| Lake Puyallup | |
|---|---|
 Glacial lakes Lake Puyallup & Early Lake Russell | |
  Lake Puyallup | |
| Location | Puyallup River Pierce County, Washington |
| Coordinates | 47°13′25″N 122°20′40″W / 47.223655°N 122.344414°W |
| Lake type | Glacial lake (former) |
| Primary inflows | Vashon Glacier |
| Primary outflows | Ohop channel |
| Basin countries | United States |
| Max. length | 17 miles (27 km) |
| Max. width | 9 miles (14 km) |
| Max. depth | 595 feet (181 m) |
| Residence time | less than 200 years |
| Surface elevation | 350 m (1,150 ft) |
| References | [1] |
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.[1]