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Possibly landslip related. A 3-metre high localised tsunami was caused by a landslide into Deep Cove, Doubtful Sound in May During the magnitude 7 23 August Fiordland earthquake , a significant landslide swept in to Charles Sound causing a 4 to 5 metres high tsunami that damaged a wharf and helipad in the Sound. Although an inland eruption, the Taupo eruption is considered to have caused an atmospheric pressure wave of sufficient magnitude to cause a tsunami. There is evidence of a tsunami in the Bay of Plenty from the Healy volcanic eruption. The Krakatoa eruption generated a rissaga of up to 2 metres high on the New Zealand Coast.
Before this the Eltanin impact in the eastern part of the South Pacific Ocean during the late Pliocene 2. There is disputed historic evidence that a mega-tsunami with a wave height of greater than 30 metres could have struck Stewart Island in the 15th century.
A study of Puatai Beach on the East Coast of the North Island in identified three or four large tsunamis with waves between 9 and 12 metres had impacted the East Coast. While they are likely to have been from earthquakes the exact cause and timing has yet to be determined.
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Evidence of the tsunami came from marine gravel deposits at 32 sites north along the coast from Awakino. The tsunami that occurred between and was associated with the South Taranaki Bight possibly extended down to Abel Tasman National Park. The cause of this change in settlement pattern is believed to have been tsunamis. This may be linked to the previously mentioned Mahuika crater meteor event. This event is undated. The waves reached metres inland at Kaingaroa destroying a dam and two trawlers.
At Wharekauri a bridge was badly damaged and fences washed away. Te Awanui island was inundated and at Owenga several boats and some shell crushing machinery was damaged. A small hut was also washed away.
On Pitt Island the wharf was destroyed and on Mangere Island there was a large landslide. The source of the tsunami is unknown, it could have been caused by either a landslide or an unidentified earthquake. There have been numerous minor tsunamis caused by significant large earthquakes. The effect of the Kanto earthquake was reported in local newspapers as abnormal tides on 5 September. It has been suggested that this movement was caused by tsunamis.
Initial European settlement was unaware of the tsunami danger until the and tsunamis.
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No warning systems became available until after the Aleutian earthquake when the National Oceanic and Atmospheric Administration Pacific Tsunami Warning Centre was established in New Zealand became a member of the Centre and receives warnings of tsunamis caused by distant earthquakes. New Zealand is one of the 46 member countries.
Tsunamis from these may arrive within a few minutes and this is not enough time for GeoNet to locate the event, determine if it could produce a tsunami, and notify the Ministry of Civil Defence and Emergency Management who issue the warnings. Differing approaches to tsunami warning sirens are taken on a regional level.
For example, a large scale siren system was installed in Christchurch in , [51] whereas there are no tsunami warning sirens in the Wellington region. In addition New Zealand, at the time of the Indian Ocean earthquake and tsunami , did not have sea-based tsunami warning devices.
Further complicating matters is the Pacific Tsunami Warning Centre's ocean-based, tsunami warning devices are focused on protecting Alaska, Hawaii, and the United States Pacific coastline. This means that there is a gap in the Southern Ocean. Wellington was the first place to paint blue lines on its roadways to indicate the limit of potential tsunami hazards. The project evoked international interest. From Wikipedia, the free encyclopedia. Main article: Wairarapa earthquake. Main article: Arica earthquake.
Main article: Iquique earthquake. Main article: Murchison earthquake.
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Main article: Hawke's Bay earthquake. Main article: Aleutian Islands earthquake. Main article: Valdivia earthquake. Main article: Kaikoura earthquake. Further information: Kaikoura Peninsula.