Page 2: Research news on tsunamis

Tsunamis are long-wavelength, low-amplitude sea waves generated by large, impulsive disturbances of the ocean, most commonly co-seismic seafloor displacement along subduction zones, but also volcanic eruptions, landslides, or submarine mass failures. They propagate as shallow-water gravity waves with phase speeds governed primarily by ocean depth, enabling rapid trans-oceanic travel with minimal energy loss. In deep water they exhibit small surface amplitudes and long periods (minutes to tens of minutes), amplifying dramatically through shoaling, refraction, and resonance effects on continental shelves and in coastal basins. Scientific research focuses on source characterization, wave propagation modeling, inundation mapping, and hazard assessment for early warning and coastal risk mitigation.

Cascadia megathrust earthquake could trigger San Andreas fault

When the tectonic subduction zone beneath the Pacific Northwest moves, it does so in dramatic fashion. Not only is ground shaking from a magnitude 9+ earthquake incredibly destructive, the event triggers tsunamis and landslides ...

Volcano erupts after quake in Russia's far east

A volcano in Russia's far east erupted on Wednesday, Russian scientists said, hours after a major quake prompted evacuations and tsunami alerts across parts of the Pacific coast.

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