, 2019 The Cascadia subduction zone is understood to produce large, Mw 9.0, earthquakes every 300-1000 years. As a result of large ruptures along the fault, Washington, Oregon and Northern California, are susceptible large tsunamis along the coast.
Morkner, Paige
core +1 more source
Slow earthquake scaling reconsidered as a boundary between distinct modes of rupture propagation. [PDF]
Proc Natl Acad Sci U S A, 2023 Ide S, Beroza GC.
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, 1998 The Cascadia subduction zone forms the present convergent margin between the North American plate and the oceanic Gorda, Juan de Fuca and Explorer plates from approximately 40°N to 50°N.
Wang, Carl X.
core
Slab tearing and segmented subduction termination driven by transform tectonics. [PDF]
Sci AdvShuck B +14 more
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Toward equitable coastal community resilience: Incorporating principles of equity and justice in coastal hazard adaptation. [PDF]
Camb Prism Coast Futur, 2023 Fox N +4 more
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Secondary acceleration of slip fronts driven by slow slip event coalescence in subduction zones. [PDF]
Nat CommunWang J +7 more
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Rapid fault healing from cementation controls the dynamics of deep slow slip and tremor. [PDF]
Sci AdvThomas AM +5 more
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Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions. [PDF]
Proc Natl Acad Sci U S AChen S +6 more
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The big impact of small quakes on tectonic tremor synchronization. [PDF]
Sci AdvFarge G, Brodsky EE.
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Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface. [PDF]
Sci Rep, 2023 Lee C, Kim Y.
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