2010 canterbury earthquake facts

View of the Oxford Terrace Baptist Church after the 2010 Canterbury earthquake, with props holding the frontage up (It was later destroyed in the 22 February aftershock). However, this may be revised when a clearer picture emerges of the extent of the damage not only to buildings but infrastructure such as sewerage and water supply networks. Sampling included organisations proximal and distal to the fault trace, organisations located within central business districts, and organisations from seven diverse industry sectors.     At least 15,899 people died, and another 2,500 went missing. GNS Science. Earthquakes in Christchurch today and historic (Canterbury, Christchurch City, , New Zealand) Map of the most recent 25 earthquakes in Christchurch and Canterbury, New Zealand.Christchurch Quake Map. The Canterbury quake caused extensive damage to certain buildings in Christchurch, in addition landslides occurred in the Rakaia Gorge and flooding where the Hororata River had burst its banks. 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. Geotechnical Reconnaissance of the 2010 Darfield (New Zealand) Earthquake, Report. No one died, but buildings in Christchurch were damaged. No lives were lost, but buildings were damaged and deemed unsafe leading to a state of emergency being pronounced in the city of Christchurch. Liquefaction is a phenomenon in which the strength and stiffness of a soil is reduced by extreme shaking. These MPs represent 65 general electorate seats and seven Māori electorates. Darfield earthquake damages Canterbury. 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. In the United States, a magnitude 7.0 tremor struck near Anchorage, Alaska on November 30. losses totaled more … During the Canterbury earthquake liquefaction and lateral spreading (sideways movement of the ground) occurred in the Kaiapoi area and some of Christchurch's eastern suburbs. Tension builds up as they scrape over, under or past each other. The scale quantifies the intensity of ground-shaking and destructiveness of an earthquake from MM1 (smallest) to MM12 (cataclysmic). Other areas, where the movement is not constant, are prone to stronger quakes separated by longer periods of time. For more information about tours and visiting Parliament, click here. There was no loss of life and few serious injuries, but many stone and masonry buildings were damaged. Sometimes excess water will come to the surface through cracks bringing liquefied sand with it, creating what are known as sand boils or sand volcanoes. 2). After the 2010 Canterbury Earthquake, a 7.1 magnitude earthquake near Christchurch, New Zealand, the region has been hit by hundreds of aftershocks - many of them widely felt around Christchurch, and some of which have caused further damage. In the first eighty years of European settlement in Christchurch (1850–1930), four earthquakes caused significant damage, the last of these centred at Motunau on the North Canterbury coast in 1922. Some damaging aftershocks followed the main event, the strongest of which was a magnitude 6.3 shock known as the … Elisabeth Bowman. Central Kaiapoi suffered major damage; many of the town's buildings had to be bulldozed as a result of the 2010 earthquake and subsequent quake in February 2011. In the South Island, these plates mainly slide past each other horizontally, producing earthquakes along fault lines such as the Alpine fault. Less than 6 months later, another earthquake struck within a few kilometers of Christchurch city. These plates are in constant motion, travelling at a few centimetres per year. Businesses in the city centre were closed the day of the quake. 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. Although it is impossible to predict the exact timing of the next big quake, scientists will increase their knowledge of the statistical risks and potential size of future earthquakes. 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. The 2010 Canterbury earthquake measured 7.1 on the Richter Scale and struck the South Island of New Zealand at 4:35 am on the 4th of September 2010. In contrast the Fiordland earthquake on 15 July 2009 of magnitude 7.8, was given an intensity measurement of MM7 because it occurred in an isolated area and there was only a small amount of damage to buildings reported in Invercargill. Public servants and special interest groups, http://www.geonet.org.nz/about/index.html, http://www.geonet.org.nz/news/article-sep-4-2010-christchurch-earthquake.html, http://www.gns.cri.nz/Home/News-and-Events/Media-Releases/Most-damaging-quake-since-1931/Canterbury-quake, http://creativecommons.org/licenses/by/3.0/nz/, http://www.gns.cri.nz/Home/News-and-Events/Media-Releases/Text-book-aftershock, Parliamentary.Information@parliament.govt.nz. Parliamentary.Information@parliament.govt.nz. 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). During the 2010 and 2011 Canterbury earthquakes, over 400 000 tonnes of silt came to the surface, covering streets and gardens in several suburbs. Around six months later, at 12:51 pm on 22 February 2011, a magnitude 6.3 earthquake hit south-east of Christchurch. Earthquake Commission and GNS Science. See more ideas about earthquake, natural disasters, earthquake and tsunami. The Canterbury earthquakes are in no way related to the flooding events in Queensland or the massive earthquake in Japan. The main quake was felt widely across the South … on the 4th of september there was a 7.1 magnatude earthquake hit canterbury with around 200 aftershocks so far. 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). Liquefaction is not just a New Zealand problem. Schwede 66 02:35, 4 September 2010 (UTC) I agree. The other 48 MPs are selected from the party lists. Aftershock sequences follow predictable patterns based on seismological observations and mathematical modelling. The Canterbury region has had six months of unexpected and extremely difficult challenges as a result of a sequence of damaging and deadly earthquakes and the associated aftershocks. Luck played a part-the quake occurred at … The 1855 Wellington and 1931 Napier earthquakes were both MM10 at their epicentres. There have been thousands of aftershocks in Canterbury since the 2010 earthquake. On 4 September 2010 Canterbury was affected by a magnitude 7.1 earthquake. Latest earthquake is #25940 being magnitude 2.43 ( II) at 33.12 km at 12:10am, about 23 hr 8 mins ago. Tourism infrastructure in Canterbury and Christchurch is operating as usual. GeoNet. On June 17 another strong earthquake impacted Osaka Japan, resulting in insured losses of at least $935 million. In general, aftershocks decline in magnitude and frequency, as the distance increases from the epicentre of the main quake. , resulting in insured losses of at least 15,899 people died, and another went... On 4 September 2010 has been named the Greendale, Darfield, at a depth of km... Parliament, click here five to ten years 7.1 magnatude earthquake hit Canterbury with around 200 aftershocks far... Schwede 66 02:35, 4 September 2010, there was a New Zealand Crown entity in... Of ground-shaking and destructiveness of an earthquake, which is a measure of main., causing frequent small or moderate earthquakes 6160T: +64 4 817 9647 @... 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