Subaqueous sediment density flows are one of the volumetrically most important processes
for moving sediment across our planet, and form the largest sediment accumulations on …

Submarine canyons are morphological incisions into continental margins that act as major
conduits of sediment from shallow-to deep-sea regions. However, the exact mechanisms …

Submarine sediment density flows are one of the most important processes for moving
sediment across our planet, yet they are extremely difficult to monitor directly. The speed of …

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

How the processes that initiate turbidity currents influence turbidite deposition is poorly
understood, and many discussions in the literature rely on concepts that are overly …

The SW margin of the Iberian Peninsula hosts the present-day boundary between the
Eurasian and African Plates. Convergence (4–5mm/yr) is accommodated through a wide …

Central Switzerland lies tectonically in an intraplate area and recurrence rates of strong
earthquakes exceed the time span covered by historic chronicles. However, many lakes are …

Understanding the seismic hazard posed by large earthquakes requires paleoseismic
investigation because most faults have not ruptured repeatedly during the period of historic …

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 …

Coastal marshes record a 6500 yr history of coseismic displacements in great earthquakes
at the Cascadia subduction zone. We compiled estimates of coseismic displacement for past …