海嘯是一種具有強(qiáng)大破壞力的海浪。當(dāng)?shù)卣鸢l(fā)生于海底，因震波的動(dòng)力而引起海水劇烈的起伏，形成強(qiáng)大的波浪，向前推進(jìn)，將沿海地帶一一淹沒(méi)的災(zāi)害，稱(chēng)之為海嘯。
Tsunamis are powerful waves caused by underwater earthquakes or eruptions that can crash over ten stories tall into a coastline. If you were sailing far from shore, how would you feel about a tremendous tsunami heading your way? Actually, you wouldn’t notice a tsunami at all. In deep water, a tsunami raises the ocean’s surface only about one or two feet—much less than ordinary ocean waves. What’s more, it takes up to an hour for a single tsunami to roll by. How can a wave be so deadly to a coastline, but so tame in the open ocean? The energy of a wave has more to do with how deep the water churns than how tall the wave rises. Ordinary waves can be rather tall, but they don’t go very deep. What’s more there’s never much distance between one ordinary wave’s crest and the one following it. The distance between waves is called “wavelength,” and it’s another secret of a tsunami’s strength. While ordinary waves only tug at the surface water, tsunamis churn the water all the way to the deepest ocean floor! They also have very long wavelengths—a hundred miles or more. Although tsunamis raise the surface only a foot or so in deep water, they carry a lot of energy. When a tsunami approaches a coastline, the water gets shallower. This causes friction at the front of the wave and slows it down. The faster moving back of the wave piles into the slower front, squeezing the whole hundred mile tsunami like an accordion. Just as a rug will crumple and rise if it’s scrunched by an opening door, the tsunami gets taller. By the time it hits the beach, it can be a hundred feet high!