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Casualties can be high because the waves move faster than humans can run.Earthquakes, volcanic eruptions and other underwater explosions (detonations of nuclear devices at sea), landslides and other mass movements, bolide impacts, and other disturbances above or below water all have the potential to generate a tsunami.This makes tsunamis difficult to detect over deep water. As the tsunami approaches the coast and the waters become shallow, wave shoaling compresses the wave and its velocity slows below 80 kilometres per hour (50 mph).Its wavelength diminishes to less than 20 kilometres (12 mi) and its amplitude grows enormously, producing a distinctly visible wave.
A tsunami is a wave in the ocean caused by earthquakes or volcanic eruptions. The waves travel at a great speed across an ocean with little energy loss.
They can remove sand from beaches, destroy trees, damage houses and even destroy whole towns.
The water will draw back from the coast half of the period of the wave before it gets to the coast.
Since the wave still has such a long wavelength, the tsunami may take minutes to reach full height.
Except for the very largest tsunamis, the approaching wave does not break (like a surf break), but rather appears like a fast moving tidal bore.
Such a storm surge inundated Burma (Myanmar) in May 2008.