On 5 September the Herald on Sunday reported the experiences of people such as Daryl Collier, who was working at the South Terrace bakery in Darfield when the earthquake struck: The railway line is behind us and I thought it was a train coming right through the back of the building. Widely felt over the South Island and the southern North Island, it caused considerable damage in central Canterbury, especially in Christchurch. Canterbury Earthquake (Building Act) Order 2010: revoked (after expiring on the close of 16 September 2011), on 19 April 2016, by section 146(2) of the Greater … For the severe aftershock of 22 February 2011, see 2011 Christchurch earthquake. 8, 2014, pp. Strong aftershocks were reported, including ones of magnitude 5.3. An overview of the impacts of the 2010-2011 Canterbury earthquakes S.H. It was the first Canterbury earthquake which fair walloped Kaiapoi. The Canterbury Earthquake Response and Recovery Act 2010 was a New Zealand statute designed to assist reconstruction after the 2010 Canterbury earthquake. Night brings on the nerves, the ill feelings and the need for adult company to feel safe. [7] http://www.sva.org.nz/history/; Helen Tatham, ‘Social media key to “army” success’, New Zealand Doctor, 21 September 2011, p. 15. I’m certainly not in a rush for Mark to start working nights again. [8] Rachel Harre and Frank Malone operated Fragments of Grace gallery in Kaiapoi, which was badly affected by the September quake. September September 4 – 2010 Canterbury earthquake: A magnitude 7.1 earthquake strikes the South Island of New Zealand, including the city of Christchurch, causing widespread damage and power outages. Australasian Journal of Disaster and Trauma Studies, 2011-2 (Special Issue: A Focus on the Canterbury E, pp. We followed a 4×4 across the bridge and only just made it in our sedan with the car scraping over the gaps. This article has been written by Molly Mcintosh. quake; furthermore, many had been partially damaged and weakened in the 2010 earthquake. I stumbled from the bed and slammed into the door frame whilst trying to get to my son, I eventually made it to his room, I fumbled for the light switch and couldn’t work out why it wouldn’t turn on, I gave up and carried on to his cot. It revealed the existence of a hidden west-east fault under the gravels of the Canterbury Plains. Aftershocks continued for months after the September quake. facilitate the response to the Canterbury earthquake . There confusion reigned supreme. The earthquake shaking also produced liquefaction - ‘a liquid mush’ of soft sand and silt. Reports indicate terror during the main earthquake, however, there was a sense that on-going aftershocks were more devastating and difficult to bear. If the Canterbury earthquake had occurred at 4:53pm, as it did in Haiti, the number of deaths and serious injuries would surely be much higher. It was centred 40 km west of Christchurch, near the town of Darfield, at a depth of 10 km. On 4 September 2010 a moment magnitude (M w) 7.1 earthquake occurred near the small town of Darfield in the Canterbury Plains of the South Island of New Zealand (; Fig. The initial shaking did not cause me to feel too much panic but as we drove and found roads to be splitting and the bridge across the estuary collapsing it became more alarming. Christchurch earthquakes of 2010–11, series of tremors that occurred within and near the city of Christchurch, New Zealand, and the Canterbury Plains region from early September 2010 to late December 2011. The region’s port and airport remained operational, and its manufacturing hub did not sustain significant damage, minimising the disruption to ‘industrial production and good exports and activity’. This will be terrifying!’ knowing with distance it will get smaller, so that was my first reaction. This citation is automatically generated and … [2]. 2010 Canterbury earthquake September 2010 earthquake in New Zealand. The epicentre of the Canterbury earthquake was near the town of Darfield, and felt throughout the South Island and as far north as New Plymouth. It was magnitude 4.9 and 12 kms deep. This site is produced by the History Group of the New Zealand Ministry for Culture and Heritage. One truck started at East, one started at West, and the van we sent around to Rapaki and Corsair Bay, just to do a circuit, to make sure no one was in dire straits of any degree. Liquefaction happens when shaking pushes underground water upwards, making solid ground behave like quicksand. The 4 September 2010 earthquake was the largest to affect a major urban area since the 7.8-magnitude shock that struck the Hawke’s Bay region on 3 February 1931. But they also caused real fear and anxiety – both for people’s own safety and that of their families, friends and neighbours, and for what they might mean for the future of their homes, businesses and community. They were to answer many more in the following days. Though it was reported no lives were lost, that was not entirely correct. And we gave the best advice. While most came from the South Island, there were some from the lower North Island and Stewart Island. Focusing on ‘low risk areas during the immediate response period’, they ‘cleared over 65,000 tons of liquefaction’. [1] Casey Rowney, Panteá Farvid and Chris G. Sibley, ‘I laugh and say I have “earthquake brain!”’: resident responses to the September 2010 Christchurch earthquake’, New Zealand Journal of Psychology, vol. The 2010 Canterbury earthquake (also known as the Darfield earthquake) struck the South Island of New Zealand with a moment magnitude of 7.1 at 4:35am local time on 4 September, and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Most Cantabrians were at home and asleep when the 7.1-magnitude earthquake struck the region before dawn on Saturday 4 September 2010. On 4 September 2010, Canterbury experienced the first of a series of earthquakes that caused widespread damage to the region’s infrastructure and serious disruption to the lives of its people. A plinth in the middle of the room had three figures on it but two had fallen off and were lying amongst the smashed ceramics on the floor. September 28 – A landslide kills at least 7 people in Oaxaca, Mexico. Some sectors were hit hard, ‘notably retail, accommodation and hospitality’. Johnstonb, K.P. Identifying the economic impact is difficult. [6]. BiblioWeb: app03 Version 3.26.0 Last updated 2021/01/20 06:52, Kete Christchurch: Canterbury earthquakes 2010 2011, Christchurch City Libraries' Terms of Use and Privacy Policy. 4 September 2010 Canterbury (Darfield) earthquake 1 This survey was part of a Master of Emergency Management research report to develop recommendations to enhance companion animal … This article has been written by Molly Mcintosh. 1-3. A 2012 Reserve Bank report concluded that Canterbury’s economy had proved ‘reasonably resilient to the impact of the earthquakes’, and that ‘the spill over to other regions’ was limited. I know we are, but it was nice to be looked after. Many buildings were damaged, but only one person died and few people were injured. Initially some Cantabrians worried that they were feeling an even more severe earthquake centred near Wellington – an area known for its seismic activity and where many New Zealanders expected ‘the big one’ to hit. Soil liquefaction caused a lot of problems with flooding, damaging buried pipes and building foundations. Most of the 185 deaths (72%) took place in the collapses of two multistory downtown buildings, designed and constructed in the mid-60s and mid-80 [s, respectively. 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.There was one important difference-this time there has been no loss of life. Seismologists noted that the earthquake sequence was highly unusual, and likely to never happen again anywhere else in the world. In the Waimakariri District, people had to keep boiling their water for longer. Research about the effects of the September earthquake on a group of 191 Canterbury residents highlights the psychological impact of the aftershocks: After the main earthquake, accounts of ongoing trepidation related to the aftershocks and concern of another earthquake happening were reported…. 2010 Canterbury Earthquake 2003 Fiordland Earthquake 2009 Dusky Sound Earthquake What really happened at the 2010 Canterbury earthquake. At 12.51 p.m. on Tuesday 22 February 2011, a magnitude 6.3 earthquake caused severe damage in Christchurch and Lyttelton, killing 185 people and injuring several thousand. [9]. The CTV Building was the headquarters of Canterbury Television (locally known as CTV) and other companies. One person died from a heart attack, possibly caused by the shock of the earthquake, but there were no other deaths. Schools were closed for about two weeks after the earthquake. [9] Stan Darling and Jackie Watson, Kaiapoi shakes: interviews with Kaiapoi residents affected by the September 2010 earthquake, Jackie Watson, Christchurch, 2012, pp. [5] Rowney, Farvid and Sibley, ‘I laugh and say I have “earthquake brain!”’, p. 7. 2, July 2014, p. 7, Janet K. Spittlehouse, Peter R. Joyce, Esther Vierck, Philip J. Schluter and John F. Pearson, ‘Ongoing adverse mental health impact of the earthquake sequence in Christchurch, New Zealand’, Australian & New Zealand Journal of Psychiatry, vol. 75, no. Some went sightseeing in quake-damaged areas. The severest of those events were the earthquake (magnitude from 7.0 to … Despite their efforts, and those of the ambulance officers who soon arrived, she died on her way to hospital. It makes extensive use of contributions to QuakeStories, a website established by the Ministry for Culture and Heritage in 2011. 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