Tsunamis
A succinct definition of a tsunami is " ... A natural phenomenon consisting of a series of waves generated when water in a lake or the sea is rapidly displaced on a massive scale. ( Wikipedia: Tsunami) A more explicit and technical definition is, " A tsunami is a very long-wavelength wave of water that is generated by sudden displacement of the seafloor or disruption of any body of standing water. Tsunamis are sometimes called "seismic sea waves." ( Nelson A.)
The essential characteristic of a tsunami is therefore a radical displacement of water. This displacement of water can be caused by various events, such as, earthquakes, ocean landslides, volcanic eruptions and large meteorite impacts as well as large explosions. The effect of a Tsunami depends on the severity and size of the initial causative factors and the original displacement of water mass. The effects can range from a minor and hardly noticeable ocean surge to complete devastation. Tsunamis are often not even noticed out at sea. This is due to another tsunami characteristic, namely that they "have a much smaller amplitude offshore, and a very long wavelength -often hundreds of kilometers long," (Wikipedia: Tsunami) A tsunami can reach speeds of over 500 mph or 800 kph. The average heights of a tsunami wave are 30 feet or nine meters. However tsunamis of have been reordered of over 100 feet to 30 meters. (What are tsunamis)
The main areas that are threatened by Tsunamis are coasts throughout the Pacific Ocean, where earthquakes are a frequent occurrence. At risk are the islands of Japan and Hawaii and the Alaskan and northern South American coasts. Tsunamis also occur in the Atlantic Ocean, and Mediterranean Sea
In the last 200 years tsunamis have affected the parts of the United States.
'Since 1946, six tsunamis have killed more than 350 people and caused significant property damage in Hawaii, Alaska, and along the West Coast. Tsunamis have also occurred in Puerto Rico and the Virgin Islands."
(Rosenberg, M.)
2. Causes
Simply stated, tsunamis are phenomenon created by the displacement of water mass. As this displaced mass moves according to gravitational forces, it radiates across the waters with a ripple effect. As they approach the land, tsunamis take on the characteristics of tide surge. The resemblance to a sudden tide surge has resulted in the name "tidal wave" being applied to them. However, they are not related to tides or tidal actions in any sense.
The most common cause of a tsunami is the displacement of the sea bed structure. This is usually a result of intense earthquake action. "Tsunamis can be generated when the sea floor abruptly deforms and vertically displaces the overlying water." Such large vertical movements of the earth's crust can occur at plate boundaries and subduction zones. Subduction zones " ... exist at convergent plate boundaries where Oceanic lithosphere collides with either continental lithosphere or oceanic lithosphere and sinks below the latter plate into the mantle." ( Wikipedia: subduction) Subduction earthquakes are one of the main generators of tsunamis. They occur when there is movement of the denser oceanic plates which move beneath the continental plates.
The sense of displacement of the ocean floor is an important factor in wave generation. Tsunamis are formed when there is a vertical displacement of the ocean floor. Therefore, it is not the case that even large earthquakes will necessarily produce large tsunami. For example, the 1906 earthquake near San Francisco California had a Richter Magnitude of about 7.1, yet no tsunami was generated as a result of this event " because the motion on the fault was strike-slip motion with no vertical displacement. " ( Nelson A.)
The reason why so many tsunamis are generated in the Pacific Ocean is mainly due to the fact that the Pacific is surrounded by plate boundaries and most of these events are the result of earthquakes which occur along the subduction boundaries.
The process of the tsunamis aproach to the shore is described as follows.
As a tsunami leaves the deep water of the open sea and arrives at the shallow waters near the coast, it undergoes a transformation. Since the velocity of the tsunami is also related to the water depth, as the depth of the water decreases, the velocity of the tsunami increases. The change of total energy of the tsunami, however, remains constant. Furthermore, the period of the wave remains the same, and thus more water is forced between the wave crests causing the height of the wave to increase. Because...
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