Causes of Tsunamis

sunami the Great Waves Tsunami is a Japanese word with the incline translation, harbor moving ridge. Represented by two characters, the top character, tsu, means harbor, time the bottom character, nami, means wave. In the past, tsunamis were sometimes referred to as tidal waves by the general public, and as seismic sea waves by the scientific community. The full term tidal wave is a misnomer although a tsunamis impact upon a coastline is subordinate upon the tidal level at the time a tsunami strikes, tsunamis are unrelated to the tides.Tides result from the imbalanced, extraterrestrial, gravitational influences of the moon, sun, and planets. The term seismic sea wave is also misleading. Seismic implies an earthquake-related generation mechanism, but a tsunami drive out also be peed by a nonseismic until nowt, such as a landslide or meteorite impact. Tsunamis are a threat to life and property to anyone living undecomposed the marineic. For example, in 1992 and 1993 ever yplace 2,000 people were killed by tsunamis occurring in Nicaragua, Indonesia and Japan. Property impose on _or_ oppress was nearly one billion dollars.The 1960 Chile Earthquake generated a Pacific-wide tsunami that caused widespread death and destruction in Chile, Hawaii, Japan and other areas in the Pacific. heavy(p) tsunamis have been known to rise over 100 feet, while tsunamis 10 to 20 feet high asshole be very cataclysmic and cause many deaths and injuries. What Cause Tsunamis? Tsunamis, also called seismic sea waves or, incorrectly, tidal waves, broadly speaking are caused by earthquakes, less commonly by submarine landslides, infrequently by submarine volcanic eruptions and very rarely by a big meteorite impact in the nautical.Submarine volcanic eruptions have the strength to produce truly awesome tsunami waves. The Great Krakatau Volcanic Eruption of 1883 generated freak waves reaching heights of 125 feet above sea-level, killing thousands of people and wiping bre ak through numerous coastal villages. Ring of Fire About two-thirds of the earth is cover by the weewees of the four oceans. The Pacific nautical is the worlds largest, covering much than one third of the total surface area of our planet.The Pacific ocean is surrounded by a series of mountain chains, deep ocean trenches and island arcs, sometimes called a ring of fire. The large size of the Pacific Ocean and the large earthquakes associated with the ring of fire combine to produce deadly tsunamis. Tsunamis on the Move Wave Height and Water Depth In the circularize ocean a tsunami is less than a a couple of(prenominal) feet high at the surface, but its wave height increases rapidly in shallow weewee. Tsunamis wave efficacy extends from the surface to the bottom in the deepest waters.As the tsunami attacks the coastline, the wave energy is compressed into a much shorter distance creating destructive, live-threatening waves. In the deep ocean, destructive tsunamis can be smal loften only a few feet or less in heightand cannot be take inn nor can they be felt by ships. But, as the tsunami reaches shallower coastal waters, wave height can increase rapidly. Sometimes, coastal waters are drawn out into the ocean just before the tsunami strikes.When this occurs, more shoreline may be exposed than even at the lowest tide. This major withdrawal of the sea should be interpreted as a warning of the tsunami waves that will follow How Fast? Where the ocean is over 20,000 feet deep, unnoticed tsunami waves can travel at the speed of a commercial jet plane, nearly 600 miles per hour. They can move from one spattere of the Pacific Ocean to the other in less than a day. This great speed makes it important to be aware of the tsunami as soon as it is generated.Scientists can predict when a tsunami will arrive since the speed of the waves varies with the forthright root of the water depth. Tsunamis travel much slower in shallower coastal waters where their wave height s begin to increase dramatically. How Big? inshore and coastal features can determine the size and impact of tsunami waves. Reefs, bays, entrances to rivers, undersea features and the slop of the beach all help to modify the tsunami as it attacks the coastline.When the tsunami reaches the coast and moves inland, the water level can rise many feet. In extreme cases, water level has risen to more than 50 feet for tsunamis of distant origin and over 100 feet for tsunami waves generated near the earthquakes epicenter. The first wave may not be the largest in the series of waves. One coastal community may see no damaging wave activity while in some other community destructive waves can be large and violent. The flooding can extend inland by 1000 feet or more, covering large expanses of land with water and debris.