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Cascadia Fault

The Cascadia Subduction Zone: A Looming Threat to the Pacific Northwest

One of the worst nightmares for many Pacific Northwest residents is a huge earthquake along the offshore Cascadia Subduction Zone, a 960-kilometer (600-mile) fault that stretches from northern California to southern British Columbia.

The Cascadia subduction zone is a complex system of faults and plates that has the potential to generate a magnitude 9 earthquake. Such an event would cause widespread devastation, including ground shaking, tsunamis, and landslides.

The new finding could help scientists better understand the earthquake potential of the Cascadia subduction zone and develop more effective earthquake early warning systems.

The Cascadia subduction zone is a convergent plate boundary, where the Juan de Fuca Plate is subducting beneath the North American Plate. The subducting plate is slowly sinking into the mantle, and as it does, it builds up stress on the overriding plate. When the stress becomes too great, the plates can slip, causing an earthquake.

The Cascadia subduction zone has a long history of generating large earthquakes. The most recent major earthquake occurred in 1700 and had an estimated magnitude of 9.0. This earthquake caused widespread damage and tsunamis that reached as far as Japan.

Scientists believe that the Cascadia subduction zone is capable of generating another magnitude 9 earthquake in the future. The next earthquake is expected to occur within the next 50 years, and it could have a devastating impact on the Pacific Northwest.


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