The Cascadia subduction zone (CSZ) is an exceptional geologic environment for recording
evidence of land-level changes, tsunamis, and ground motion that reveals at least 19 great …

▪ Abstract We present preliminary evidence for a∼ 10,000-year earthquake record from two
major fault systems based on sediment cores collected along the continental margins of …

Abstract The 2014 Working Group on California Earthquake Probabilities (WGCEP14)
present the time‐independent component of the Uniform California Earthquake Rupture …

A puzzling tsunami entered Japanese history in January 1700. Samurai, merchants, and
villagers wrote of minor flooding and damage. Some noted having felt no earthquake; they …

Tide gauges show that global sea level has risen about 7 inches during the 20th century,
and recent satellite data show that the rate of sea-level rise is accelerating. As Earth warms …

The 1700 Cascadia earthquake attained moment magnitude 9 according to new estimates
based on effects of its tsunami in Japan, computed coseismic seafloor deformation for …

Published areas of high coseismic slip, or asperities, for 29 of the largest Circum‐Pacific
megathrust earthquakes are compared to forearc structure revealed by satellite free‐air …

Tsunami deposits related to the 1929 Grand Banks earthquake and washover deposits
related to the 1991 Halloween storm differ in their sedimentary characteristics and positions …

Bradley Lake, on the southern Oregon coastal plain, records local tsunamis and seismic
shaking on the Cascadia subduction zone over the last 7000 yr. Thirteen marine incursions …

Comparison of histories of great earthquakes and accompanying tsunamis at eight coastal
sites suggests plate-boundary ruptures of varying length, implying great earthquakes of …