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 A tsunami (/(t)suːˈnɑːmi, (t)sʊˈ-/ (t)soo-NAH-mee, (t)suu-;[1][2][3][4] from Japanese: 津波, lit. 'harbour wave',[5] pronounced [tsɯnami]) is a seri of waves in a water bodi caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami.[6] Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large moment. Taruhan Bola Online   Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer.[7] Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide.[8] For this reason, it is often referr