When a tsunami is in the deep waters of the ocean they can have a wave length of over 120 miles traveling at speeds of up to 500 mph. This great speed means that tsunamis can turn deadly to areas far away from the original seismic event before anyone has time to adequately prepare. To understand how a tsunami works think about sitting on the side of a pool when someone takes a giant leap into the water. That sudden and massive event causes the water to suddenly be displaced, rising up and splashing out of the pool. This same principle applies when there is a large landslide or a volcanic explosion in or near the sea. The force from that event pushes the water but since it happens so suddenly and on such a large scale the resulting wave grows in length and power and can cause an often devastating “splash” when it hits shore. As it approaches the shore, the resistance from the land begins to slow the wave, to about 50 mph, and compresses the wave length. As this water is compressed, the wave begins to form and grow in height

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before finally cresting as it slams into the shore. While any victims on the coast would see this process occurring, the wave would grow so rapidly that there is little time for them to get out of harms way. In some cases, with very large tsunamis, the water may recede dramatically as the wave forms depending on where the seismic activity occurred and the magnitude of the wave.
Understandably, tsunamis can be quite deadly and have killed thousands in a single strike. But does global warming play any role in this? Stay tuned for the second part of this article in which we will discuss the theories involving global warming's effect on tsunamis and the impact that they have.