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A tsunami can be created when a disturbance displaces a large water mass from its equilibrium position. In earthquake-generated tsunamis, the water column is disturbed by the uplift or subsidence of the ocean floor. Submarine landslides, which often come with large earthquakes, as well as disintegration of volcanic edifices, can also disturb the overlying water column as sediment and rock slump downslope and are redistributed across the sea floor. Similarly, a violent submarine volcanic eruption can create an impulsive force that uplifts the water column and generates a tsunami (Ruff, 2003, Yalciner, 2003)...
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