Power to up to 75 percent of the city was disrupted. The historic homesteads of Hororata and Homebush inland from Christchurch were both extensively damaged, as were Ohinetahi homestead and Godley House on Banks Peninsula. Liquid silt has gushed up through cracks in the surface - Photos by Nicola Litchfield. in Engineering from UCLA in 2005 and 2010. Part of the Daily Mail, The Mail on Sunday & Metro Media Group. Over the months that followed, it was established that more than 180 people had died in the quake; many of them had been killed outright as structures collapsed and debris fell in the streets, crushing cars and buses as well. this month: 5.5 in Te ... 10 km depth Pleasant Point, Canterbury, New Zealand. 'It was strong in Blenheim! The fire was quickly extinguished by the Fire Service before it could spread. Map of the central part of New Zealand's South Island depicting the intensity of shaking caused by the earthquake of Sept. 4, 2010, and the strong aftershock of Feb. 22, 2011. This multi-fault rupture produced a magnitude 7.1 earthquake that released 13 times more energy than the Christchurch earthquake. We are no longer accepting comments on this article. Our editors will review what you’ve submitted and determine whether to revise the article. Water and sewer pipes in the ground broke and water from the cracked mains flooded many streets. Civil Defence also declared a state of emergency for Selwyn District and Waimakariri District. The New Zealand Army deployed personnel upon the request of the Christchurch mayor. Muddy mixtures of sand and silt squirted upward through cracks to produce miniature sand volcanoes. [73] This was at least in part due to outlying birthing centres being closed,[74] pending structural checks, forcing more mothers to deliver at hospitals than was generally the case. Some of these have been strong enough to cause damage to structures that were already weakened by the main earthquake. Bexley and other suburbs were flooded after water mains broke; after the waters receded, quake-damaged roads and homes remained covered with silt.

Luck played a part - the quake occurred at a time when everyone was home in bed and the streets were largely deserted. The fault, later named the Greendale Fault, appeared about 50 to 56 miles (80 to 90 km) southeast of the boundary between the Australian and Pacific tectonic plates, and part of the fault became visible at the surface because of the earthquake. … [1] Some damaging aftershocks followed the main event, the strongest of which was a magnitude 6.3 shock known as the Christchurch earthquake that occurred nearly six months later on 22 February 2011. [98] Homebush, located four kilometres from Glentunnel and only 15 kilometres from the earthquake's epicentre, was the historic home of the Deans family, one of the Canterbury Region's pioneer settler families, but was so extensively damaged that it has been described as being "practically in ruins". In the early hours of Saturday morning on 4 September 2010, people in Christchurch and the surrounding Canterbury region were jolted awake by the most damaging earthquake in New Zealand since the deadly magnitude 7.8 Hawke's Bay (Napier) earthquake in 1931. ", "M 7.2 Darfield (Canterbury) Sat, Sep 4 2010: Story", "Canterbury earthquake really three quakes? During the first day after the earthquake, the aftershocks were clustered close to the east-west fault trace across the Canterbury Plains. [75] Four metres (13 ft) of sideways movement has been measured between the two sides of the previously unknown fault. [86] After inspection, services south of Dunedin and north of Kaikoura recommenced at 10:30 am that day. The focus of this temblor was relatively shallow, however, occurring only 3 miles (5 km) beneath the surface of Heathcote Valley, a suburb of Christchurch located on the Banks Peninsula.

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