma. It is sometime confused with Early Lake Russell which covered the same area during a previous northward retreat of the glacier. The glacier returned southward, then on its final retreat northward, the waters filing this basin are referred to as Lake Nisqually. Its discharge was across the Black Lake channel at 160 feet (49 m) above sea level. Two deltas formed along the eastern margin of the lake from the outflow of Lake Tacoma in the Puyallup River valley. Both the Steilacoom and Sequalichew deltas, at 160 feet (49 m). A rise in level to 180 to 200 feet reflects the closure of the Black Lake outlet while the two deltas were still growing.

<span class="mw-page-title-main">Lake Puyallup</span> Glacial lake (former) in Pierce County, Washington

Lake Puyallup developed along the south edge of the Puget Sound Glacier. The glacier was in retreat northward after having reached its most southerly point. Drainage off the north face of Mount Rainier and the melting ice of the glacier was trapped in the valley of the Puyallup River. As the glacier moved north, the lake grew until it reached its largest capacity with the glacier at the glacial front across the Puyallup valley just south of Commencement Bay at Tacoma and northern bend of the White River at Auburn. When the ice retreated further north, it was reduced in depth and volume and takes on the name of Lake Tacoma.

References

  1. 1 2 Washington Geological Survey, Bulletin No. 8; Glaciation of the Puget Sound Region; J. Harlen Bretz; Olympia, Wash, Frank M. Lamborn Public Printer; 1913