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Tsunami waves are never deep-water waves, because even in the deepest ocean they still feel the bottom. As the sea bottom becomes shallower, the velocity of the tsunami slows down, and to conserve energy the wave amplitude builds up.
The largest number of earthquakes occur around the rim of the Pacific Ocean associated with a series of volcanoes and deep-ocean trenches known as the "Ring of Fire". As a result, the largest source region for tsunamis is in the Pacific Ocean with 71% of all occurrences.
When these tectonic plates slip over, under, or past each other at the fault lines where they meet, energy builds up and is released as an earthquake. Undersea earthquakes sometimes cause ocean waves called tsunamis.
Because of a tsunami's long wavelengths, which can be hundreds of miles, a tsunami is barely noticeable in the deep ocean and rarely more than three feet (one meter) high. Mariners at sea will not normally notice a tsunami as it passes beneath their hulls.
Deep-ocean tsunami detection buoys are one of two types of instrument used by the Bureau of Meteorology (Bureau) to confirm the existence of tsunami waves generated by undersea earthquakes. These buoys observe and record changes in sea level out in the deep ocean.
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As a result, the largest source region for tsunamis is in the Pacific Ocean with 71% of all occurrences. Within the main Pacific Ocean basin, tsunamis generated in the tropics, while locally devastating, tend to weaken rapidly with distance.
A tsunami is a series of extremely long waves caused by a large and sudden displacement of the ocean, usually the result of an earthquake below or near the ocean floor. This force creates waves that radiate outward in all directions away from their source, sometimes crossing entire ocean basins.
Tsunamis can be generated by earthquakes on all of these faults, but most tsunamis, and the largest, result from earthquakes on reverse faults. These tsunami-generating earthquakes originate mainly in subduction zones, where tectonic plates collide and one is forced under the other.
An earthquake happens when a big piece of the Earth's crust suddenly shifts. Basically, the Earth's crust is made up of large pieces called tectonic plates. These plates usually grind together. But sometimes, the plates get stuck. The pressure builds and they suddenly get slammed and are pushed into a new position.
Mariners at sea will not normally notice a tsunami as it passes beneath them; in deep water, the top of the wave rarely reaches more than three feet higher than the ocean swell.

devices designed to recognize a tsunami form