2014-2060

The Cascadia Subduction Zone is a 600 mile-long converging plate boundary stretching from northern California to southern British Columbia. The fault causes a major earthquake about once every 300 years. Compared to other fault lines, this is an unusually long return time – resulting in greater stress build-up and stronger subsequent earthquakes. The last major event (a so-called megathrust quake) took place in 1700 and was estimated to have had a magnitude of at least 9.0.

Bridges and highways collapse, while the ground in the Seattle bay area liquefies, dragging buildings underwater. Broken gas mains and power lines spark many fires. The quake generates massive tsunamis,* which inundate coastal communities from California to Alaska. These giant waves are sent racing across the Pacific, causing damage as far away as Hawaii and Japan. Millions are left without power, while emergency responders struggle to adapt to the scale of the disaster. The death toll quickly reaches into the thousands, while the financial cost exceeds $100 billion. Along with the similarly devastating southern California earthquake, this disaster pushes much of the American west coast toward financial ruin.
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