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CASCADIA SUBDUCTION ZONE Taylor Peacock EPSC 330 Setting: ~1000 - PDF document

CASCADIA SUBDUCTION ZONE Taylor Peacock EPSC 330 Setting: ~1000 kilometers long Northern Vancouver Island to Cape Mendocino, California Juan de Fuca plate is subducting under the North American plate Subduction Zone


  1. CASCADIA SUBDUCTION ZONE Taylor Peacock EPSC 330 Setting: ~1000 kilometers long • Northern Vancouver Island to Cape Mendocino, • California Juan de Fuca plate is subducting under the North • American plate Subduction Zone megathrust earthquakes are very  powerful and generate tsunamis. The last great earthquake (M>8) that occurred was just  over 300 years ago. 1700 Cascadia Earthquake: Magnitude 9.0  Evidence:  groves of red cedar trees killed by saltwater when o subsidence occurred orphan tsunami in Japan (16 feet high) o Tribal history of the coastal First Nations Peoples o Recurrence Interval: Research done at Oregon State University determined  that the fault has ruptured 41 times in the last 10,000 years 1/3 chance this will happen in the next 50 • years 19 of these events entailed rupturing along the full length • of the fault 1/10 chance of full margin rupture in next 50 • years Tseax Cone Eruption: Deadliest natural disaster in Canada • Earthquake as a trigger for volcanic eruptions •

  2. Last eruption was between 1668 and 1714 • Carbon dating of wood from trees and based on • historical and magnetic dating Cascadia ruptured 450 km south of Tseax • First Nations told stories of shaking before any fire and • smoke Could the next rupture of of the CSZ trigger a volcanic • eruption in this region? During the event: Initial waves=compressional • May be detected by sensors 30-90s prior to • beginning of shaking Audible to dogs/other animals • Provide warning and to trigger safety procedures • 3-5 minutes of shaking • M 8.0-8.6 if southern portion ruptures and 8.7+ if the • entire length ruptures Several feet of vertical motion and up to 100 feet of • westward motion The wave is estimated to be 20-100 feet tall • depending on where it reaches the coast Impact and Aftermath: 71,000 people in the inundation zone must evacuate  between earthquake and tsunami, which is 10-30 minutes. Earthquake and ensuing tsunami is expected to leave • >12,000 people dead and >26,000 injured (FEMA model: early February event) Results: • Fallen bridges will trap people on the coast and • prevent rescue workers from being able to reach them Liquefaction: solid ground behaves as a liquid and • causes instability Highways and roads will be damaged, power will go • out, fires will start ~30,000 landslides will occur in Seattle alone •

  3. They anticipate having to provide food and water for 2.5 • million people, and shelter for 1 million. According to OSSPAC: Improvements in seismic codes since 1994: ~75% of • structures are likely to fail Evacuation procedures + routes • Illegal to build hospitals, schools, firehouses, police • stations in the inundation zone The inundation zone will be ~uninhabitable for years • Time estimates for restoration on the coast: • 3-6 months for electricity • 1-3 years for drinking water and sewage systems • Time estimates for restoration west of Interstate 5: • 1-3 months for electricity • 1-12 months for drinking water and sewer services • 6-12 months for major highways • 18 months for healthcare facilities • Collapse of the economy in the PNW •

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