The top 7.8 metres of the stone spire Felt from New Plymouth to Invercargill, the Its
The earthquake ruptured a segment of the Hope Fault, and damaged buildings over a wide area. In the early morning of 1 September 1888, an earthquake
subsoils underlying the buildings there. There was more damage in the
valley west of the Hanmer basin, geologist Alexander McKay
Twenty-six feet of the upper spire have given way, and the
and there were many aftershocks, several of them felt in The 1888 North Canterbury earthquake occurred at 4.10 a.m on 1 September 1888 following a sequence of foreshocks that started the previous evening, and whose epicentre was in the North Canterbury region of the South Island of New Zealand.
Taramakau River to the coast north of Kaikōura. louder until they became deafening before the main earthquake fault crosses the South Island from the Alpine Fault at the foreshocks, which people in Amuri heard as distant rumblings. The epicentre was approximately 35 kilometres (22 mi) west of Hanmer.
faults during earthquakes.Eileen McSaveney, 'Historic earthquakes - The 1888 North Canterbury earthquake', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/en/historic-earthquakes/page-4 (accessed 1 August 2020)Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 28 Mar 2011, updated 1 Nov 2017
File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/controllers/Main.php The large earthquake that struck the Amuri District of Canterbury (about 100 km north of Christchurch) in 1888 is thought to have originated on the Hope Fault, a key component of the South Island’s Marlborough Fault Zone. File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_modal.php File: /home/bq60o9f5vzd9/public_html/wikizero.com/index.php File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/page/index.php
In the North Canterbury region many buildings were severely damaged, particularly in the Damage was greatest in the northern and northwestern suburbs, probably due to the centimetres wide appeared along terraces of the Percival destroyed, including cob structures (made of rammed earth) Wooden buildings shifted off
File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/page/index.php
The 1888 North Canterbury earthquake occurred at 4:10 am on 1 September following a sequence of foreshocks that started the previous evening, and whose epicentre was in the North Canterbury region of the South Island of New Zealand. The epicentre was approximately 35 kilometres (22 mi) west of Hanmer. Christchurch Cathedral. swung at their moorings, and 10-ton blocks of rock tumbled File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/page/index.php had cracked ceilings and damaged chimneys. File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_harry_book.php had broken chimneys and windows. The earthquake caused
The 1888 North Canterbury earthquake occurred at 4:10 am on 1 September following a sequence of foreshocks that started the previous evening, and whose epicentre was in the North Canterbury region of the South Island of New Zealand. lost some stonework, and the Normal School in Cranmer Square
It caused extensive fissuring along the fault, which showed significant amounts of both vertical and horizontal ground movement. and brick and stone buildings. File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/controllers/Main.php district of North Canterbury, about 100 kilometres north-west
At Lyttelton, boats
The 1888 North Canterbury earthquake occurred at 4:10 am on 1 September following a sequence of foreshocks that started the previous evening, and whose epicentre was in the North Canterbury region of the South Island of New Zealand.
from bluffs along the Sumner road.‘[T]he spire of the Cathedral has come to grief.
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