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There is evidence that the Australian coast may have experienced large tsunami during the past few thousand years.This evidence is revealed through anomalous sedimentary deposits (such as those containing shell or coral) or other geomorphic features (Dominey Howes, 2007; Goff and Chauge-Goff, 2014).A tsunami is different from a wind-generated surface wave on the ocean.While wind-generated waves in deep water only cause water movement near the surface, the passage of a tsunami involves the movement of water from the surface to the seafloor.Until recently, tsunami were called tidal waves, but this term is generally discouraged because tsunami generation has nothing to do with tides (which are driven by the gravity of the Earth, Moon and Sun).

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The significant tsunamis recorded in recent times have all been recorded at tide gauges around the country with some causing damage in the marine environment.Tsunami (pron: 'soo-nar-me') is a Japanese word: 'tsu' meaning harbour and 'nami' meaning wave.Tsunami are waves caused by sudden movement of the ocean surface due to earthquakes, landslides on the sea floor, land slumping into the ocean, large volcanic eruptions or meteorite impact in the ocean.Upon receiving the earthquake alert from Geoscience Australia, the Bureau of Meteorology issues a tsunami bulletin within 10 minutes of receiving the alert.The JATWC is thus able to issue tsunami bulletins within 20 minutes of the origin time of the earthquake.This assessment could then be used by Australian emergency managers in understanding the tsunami hazard to Australia.