Many of the largest earthquakes are generated at subduction zones or other plate boundary
fault systems near enough to the coast that marine environments may record evidence of …

Cascadia Basin includes the deep ocean floor over the Juan de Fuca and Gorda Plates and
extends from Vancouver Island, Canada, to the Mendocino Escarpment off northern …

The Washington continental margin presents both a classic test of submarine
paleoseismology, and an opportunity to explore advancement of the field through analysis of …

74 piston, gravity and jumbo Kasten cores were collected from channel and canyon systems
draining the northern California continental margin to investigate the record of periodic …

We relate the late Holocene northern San Andreas fault (NSAF) paleoseismic history
developed using marine sediment cores along the northern California continental margin to …

In order to investigate the possibility of a long-term paleoseismic history from offshore
sedimentary records in Sumatra, we collected 144 deep-sea sediment cores in the trench …

Deep-sea turbidite has been used to determine the history of occurrence of large
earthquakes. Surface-sediment remobilization is a mechanism of the generation of …

A series of 23 thin, mostly mud-silt turbidites are found interspersed between larger, well-
dated and regionally correlated paleoseismic sandy turbidites that extend along most of the …

Here we investigate sedimentary records from four small inland lakes located in the
southern Cascadia forearc region for evidence of earthquakes. Three of these lakes are in …

Turbidite deposition along slope and trench settings is evaluated for the Cascadia and
Sumatra–Andaman subduction zones. Source proximity, basin effects, turbidity current flow …