Puget Sound faults about 1100 years ago (AD 900—930) an earthquake of magnitude 7+ uplifted Restoration Point and Alki Point, dropped West Point (the three white triangles in the Seattle Basin on the map), caused rockslides in the Olympics, landslides into Lake Washington, and a tsunami on Puget Sound. It extends as far east as (and probably terminates at) the Rattlesnake Mountain Fault Zone (RMFZ; the southern extension of the SWIF) near Fall City. This seems geologically reasonable, as both the SWIF and RMFZ appear to be the contact between Tertiary Crescent Formation basement of Puget Sound on the west and the older
Puget Sound salmon recovery spawn in the rivers running into the Puget Sound. Some Puget Sound rivers that salmon swim up are: Nooksack, Samish, Skagit, Baker, Cascade, Stillaguamish, Snohomish, Skykomish, Green, Puyallup, Carbon, Nisqually, Deschutes rivers. Salmon also go up Lake Washington, Lake Sammamish, Kennedy Creek, and Minter Creek. The life cycle of salmon requires specific conditions within the chain of connected environments. Salmon typically live 3–6 years, which often changes depending on life conditions. While some salmon stay within the Puget Sound, others will migrate and live deeper in the Pacific Ocean. The salmon begin their journey as fertilized eggs in a stream