A Statistical Analysis of Large Magnitude Earthquakes along the Cascadia Subduction Zone

Faculty Mentor

Richard Orndorff

Presentation Type

Poster

Start Date

4-14-2026 2:00 PM

End Date

4-14-2026 4:00 PM

Location

PUB NCR

Primary Discipline of Presentation

Geosciences

Abstract

The Pacific Northwest is home to the Cascadia Subduction Zone, a 1,000 km-long megathrust fault that stretches from Northern California to Southern Canada. Earthquakes are generated as the results of stresses associated with movement of the Juan de Fuca plate beneath the North American plate, a process known as subduction. Subduction zone megathrust faults are the only faults in the world that can produce earthquakes with magnitudes of 8.5 or greater. For example, in 1700 the Cascadia Subduction Zone produced a devastating 9.0 magnitude earthquake. Geological records also indicate that it has generated 19 great (M8+) earthquakes over the past 10,000 years in approximately 500-year intervals and is expected to rupture again in the future. The goal of this project is to use binomial, geometric, and Poisson analyses to calculate probabilities of major Cascadia Subduction Zone earthquakes in the next 50 years from 126 years of earthquake records from the USGS Earthquake Hazards Program - Earthquake Catalog.

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Apr 14th, 2:00 PM Apr 14th, 4:00 PM

A Statistical Analysis of Large Magnitude Earthquakes along the Cascadia Subduction Zone

PUB NCR

The Pacific Northwest is home to the Cascadia Subduction Zone, a 1,000 km-long megathrust fault that stretches from Northern California to Southern Canada. Earthquakes are generated as the results of stresses associated with movement of the Juan de Fuca plate beneath the North American plate, a process known as subduction. Subduction zone megathrust faults are the only faults in the world that can produce earthquakes with magnitudes of 8.5 or greater. For example, in 1700 the Cascadia Subduction Zone produced a devastating 9.0 magnitude earthquake. Geological records also indicate that it has generated 19 great (M8+) earthquakes over the past 10,000 years in approximately 500-year intervals and is expected to rupture again in the future. The goal of this project is to use binomial, geometric, and Poisson analyses to calculate probabilities of major Cascadia Subduction Zone earthquakes in the next 50 years from 126 years of earthquake records from the USGS Earthquake Hazards Program - Earthquake Catalog.