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Earthquake waves travel faster in rocks. In rocks near the Earth's surface the waves can move at 6 or 7 kilometers per second. In water, sound can travel about 1.5 kilometers per second, and a tsunami wave can travel at up to 1000 km per hour- fast, but not nearly as fast as in the rocks.

That's why seismometers can give warnings of a possible tsunami. The earthquake waves arrive at the seismometers far in advance of any possible tsunami. But earthquakes in the seabed don't always cause tsunamis.

Some earthquake waves won't travel through water at all. The two first waves on any seismometer's trace of an earthquake are called P and S, for "primus" and "secondus" or some wretched thing- "primary" and "secondary" are good enough. But it would also be adequate to call them "pressure" and "shear," or "push" and "shake," since that's what they do. The P wave is a compression in the direction the wave is moving, like a sound wave. It will go through water or other liquids. The S-wave is a shear, a side-to-side shaking. Liquids just slip aside and absorb that kind of motion, they won't transmit it.

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