Where is the inundation zone in the Pacific Northwest?

Where is the inundation zone in the Pacific Northwest?

Known as the Cascadia subduction zone, it runs for seven hundred miles off the coast of the Pacific Northwest, beginning near Cape Mendocino, California, continuing along Oregon and Washington, and terminating around Vancouver Island, Canada.

Could the Puget Sound have a tsunami?

New tsunami hazard maps published by the Washington Geological Survey and the Washington State Department of Natural Resources (DNR) show that a large earthquake on the Cascadia subduction zone (CSZ) off the Washington coast could cause a tsunami that will not only reach the Puget Sound and Hood Canal, but will leave …

Where is the Cascadia inundation zone?

The Cascadia Subduction Zone (CSZ) is a 1,000 kilometer fault where the Juan de Fuca and North American plates meet. Located off the Pacific Northwest coast, this plate runs from central Vancouver Island, B.C. to northern California.

Can a tsunami hit Tacoma WA?

Bellingham, Olympia, Seattle, and Tacoma could see anywhere from 6 inches to 11 feet of water from a tsunami off the Washington coast. EVERETT, Wash. Part of the Snohomish River Delta between Everett and Marysville could get nearly 6 feet, and Seattle’s Harbor Island could be inundated with nearly 4 feet of water.

Where is the fault line in Washington State?

The Seattle Fault is a zone of multiple shallow east–west thrust faults that cross the Puget Sound Lowland and through Seattle (in the U.S. state of Washington) in the vicinity of Interstate Highway 90.

Which Washington State city did NOAA model a tsunami inundation on the Pnsn website?

Ocean Shores Washington
NOAA modeled a tsunami train attacking Ocean Shores Washington in this animation.

Could a tsunami hit Edmonds WA?

EDMONDS, Wash. — Communities in western Washington like Edmonds, Everett and Bellingham are no longer considered out of reach of damaging tsunami waves.

Can a tsunami hit Everett WA?

The tsunami risk in Everett is mainly concentrated along the waterfront and Snohomish River delta including Jetty Island, marinas, and other low-lying coastal areas. That’s why it’s important to be signed up for tsunami alerts and to have a NOAA weather radio receiver.

Where in Washington are earthquakes most likely to occur?

While most earthquakes occur in Western Washington, some damaging events, such as the 1872 magnitude 6.8 (est.) quake, do occur east of the Cascades.

Is Seattle on the San Andreas Fault?

Unlike the better-known San Andreas Fault in California, which consists of a single fracture that parallels the coastline, the Seattle Fault Zone is at least four closely related fractures that run west to east for about 30 miles.

Is there going to be a tsunami in Washington State?

Tsunamis have hit Washington in the past, and they will happen again in the future. Click on the icons below to learn about how and where tsunamis occur, how to recognize a tsunami, how to evacuate before a tsunami arrives, and what geologists at the Washington Geological Survey are doing to learn more about these natural hazards.

Where are the tsunami fault lines in Washington State?

The Cascadia subduction zone off the coast of Washington, British Columbia, Oregon, and northern California is the biggest tsunami hazard for Washington State. This very large fault is capable of generating some of the largest and most damaging earthquakes in the world.

Where can I find tsunami walk time maps?

Use your scroll wheel or the zoom buttons in the upper left corner to zoom. You can read more about the walk time maps on the Evacuation Page. The Northwest Association of Networked Ocean Observing Systems (NANOOS) has developed an interactive map of tsunami evaucation zones, routes, and assembly areas for both Oregon and Washington.

What kind of earthquakes occur in Washington State?

Washington has three major earthquake sources that have the potential to cause tsunamis: subduction zone earthquakes, deep (Benioff Zone) earthquakes, and shallow crustal fault earthquakes. Sources of earthquakes in Washington and the relative frequency of occurrence.