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Normal tsunamis result from displacement of the sea floor due to plate tectonics. A megatsunami is a separate class of event from an ordinary tsunami and is caused by different physical mechanisms. ( July 2021) ( Learn how and when to remove this template message)Ī megatsunami is a tsunami with an initial wave amplitude ( height) measured in many tens, hundreds, and possibly up to thousands of metres. Unsourced material may be challenged and removed. Please help improve this article by adding citations to reliable sources. This section needs additional citations for verification.
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Prehistoric examples include the Storegga Slide (landslide), and the Chicxulub, Chesapeake Bay, and Eltanin meteor impacts. These giant wave heights occur because the water is "splashed" upwards and outwards by the impact or displacement.Įxamples of modern megatsunamis include the one associated with the 1883 eruption of Krakatoa ( volcanic eruption), the 1958 Lituya Bay megatsunami ( landslide into a bay), and the wave resulting from the Vajont Dam landslide (caused by human activity destabilizing sides of valley). They can have extremely large initial wave heights ranging from hundreds and possibly up to thousands of metres, far beyond the height of any ordinary tsunami. By contrast, megatsunamis occur when a large amount of material suddenly falls into water or anywhere near water (such as via a meteor impact or volcanic activity). Ordinary tsunamis exhibit shallow waves in the deep waters of the open ocean that increase dramatically in height upon approaching land to a maximum run-up height of around 30 metres (98 ft) in the cases of the most powerful earthquakes. Ordinary tsunamis are caused by underwater tectonic activity (movement of the earth's plates) and therefore occur along plate boundaries and as a result of earthquake and the subsequent rise or fall in the sea floor that displaces a volume of water. Megatsunamis have quite different features from ordinary tsunamis.
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