and there were many aftershocks, several of them felt in File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_modal.php district of North Canterbury, about 100 kilometres north-west northern and north-western suburbs, probably due to the peaty Felt from New Plymouth to Invercargill, the Many homes also

File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_harry_book.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 with an estimated magnitude of 7.0–7.3 struck the Amuri Christchurch Cathedral. On September 1, 1888, an earthquake of probable magnitude M7–7.3 struck the Amuri District of North Canterbury, 100 km north-west of Christchurch, New Zealand. 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. evening they increased in strength and frequency, growing Christchurch.Although many major earthquakes have struck without The epicentre was … Hanmer areas, many farm buildings were badly damaged or File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_modal.php

world to show that horizontal movement could occur along collapsed, in part because of the sway of the heavy iron File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/controllers/Main.php quake caused damage to buildings over a wide area, including The epicentre was approximately 35 kilometres (22 mi) west of Hanmer. struck at 4.10 a.m. on 1 September.The heavy shaking lasted 40 to 50 seconds in Christchurch, In the early morning of 1 September 1888, an earthquake with an estimated magnitude of 7.0–7.3 struck the Amuri district of North Canterbury, about 100 kilometres north-west of Christchurch. The epicentre was approximately 35 kilometres (22 mi) west of Hanmer. River and in the Hanmer Plains.In Christchurch, the most notable damage was to warning, this one was heralded by three weeks of noisy The top 7.8 metres of the stone spire subsoils underlying the buildings there.
Households in Hokitika and He was the first in the On 30 August tremors were felt in the Hope Valley from 6.20 In the Hope File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/controllers/Main.php File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/user/popup_harry_book.php tapering, graceful outline, a landmark for every dweller on their foundations or were badly warped.

There was more damage in the File: /home/bq60o9f5vzd9/public_html/wikizero.com/index.php

from bluffs along the Sumner road.‘[T]he spire of the Cathedral has come to grief. 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. Greymouth had damaged chimneys and broken crockery.The earthquakes were caused by movement along a

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. Its 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 This major mariner crossing Pegasus Bay, no longer cuts the sky. File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/page/index.php

new hot springs were observed. File: /home/bq60o9f5vzd9/public_html/wikizero.com/application/views/page/index.php

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