Page 5: Research news on tsunami

A tsunami is a long-wavelength, gravity-driven water wave phenomenon typically generated by large, sudden displacements of the seafloor due to subduction-zone earthquakes, but also by submarine landslides, volcanic eruptions, or impact events. In deep ocean, tsunamis travel at jetliner speeds with low amplitudes and very long periods (minutes to an hour), behaving as shallow-water waves whose phase speed depends on water depth. As they shoal on continental shelves, energy conservation forces rapid increases in wave amplitude and reductions in wavelength and speed, producing highly nonlinear run-up, strong nearshore currents, and complex inundation patterns that are central to hazard assessment and numerical modeling.

The Soviet Union's secret tsunami

On July 30, one of the largest earthquakes ever recorded struck off the Kamchatka peninsula, in Russia's far east. Within minutes, tsunami warnings were issued in Russia, much of Asia and across the Pacific in Hawaii, New ...

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.

Huge quake off Russia sparks Pacific tsunamis

One of the strongest earthquakes ever recorded struck Russia's sparsely populated Far East on Wednesday, causing tsunamis up to four meters (12 feet) high across the Pacific and sparking evacuations from Hawaii to Japan.

page 5 from 7