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Zodiac sign: Pisces. My name is Sammy. On the Waimakariri River a 1. The schooner Challenge broke away from her wharf and collided with the Gazelle. The William and Julia were lifted onto the river bank and the Nora and Dart broke free from their wharf. After the tsunami Ferdinand von Hochstetter undertook a detailed analysis of the tsunami. He charted its progress across the Pacific determining wave speeds and the ocean depth along several paths. It was the first detailed scientific analysis of a major tsunami.

In the Evening Post carried a letter which suggested Westport had been submerged under a metre high wave, with the old township now lying metres under the sea. This story was later modified in the Colonist by its writer to being associated with the Arica earthquake with the sea at Westport receding some 7—8 metres and a returning wave of much less significance. Both harbours reported tidal waves with the one at Nelson over-topping the Boulder Bank. The wave was estimated to be just over a metre in height. The paper also reported that the tidal wave had impacted numerous South Island ports.

On 10 May at UTC a magnitude 8. The wave had a reported metre height in most places and impacted the coast from the Bay of Islands to Bluff. At Port Charles on the Coromandal Peninsula the waves were reported being over 3 metres high. With the knowledge gained from the tsunami, newspapers of the day were already speculating that the source of the wave was from a South American earthquake. On 22 February a 1 metre high tsunami followed a local magnitude 6.

On 17 June a 2. The earthquake triggered a landslip at Waikare which in turn caused a localised At Napier there was a tsunami of about 3 metres. A 1 metre high tsunami was said to have reached Northland from the Aleutian Island earthquake. Within 30 minutes the coast from Muriwai to Tolaga Bay experienced a tsunami which peaked at 10 metres high at Turihaua. At Tatapouri Point four people at the nearby hotel escaped by getting to high ground.

Two waves drove through the hotel ground floor at up to window sill height and a number of small buildings were washed away. Two men in a cottage at Turihaua were swept inland onto the coast road.

The cottage was totally destroyed, except for the kitchen they were in. Other damage included the Pouawa River bridge which was swept metres inland, a house at Te Mahanga Beach which was swept off its piles, and six hectares of pumpkins at Murphy's Beach. No one was killed. On 17 May another tsunami hit the coast between Gisborne and Tolaga Bay with a maximum height of 6 metres north of Gisborne.

Again there were no casualties. The earthquake responsible for it was a 6. A tsunami generated by the Mw 9. As with the other earlier and Chilean tsunamis the eastern coast of New Zealand from Cape Reinga to Stewart Island was impacted. More unusually, effects of the tsunami was also observed on the west coast of both islands, including Ahipara, Whanganui, Paremata, Nelson, Motueka, and several West Coast South Island towns.

At the Chatham Islands and Campbell Island water heights above sea level ranged from 3 metres to over 5 metres. The largest and most damaged waves were generally within 12 to 15 hours after the first ones although some were within the first 2—4 hours. The Pacific Tsunami Warning Center alerted New Zealand authorities of the approaching tsunami prompting the first major tsunami evacuation in New Zealand.

A tsunami, caused by the Kaikoura earthquake, of 2. It also travelled metres up a creek adjacent to the cottage.

Sonar mapping has found the presence of massive submarine landslides near the New Zealand coast that would have triggered large localised tsunamis. Three large waves greater than 4 metres high over the period to 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.

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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.