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We contact these puzzle pieces tectonic plates, and the edges from the plates are called the plate boundaries. The plate boundaries are created up of many faults, and almost all of the earthquakes all over the world manifest on these faults. Since the edges with the plates are tough, they get caught whilst the rest of the plate retains transferring. Finally, in the event the plate has moved considerably adequate, the perimeters unstick on one of many faults and there is an earthquake.
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A tsunami isn't a tidal wave – these are attributable to the forces from the moon, sun, and planets upon the tides, along with the wind as it moves in excess of the h2o.
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