Because of a combination of new observational tools and a flurry of large megathrust
earthquakes, tremendous progress has been made in recent years towards understanding …

A new history of great earthquakes (and their tsunamis) for the central and southern
Cascadia subduction zone shows more frequent (17 in the past 6700 yr) megathrust …

Active fault traces are a surface expression of permanent deformation that accommodates
the motion within and between adjacent tectonic plates. We present an updated national …

Past earthquake rupture models used to explain paleoseismic estimates of coastal
subsidence during the great AD 1700 Cascadia earthquake have assumed a uniform slip …

Annual exceedance probabilities of the maximum tsunami inundation depth, h Max, and
momentum flux, M Max, conditional on a full-rupture event of the Cascadia Subduction Zone …

We conduct a comprehensive modeling study of the impact of the 1964 Prince William
Sound tsunami on the US Pacific Northwest coast. A 3D unstructured grid model, SELFE, is …

The generation, propagation and inundation for a probabilistic near-field tsunami hazards
assessment (PTHA) at the Cascadia Subduction Zone (CSZ) are analyzed numerically. For …

We present a preliminary probabilistic tsunami hazard assessment of Canadian coastlines
from local and far-field, earthquake, and large submarine landslide sources. Analyses …

The criteria for zoning the surface fault rupture hazard (SFRH) along thrust faults are defined
by analysing the characteristics of the areas of coseismic surface faulting in thrust …

Characterizations of tsunami hazards along the Cascadia subduction zone hinge on
uncertainties in megathrust rupture models used for simulating tsunami inundation. To …