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Kōrero: Earthquakes

Wairarapa Fault scarp, Pigeon Bush

Image
Wairarapa Fault scarp, Pigeon Bush

The steep scarp marks the Wairarapa Fault, which has ruptured several times during earthquakes in the last 5,000 years. The last recorded earthquake, in 1855, caused the channel of a stream to be offset by 18.7 metres – the largest single horizontal offset during an earthquake recorded anywhere in the world. An older offset channel to the left, which moved during an earlier earthquake, is indicated in the photograph.

Te whakamahi i tēnei tūemi

Victoria University of Wellington, Rodney Grapes

by Timothy Little

This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. It is the responsibility of the user of any material to obtain clearance from the copyright holder.

Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Me pēnei te tohu i te whārang

Eileen McSaveney, Earthquakes – What causes earthquakes?, Te Ara – the Encyclopedia of New Zealand, https://teara.govt.nz/mi/photograph/4400/wairarapa-fault-scarp-pigeon-bush (accessed 4 June 2026).

He kōrero nā Eileen McSaveney, i tāngia i te 2 March 2009, updated 1 August 2017.

Comments

jayedeesalinas
11 June 2015
what is p=wave-these are called 'p' for primary wave they are the ones that travel fastest and there by are usually "felt" first.