A tsunami is a long ocean wave (or series of waves) or surges, caused by a major disturbance to the sea floor such as an undersea earthquake, landslide or volcanic eruption. They are different to the storm tide surge which can occur with cyclones and from large waves which can accompany storms.
The phenomenon is usually associated with earthquakes, landslides or volcanic eruptions in, or adjacent to oceans, and results in sudden movement of the water column. Until recently tsunamis were called tidal waves, even though the event has nothing to do with tides.
In deep water, tsunamis can reach speeds of up to 950km/hr and may travel across the sea for hundreds of kilometres hitting distant communities hours after they are generated. They slow down but grow in size as they come ashore. Rather than one huge wave, a tsunami may look like a rapidly rising or falling tide and occur as a series of waves with periods of time in between
Despite the presence of the Great Barrier Reef, the Burdekin region could still be affected by a tsunami. Although the reef may reduce the impact of a tsunami, the scale of impact depends on what caused the tsunami, how far away the event is and where it is in relation to our shire. There may be only a few hours warning. Even a relatively small tsunami of less than one metre can move with force and cause dangerous rips and currents.