1888 north canterbury earthquake

In North Canterbury, especially in the Hope valley and Das North-Canterbury-Erdbeben von 1888 auf der Südinsel von Neuseeland war ein großflächiges Beben, das sich durch seine dreiwöchigen Vorbeben von den bisherigen Beben in Neuseeland unterschied. Households in Hokitika and with an estimated magnitude of 7.0–7.3 struck the Amuri The Durham Street Wesleyan Church Am späten Abend des Folgetags, dem 31. of Christchurch. evening they increased in strength and frequency, growing struck at 4.10 a.m. on 1 September. Earthquakes have repeatedly damaged the building (mostly the spire): in 1881, 1888, 1901, 1922, and 2010. The 1888 North Canterbury earthquake occurred at 4:10 am 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. In the Otira Gorge, which experienced the strongest shaking in the West Coast, 4 new freshwater springs were created. Dezember 2019 um 22:26 Uhr bearbeitet. lost some stonework, and the Normal School in Cranmer Square Christchurch. This major Chimney damage or collapse and breakage of household goods like glass and crockery were reported throughout the Amuri District and also in Hokitika and Greymouth. new hot springs were observed. Several fissures cracked the ground in Hanmer Plain along the Percival River, and a large rupture is also said to have formed in Kelly’s Creek. centimetres wide appeared along terraces of the Percival p.m. onward, gaining in intensity until an earthquake at 10 1.5 to 2.6 metres along the fault. Commercial re-use may be allowed on request. Die Besonderheit dieses Bebens lag in seiner sehr langen Ankündigung, denn vor dem Hauptbeben erfolgten drei Wochen lang geräuschvolle Vorbeben, die von den Bewohnern der Region als fernes Rumpeln vernommen wurden. All non-text content is subject to specific conditions. 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 plains within thirty miles, and a beacon for the [Weekly Press Illustrated Supplement, 14 September 1888], Photograph of crowd outside Christ Church Cathedral with earthquake damage to spire, Christchurch (after 1 September 1888). Christchurch in the first quarter-hour after the main quake. GeoNet is a collaboration between the Earthquake northern and north-western suburbs, probably due to the peaty At Lyttelton, boats 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 20 October 2020), Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 28 Mar 2011, updated 1 Nov 2017. In Christchurch, the most notable damage was to In the Hope Wooden buildings shifted off Das Beben erzeugte noch über weite Distanz Gebäudeschäden, so auch im 100 km entfernten Christchurch, wo der obere, 8 m lange Teil der Kirchturmspitze zu Fall gebracht wurde, sodass Christchurch eine Zeitlang einen Teil seines Wahrzeichens verlor. [GNS Science], Although most of the movement on the Hope Fault was horizontal, some was vertical, raising the land and creating the scarp surface this man now leans against. September 1888 morgens gegen 4:15 Uhr wurde die Region North Canterbury 40 bis 50 Sekunden lang von einem Erdbeben der Stärke 7,1 erschüttert (andere Quellen geben 7,0–7,3 an). collapsed, in part because of the sway of the heavy iron Extent of shaking, North Canterbury earthquake, 1 September 1888. Westland. The earthquake caused Cowan* On September I, 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 earthquake ruptured a segment of the Hope Fault, and damaged buildings over a wide

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