http://www.quakestories.govt.nz/184/story/I remember vaguely thinking that the noise on our roof sounded like hundreds of heavy footed birds landing on the corrugated iron. It was based on the Greendale fault, which is a newly discovered fault. I was so angry I picked up the surviving one and lifted it over my head ready to smash it but Frank saw me and yelled ‘That’s not broken!’ I didn’t smash it…. [9]. 1905, All Blacks' non-try hands Wales historic win, Home A recent post was centred on images of the fault rupture of the September 2010 Canterbury earthquake in New Zealand. 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. All non-text content is subject to specific conditions. For example, 3 News reported that between 4.35 a.m. and 7 a.m. the operators at Christchurch’s 111 Communications Centre, based at the Christchurch Central Police Station, took four or five times the usual number of calls – 788 rather than 172. Widely felt over the South Island and the southern North Island, it caused considerable damage in central Canterbury, especially in Christchurch. Individual businesses also suffered badly – whether from damage to stock or buildings, the impact of damage to infrastructure such as roads and utilities, or because of a decline in the demand for their services. They were to answer many more in the following days. The earthquake was felt throughout the South Island and as far north as New Plymouth. [1] The family of Lillian (Lill) Daniels-Witika believe she was a casualty of the September 2010 earthquake. It was centred 40 km west of Christchurch, near the town of Darfield, at a depth of 10 km. [6] 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. 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. A magnitude 7.1 earthquake struck the Canterbury Region of New Zealand at 4:35 am on 4 September 2010. Ground near the Darfield epicentre moved at up to 1.25 times the acceleration due to gravity. The 2010 Canterbury (Darfield) earthquake (Te Ara), Canterbury District Health Board, media updates, 4-9 September 2010, Christchurch City Council, media releases, Stan Darling and Jackie Watson, Kaiapoi shakes: interviews with Kaiapoi residents affected by the September 2010 earthquake, Jackie Watson, Christchurch, 2012, pp. The severest of those events were the earthquake (magnitude from 7.0 to … The 2010 Canterbury earthquake was a powerful 7.1 magnitude earthquake, which struck the South Island of New Zealand at 4:35 am September 4, 2010 local time (16:35 3 September UTC ). It didn’t seem that we could be of any assistance, so we left them to it; there were no doubt caregivers inside.http://www.quakestories.govt.nz/612/story/. That’s where Joan Curry was when the quake struck on 22 February 2011: After the first earthquake, on 4th September, 2010, I declared that I wouldn’t want to be in a shopping mall should another one strike – but there I was, in a mall. It was the first Canterbury earthquake which fair walloped Kaiapoi. That sequence of earthquakes was the most damaging natural disaster to occur in New Zealand in recorded history. 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. Those living near the coast soon realised that the earthquake might have caused a tsunami, and many headed for the hills or higher ground. As well as damaging properties and the local economy, the earthquake had both physical and psychological effect… Areas close to the coast were the most badly affected, especially the town of Kaiapoi in Waimakariri District and the suburb of Bexley in east Christchurch. I tried numerous times to get my son out of his cot but the shaking was so violent it was difficult to grab hold of him. And then I thought ‘My children are in Wellington! No one died as a direct result of the earthquake, and there were relatively few casualties. We did about 185 chimneys, we either made secure or we took down, so most of them had to be taken down, well probably a 50-50 split to be perfectly honest. Her family tried to revive her and to contact emergency services on overloaded phone lines. Clock stopped after September 2010 earthquake. 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 threat became grim reality on 22 February 2011. This site is produced by the History Group of the New Zealand Ministry for Culture and Heritage. It was based near Darfield but felt all over the South Island and in the lower part of the North Island. This page was last changed on 23 January 2020, at 18:34. 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