OLYMPIA – The state Department of Natural Resources has released a new series of tsunami simulations focused on southwest Washington.
Using detailed tsunami models, geologists at DNR, home to the Washington Geological Survey, produced simulations that show the estimated height and speed of waves that would strike the southwest Washington coast following a magnitude 9.0 earthquake on the Cascadia subduction zone.
The videos show Cascadia tsunami wave simulations for the southwest Washington coast, with detailed, localized impacts for Grays Harbor and the Long Beach Peninsula.
The simulations join others created last summer that show the expected inundation of coastlines in northwest Washington and along the Strait of Juan de Fuca.
All can be found at youtubetsunami.
The simulations are designed to give emergency planners and communities visualized information about tsunami impacts and timing so they can plan accordingly.
“Tsunamis have struck Washington’s coast many times over our geologic history. It’s a question of when, not if, the next one will hit,” said Commissioner of Public Lands Hilary Franz.
“These videos are designed to give the communities that would be most impacted by tsunamis a visualization of what areas are likely to face the most damage so they can make sure their residents, businesses and institutions are secure and resilient.”
DNR has produced static tsunami hazard maps for the area that show maximum inundation.
These simulations demonstrate how the tsunami wave heights change throughout the entirety of the tsunami event, increasing and decreasing over a span of many hours.
The last magnitude 9 Cascadia subduction zone earthquake struck in 1700 and produced a tsunami that left sand deposits and drowned forests, which can still be seen in places like the Copalis Ghost Forest in Grays Harbor County.
The geologic record shows the Cascadia subduction zone — the offshore area where the Juan de Fuca tectonic plate pushes under the larger North American plate — produces megathrust quakes every 300 to 600 years.
There have been about 40 earthquakes on the subduction zone in the last 10,000 years.
