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 4:35 am local time on 4 September, and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. 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. Because this aftershock was centred very close to Christchurch, it was much more destructive and resulted in the deaths of 185 people.
The main shock on 4 September caused widespread damage and several power outages, particularly in the city of Christchurch, New Zealand's second largest city. Two residents were seriously injured, one by a collapsing chimney and a second by flying glass. One person died of a heart attack suffered during the quake, although this could not be directly linked to the earthquake. Mass fatalities were avoided partly due to there being few houses of unreinforced construction, although this was also aided by the quake occurring during the early hours of the morning when most people were off the street.
The earthquake's epicentre was 40 kilometres (25 mi) west of Christchurch, near the town of Darfield. The hypocentre was at a shallow depth of 10 km. A foreshock of roughly magnitude 5.8 hit five seconds before the main quake, and strong aftershocks were reported, up to magnitude 6.3. The initial quake lasted about 40 seconds, and was felt widely across the South Island, and in the North Island as far north as New Plymouth. As the epicentre was on land away from the coast, no tsunami occurred.
The National Crisis Management Centre in the basement of the Beehive in Wellington was activated, and Civil Defence declared a state of emergency for Christchurch, the Selwyn District, and the Waimakariri District, while Selwyn District, Waimakariri and Timaru activated their emergency operation centres. Initially, a curfew was established for parts of Christchurch Central City from 7 pm to 7 am in response to the earthquake. The New Zealand Army was deployed to the worst affected areas in Canterbury.
Insurance claims totalled between $2.75 and $3.5 billion NZD, although it is unclear how much cost can be attributed to each of the earthquake events in the 2010–2011 Canterbury Earthquake Sequence. The total estimated damage bill was up to $40 billion NZD, making it the fifth-biggest insurance event in the world since 1953.
|2010 Canterbury earthquake|
|UTC time||2010-09-03 16:35:46|
|Local date||4 September 2010|
|Local time||04:35 NZST|
|Magnitude||7.1 Mw |
|Depth||10 km (6.2 mi) |
near Darfield, Canterbury
|Areas affected||New Zealand|
|Max. intensity||X (Extreme) |
|Peak acceleration||1.26 g |
|Aftershocks||~17,600 (as of early August 2016) |
|Casualties||2 seriously injured, approximately 100 total injuries|
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.
Modelling conducted for the New Zealand Earthquake Commission (EQC) in 1991 found that earthquakes with a Mercalli intensity of VIII (significant property damage, loss of life possible) could recur on average in the Christchurch area every 55 years. The study also highlighted the dangers of soil liquefaction of the alluvial sediments underlying the city, and the likelihood of significant damage to water, sewer and power supply services.
Geologists have recognised about 100 faults and fault segments in the region, some as close as 20 km to central Christchurch. The closest faults to Christchurch capable of producing powerful earthquakes occur in the Rangiora-Cust area, near Hororata, and near Darfield. However, the 2010 quake ruptured the ground surface on a previously unknown fault and actually involved slip on up to seven individual faults
The main quake occurred as a result of strike-slip faulting within the crust of the Pacific plate, near the eastern foothills of the Southern Alps at the western edge of the Canterbury Plains. The earthquake epicentre was located about 80–90 km (50–56 mi) to the south and east of the current surface expression of the Australia–Pacific plate boundary through the island (the Alpine and Hope Faults). Though removed from the plate boundary itself, the earthquake likely reflects right-lateral motion on one of a number of regional faults related to the overall relative motion of these plates and may be related to the overall southern propagation of the Marlborough Fault System in recent geologic time. The peak ground acceleration (PGA) measured near Darfield was 1.26g (12.36 m/s2), recorded near Darfield. GNS scientists considered this an "extremely rare seismic recording made near a fault rupture". However, the February 2011 Christchurch earthquake experienced PGA of 2.2 g.
As of 7 August 2012, the area has experienced 11,000+ recorded aftershocks of magnitude 2 or more, including 26 over 5.0 magnitude, and 2 over 6.0 magnitude. Many have caused further damage to buildings in the Christchurch central business district, with some felt as far away as 300 km to the south in Dunedin.
Notable aftershocks, in chronological order, include:
GNS seismologists and geophysicists, who believed the 7.1 Mw quake consisted of three or four separate quakes, quickly proposed at least two models for the quake. The late Dr John Beavan of GNS proposed a four-fault model consisting of a 6.5 Mw quake on the Charing Cross fault, followed by a 7.0 Mw quake on the Greendale Fault, and a 6.2 Mw quake near Hororata, with a 6.5 Mw quake on the fourth fault, which could run between West Melton, Sandy Knolls and Burnham. Dr Caroline Holden proposed a three-fault model, consisting of a 6.3 Mw quake of 2 – 4 seconds on the Charing Cross fault, followed by a 6.9 Mw quake lasting 7 – 18 seconds on the Greendale Fault, and an approximately 6.5 Mw quake of 15 – 18 seconds near Hororata. Ultimately, the event appears to have been an extremely complex earthquake that involved up to seven individual faults
The Earthquake Commission has published two Geotechnical Land Damage Assessment & Reinstatement Report[s]. The first Stage-1 report was published on 21 October 2010. The report briefly describes the mechanics of the earthquake, underlying geology, residential land damage assessment, reconstruction considerations, land and building reinstatement, and remediation options.
The second Stage-2 report was published on 1 December 2010. It divides the quake-affected areas into three zones, and outlines the remediation plans for these areas.
Most of the damage was in the area surrounding the epicentre, including the city of Christchurch, New Zealand's second-largest urban area with a population of 386,000. Minor damage was reported as far away as Dunedin and Nelson, both around 300–350 kilometres (190–220 mi) from the earthquake's epicentre.
The September 2010 earthquake caused two Christchurch residents to be seriously injured, one by a falling chimney and a second by flying glass, and led to many with less serious injuries. One person died of a heart attack suffered during the quake, but doctors could not determine whether the quake was the cause.
22 February 2011 aftershock caused a large number of deaths and casualties, along with significant damage to buildings and infrastructure. Details of this damage is listed in the article on that aftershock.
Total Earthquake Commission (EQC), private insurance and individual costs may reach as high as NZ$4 billion according to the New Zealand Treasury. Another projection of the cost covered by insurance (including EQC) was lower at $2.1 billion to $3.5 billion, but would still rank the quake as the world's fifth most costly to insurers.
The Earthquake Commission covers only domestic residences with private insurance and does not provide cover for businesses. The EQC payout is limited to the first $100,000 plus GST of any individual claim, with any amount above that covered by the insurance company holding the policy. The insurance companies themselves had limited or no exposure, having offloaded most of their risk to reinsurance companies. The EQC has reinsurance of $2.5 billion with a $1.5 billion excess, so its exposure is the first $1.5 billion and any amount after the first $4 billion. It had a total fund prior to this earthquake of approx $6 billion.
Reports of the quake's intensity in Christchurch generally ranged from IV to VIII (moderate to severe) on the modified Mercalli scale. A strong smell of sulphur was widely reported in Christchurch following the earthquake. Sewers were damaged, and water lines were broken. The water supply at Rolleston, located to the southwest of Christchurch, was contaminated. Power to up to 75 percent of the city was disrupted. Christchurch Hospital was forced to use emergency generators in the immediate aftermath of the quake. About 90% of the electricity in Christchurch had been restored by 6:00 pm the day of the earthquake. The repair of electricity was estimated to be more difficult in the rural areas. One building caught fire after its electricity was turned back on, igniting leaking LPG in the building. The fire was quickly extinguished by the Fire Service before it could spread. Damage to buried pipes may have allowed sewage to contaminate the residential water supply. Residents were warned to boil tap water before using it for brushing teeth, drinking, and washing or cooking food. Several cases of gastroenteritis were reported. By 7 September 28 cases had been observed at the city's welfare centres. The boil water notice for Christchurch and Banks Peninsula was lifted late on 8 September 2010, after more than 500 tests conducted over three days found no contamination.
Christchurch International Airport was closed following the earthquake and flights in and out of it cancelled. It reopened at 1:30 pm, following inspection of the terminals and main runway. All schools and early childhood centres in Christchurch City, Selwyn and Waimakariri Districts were ordered shut until Monday 13 September for health and safety assessments. The city's two universities, the University of Canterbury and Lincoln University, and the Christchurch campus of the University of Otago were also closed until 13 September awaiting health and safety assessments.
Crime in Christchurch decreased eleven percent compared with the previous year following the earthquake, although there were initial reports of looting in the city centre and "known criminals" trying to pass off as council workers to get into the central city cordon area. Police also observed a fifty-three percent jump in the rates of domestic violence following the earthquake. Many more heart attacks than usual were reported in the days following the quake. Usually the heart unit at Christchurch Hospital handles two to three heart attacks a day, but the rate had risen to eight to ten a day since the earthquake. A record number of babies for a Saturday were born at Christchurch Women's Hospital in the twenty-four hours after the quake, with the first baby arriving six minutes after the initial shock. This was at least in part due to outlying birthing centres being closed, pending structural checks, forcing more mothers to deliver at hospitals than was generally the case.
The quake's epicentre was around Darfield, around 40 kilometres (25 mi) from Christchurch. Four metres (13 ft) of sideways movement has been measured between the two sides of the previously unknown fault.
In many towns outside Christchurch, the electrical grid was disrupted, with it taking an estimated two days to fully restore power to those affected. Power outages were reported as far away as Dunedin.
Access was restricted to over 350 homes in the town of Kaiapoi, of which about 100 were deemed unsafe. Some 22 commercial properties were deemed unsafe. According to Ron Keating, Mayor of Waimakariri District, the town "will never be the same again". As noted above, damage to buried pipes may have allowed sewage to contaminate the residential water supply, and residents were warned to boil tap water before using it for brushing teeth, drinking, and washing or cooking food. A boil water notice for most of Selwyn District was lifted on 9 September. E. coli has been found in a water sample from Kaiapoi, and a boil water notice remained in effect for parts of Waimakariri District until 19 September.
A 5 km (3.1 mi) section of rail track was damaged near Kaiapoi and there was lesser track damage at Rolleston and near Belfast. As a precaution, state rail operator KiwiRail shut down the entire South Island rail network after the earthquake, halting some 15 trains. Two locomotives running light (i.e. without any carriages or wagons) came to a stop just 30 metres short of a major buckle in the line. After inspection, services south of Dunedin and north of Kaikoura recommenced at 10:30 am that day. The Main South Line, linking Christchurch with Dunedin, was given the all-clear and reopened, albeit with a 40 km/h speed restriction north of Ashburton, just after 6 pm to allow emergency aid, including 300,000 litres (70,000 imp gal; 80,000 US gal) of drinking water, to be railed into Christchurch. By the afternoon of Monday 6 September, the entire South Island rail network had reopened with the exception of the Main North Line between Rangiora and Addington. Freight was shuttled by road between the two points, while the TranzCoastal was replaced with a coach service.
Major bridges on state highways and the Lyttelton road tunnel were inspected by the NZ Transport Agency, and found to be in structurally sound condition. The only major road closure outside Christchurch was a slip in the Rakaia Gorge, blocking State Highway 77. The slip was partially cleared by 4 pm to allow a single lane of traffic through the site. Kaiapoi's main road was closed for a few days.
The quake caused damage to historic buildings in Lyttelton, Christchurch's port town, including cracks in a church and the destruction of parts of a hotel. The Akaroa area of Banks Peninsula came through the earthquake relatively unscathed, though there was some damage to the town's war memorial and hospital and some homes were extensively damaged. Duvauchelle Hotel was also seriously affected.
In Oamaru, 225 kilometres southwest of Christchurch, the earthquake caused part of a chimney on the St Kevin's College principal's residence to fall through the house, and caused the clock atop the Waitaki District Council building to stop at 4:36am. The earthquake also caused the Dunedin Town Hall clock and the University of Otago clocktower to stop working in Dunedin, some 350 km away from the quake epicentre.
The earthquake was a wake-up call to many New Zealand residents. Two Dunedin supermarkets sold out of bottled water following the earthquake as people stocked up on emergency supplies.
Major stores across the South Island were affected as their distribution centres in Christchurch were closed. Both The Warehouse and Progressive Enterprises (owners of Countdown), which have their sole South Island distribution centres in Christchurch, had to ship essential products to their South Island stores from the North Island, while Foodstuffs (owners of New World and Pak'n Save) had to ship to all their South Island stores from their Dunedin distribution centre.
Many of the most badly affected structures in both Christchurch and the surrounding districts were old buildings, including several notable landmarks. Heritage New Zealand board member Anna Crighton said the earthquake had been "unbelievably destructive." The historic homesteads of Hororata and Homebush inland from Christchurch were both extensively damaged, as were Ohinetahi homestead and Godley House on Banks Peninsula. Homebush, located at Glentunnel 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".
The seven-storey Manchester Courts (or MLC Building), located at the busy intersection of Manchester and Hereford Streets, was extensively damaged. It was the tallest commercial building in Christchurch when it was built in 1905–06 for the New Zealand Express Company, and blended 1890s Chicago Skyscraper style with English Edwardian architecture. The building had a Category One Historic Places trust classification, but was deemed unsafe and was one of just two historic CBD buildings the City Council initially proposed for immediate demolition. That decision was reversed hours later when the building's owner proposed to dismantle the building over several weeks. Demolition began on 19 October 2010 and was continuing in late January.
The 1911 Anglican church of St. John in Hororata, five kilometres south of Glentunnel, was extensively damaged when part of its tower collapsed. The port town of Lyttelton's most notable building, the 1876 Timeball station, was also affected by the earthquake, though strengthening work completed in 2005 may have saved it from further damage. In the later Christchurch earthquake in February 2011 the building was severely damaged, and it is planned by Heritage New Zealand for it to be dismantled, with the possibility of reconstruction.
The Valley Inn Tavern in Heathcote, built in 1877, survived the initial quake, but had to be torn down after the large 5.1 magnitude aftershock. Lincoln's historic 1883 public house, The Famous Grouse, was also irreparably damaged and was demolished within days of the earthquake.
Many of Christchurch's major landmarks survived intact, including the Canterbury Provincial Council Buildings, the Anglican cathedral, and Christ's College. The Catholic Cathedral of the Blessed Sacrament (Christchurch Basilica) also survived, although it suffered severe structural damage and also had some windows broken. The central city's iconic Christchurch Press building also survived with only minor damage.
Most modern buildings performed as they were designed to do, preserving life rather than keeping the interior in good order. The City Council's own new Civic Building sustained some interior damage, mainly to fixtures and fittings that delayed it being reopened for a week. Others, such as the city's International Antarctic Centre and Christchurch Art Gallery, the latter of which served as the Civil Defence Headquarters during the earthquake aftermath, suffered little or no damage and were able to be used immediately.
The structure of the University of Canterbury's buildings survived the earthquake, but its museum collection of Greek and Roman artefacts (the Logie Memorial Collection) was significantly damaged. Also, as many of the bookshelves in the main library were toppled, with repairs expected to take until Christmas, the University arranged electronic access to many academic publishers databases for students about to sit exams.
The Oxford Terrace Baptist Church, constructed 1881–1882, was extensively damaged. Several other Christchurch area churches also suffered serious damage, including St. Mary's Anglican church in Merivale, St. John's Anglican church in Latimer Square, and the Rugby Street Methodist church.
The city's Repertory Theatre, on Kilmore Street in the central city, was reported to be extensively damaged and may be beyond repair, however the Repertory Theatre website notes "Beneath the rubble the lower façade is intact with not even a broken window. Further into the theatre everything was undisturbed; the auditorium, stage area, fly tower and dressing rooms intact. The historic proscenium undamaged."
Several notable buildings in the Timaru area, 160 kilometres (99 mi) southwest of Christchurch, were also badly affected. A pinnacle on the tower of St Mary's Anglican Church tower fell to the ground, and the recently restored tower itself sustained "significant cracking". The spire of St. Joseph's Catholic Church in Temuka was also shifted 10 centimetres (4 in) by the earthquake, leaving it precariously balanced, and the town's historic Royal Hotel was also damaged.
Heritage experts urged building owners not to hastily demolish their buildings. The mayor warned of significant penalties for demolishing buildings without consent, and launched a fund to help repair historic buildings damaged by the quake. The Government allocated NZ$10 million towards restoration of such buildings a few days later.
A feature of the quake was the damage caused by soil liquefaction. This was particularly the case in the riverside areas of Avonside, Dallington, Burwood, Avondale, and Kaiapoi, and in river delta areas near Bexley, Brooklands, Spencerville, Pines Beach, and Kairaki, with other areas being affected to a substantially lesser degree or not at all. Damage from liquefaction may have been worsened by the high water table from a wet winter.
Liquefaction can also cause buried pipes to float up to the surface. This has caused problems for the gravity-fed sewer system, which may need to be completely rebuilt in some areas.
While the problem had long been well understood by planners, it is not clear that the public understood it as well, or that it widely influenced development, buying or building decisions. Liquefaction risk at the Pegasus Town site was identified in 2005, so the developers spent approximately $20 million on soil compaction, and the ground there held firm during the quake.
The media have remarked on the lack of casualties, despite the close parallels of the quake to incidents that have had devastating consequences in other countries, such as the 1989 San Francisco quake, which killed 63 people and was magnitude 7.1 also. The analysis especially compared the Canterbury quake with the 2010 Haiti earthquake, which also occurred in similar proximity to an urban area, also occurred at shallow depth under the surface, and was of very similar strength. Unlike the many tens of thousands of deaths in Haiti (with some estimates placing the death toll at one in ten or higher), no deaths directly attributable to the earthquake were reported in New Zealand. This was ascribed to the fact that the quake happened in the early hours of a Saturday morning, when most people were asleep in timber framed homes, and "...there would almost certainly have been many deaths and serious injuries had it happened during a busy time of the day...". Another important factor was building practices which took earthquakes into account, starting after the 1848 Marlborough earthquake and the 1855 Wairarapa earthquake, both of which badly affected Wellington. These led to formal standards after the 1931 Hawke's Bay earthquake, which have since been progressively updated. By contrast, Haiti's much lower standard codes were poorly enforced and many buildings were made of hand-made non-reinforced concrete, which is extremely vulnerable to seismic damage. Ground shaking in populated areas of Canterbury was also generally less strong than for the Haiti quake.
Christchurch's emergency services managed the early stages of the emergency as the Civil Defence organisation was activated. The St John Ambulance service had sixteen ambulances operational within half an hour of the earthquake and received almost 700 calls within the first 6 hours.
Police promptly arrested a couple of opportunists who had broken into a liquor store shortly after the quake and attempted to take alcohol. Police emphasised this was only an isolated incident. The alleged offenders subsequently appeared in Court on burglary and theft charges in connection with the looting.
A state of emergency was declared for Christchurch at 10:16 am on 4 September, and the city's central business district was closed to the general public. A curfew was put in place from 7 pm to 7 am for parts of the central business district. The New Zealand Army was deployed to help the police enforce the closure and curfew.
Civil Defence also declared a state of emergency for Selwyn District and Waimakariri District. The National Crisis Management Centre in the basement of the Beehive in Wellington was activated, while Selwyn District, Waimakariri and Timaru activated their emergency operation centres.
A Royal New Zealand Air Force C-130 Hercules plane brought 42 urban search and rescue personnel and three sniffer dogs from the North Island to Christchurch the day of the quake, to help check for people buried in the rubble and determine which buildings are safe to use. There were a large number of police and engineers present in the disaster areas. The New Zealand Army deployed personnel upon the request of the Christchurch mayor. Eighty police officers from Auckland were dispatched to Christchurch to assist with general duties there.
The United Nations has contacted the New Zealand government and offered its assistance, and is being informed and kept up to date about the situation. The United States military offered to send help from Hawaii; local authorities expressed gratitude for the offer, but turn it down saying they had matters under control. The Queen asked the Prime Minister to send her good wishes to the people affected by and helping recover from the quake.
Prime Minister John Key, who was raised in Christchurch, visited the scene of the devastation within hours of the earthquake. Christchurch mayor Bob Parker requested that the Prime Minister order the deployment of the New Zealand Army to keep stability and to assist in searches when possible within Christchurch, and the Prime Minister stated that the Army was on standby. New Zealand's Earthquake Commission, which provides government natural disaster insurance, will be assisting by paying out on claims from residential property owners for damage caused by the earthquake. On 7 September, John Key appointed Cabinet Minister, Leader of the House and MP for the Christchurch electorate of Ilam Gerry Brownlee as the Minister for Earthquake Recovery to oversee the response to the earthquake.
'Welfare centres' were set up with the help of Red Cross, The Salvation Army and St. John Ambulance at Burnside High School, Linwood College and Addington Raceway, where over 244 people slept on the night after the quake. Tankers delivered drinking water to the welfare centres.
A joint mayoral relief fund has been established by Selwyn District Council, Christchurch City Council and Waimakariri District Council, to which the government has initially given NZ$5 million. The Red Cross and Salvation Army have also appealed for donations to fund their own efforts.
Under the National-led Government the Canterbury Earthquake Response and Recovery Act was drafted and passed to assist reconstruction. The Act permits Government ministers to suspend almost any New Zealand law and attracted criticism from New Zealand and international academics specialising in constitutional law, who claim that it lacks constitutional safeguards and has set a dangerous precedent for future natural disasters.
The response to the earthquake was praised by most citizens with 94% saying that Civil Defence had performed well and 90% saying the City Council had performed well.
The earthquake occurred five weeks to the day before the Christchurch local elections. Following the earthquake, the polls for the mayoral election swung from favourite Jim Anderton to incumbent Bob Parker. Parker went on to win 9 October election with a majority 53.7% of the vote.
The earthquake was reported by local, national and international news media. It made headlines in The Sydney Morning Herald, BBC News, The Guardian, NDTV, Sky News, France 24, CNN, Fox News MSNBC, and the Chilean news agency Pichilemu News, among others.
While the earthquake quickly became the only subject on talkback radio, other early coverage relied on comments from Police and other 24-hour services who were immediately affected and needed to communicate with the media. Because the earthquake occurred early on a Saturday morning, with only overnight staff on duty, it took several hours for some media outlets to give the event full live coverage. So it took until mid-morning for some media outlets to have sufficient stories and staff on duty to allow them to commence continuous live broadcasts. One television producer later observed that if the earthquake had happened just a few hours earlier, or later, they would have had a full studio crew on duty and have been able to go live immediately.
TV One simulcast hourly TVNZ 7 bulletins from 06:00 with details of the disaster, phone reports from Vicki Wilkinson-Baker, and phone interviews with Civil Defence officials. A One News special with a hosted by Miriama Kamo interrupted normal programming from 10:00–18:00 Saturday, an extended 90 minute One News at 6 pm was hosted by Simon Dallow in Christchurch and Bernadine Oliver-Kerby in the Auckland studio, Oliver-Kerby hosted hourly updates through the evening, Paul Holmes updated the story on an extended 90 minute Q&A on Sunday morning at 9 am and Oliver-Kerby hosted a special One News at Midday bulletin on Sunday afternoon.
Radio New Zealand National interrupted some normal programming to broadcast Morning Report Saturday, Midday Report Saturday, Checkpoint Saturday and Morning Report Sunday with interviews and reports of developments.
Haiti had some of the worst buildings in world.
An earthquake occurred in Christchurch on 14 February 2016 at 1:13 p.m. local time (00:13 UTC) and initially recorded as 5.9 on the Richter scale, but subsequently reviewed as 5.7. Often referred to as the Valentine's Day earthquake, it was centred in the sea off New Brighton at a depth of 15 kilometres (9.3 mi). It was the first large earthquake that the Christchurch area had experienced since May 2012, and it was part of the earthquake sequence that started with the 4 September 2010 Canterbury earthquake.A number of cliffs collapsed at Scarborough (Godley Head and Whitewash Head), Richmond Hill, and Sumner (Peacock's Gallop). The shipping containers that were still placed along Peacock's Gallop on Main Road stopped falling rocks from hitting passing cyclists. Two surfers were below Whitewash Head and had car-size rocks crash into the sea around them.Avonside
Avonside is an eastern suburb in Christchurch, New Zealand. It is one of the oldest suburbs of the city, with only Heathcote being older.Brooklands, Christchurch
Brooklands is the northernmost suburb of Christchurch, New Zealand. The settlement was built on former swamp land adjacent to Brooklands Lagoon, which forms part of the Waimakariri River mouth. The land damage sustained in the 2010 and 2011 Christchurch earthquakes and subsequent Red Zone classification resulted in the buyout and demolition of nearly all properties in Brooklands, effectively wiping the suburb off the map.Canterbury Earthquake Response and Recovery Act 2010
The Canterbury Earthquake Response and Recovery Act 2010 was a New Zealand statute designed to assist reconstruction after the 2010 Canterbury earthquake. It expired in April 2012.
The Act permitted Government ministers to suspend or make exemptions to almost any New Zealand law by Orders in Council, transferring vast lawmaking power from the legislature to the government executive. It passed with unanimous support from all political parties in Parliament, although two of the smaller parties expressed concern over the wide powers it gave ministers. The Act attracted criticism from New Zealand and international academics specialising in constitutional law who claim that it lacks constitutional safeguards and has set a dangerous precedent for future natural disasters. The group of 27 legal academics expressed their concerns in an open letter released on 28 September 2010.The New Zealand Law Society also expressed concern and suggested Parliament amend the law to ensure the vast powers it confers are not abused. Spokesman Mr Temm said the powers delegated to Ministers “are potentially at odds with maintenance of the principles of the rule of law”.The Act was repealed on 19 April 2011, when it was replaced with the Canterbury Earthquake Recovery Act 2011.Canterbury earthquake
Canterbury earthquake can refer to:
1888 North Canterbury earthquake
1901 Cheviot earthquake that caused building damage in Christchurch.
2010 Canterbury earthquake
2011 Canterbury earthquake
2016 Kaikoura earthquakeDeon Swiggs
Deon William Swiggs (born 6 September 1986, Nelson, New Zealand) is the Christchurch City Councillor representing the Central ward. Prior to Swiggs being elected, he was most well known for his participation in Rebuild Christchurch, an organisation founded after the 2010 Canterbury earthquake.Glentunnel
Glentunnel is a small village in the Selwyn District of the Canterbury region of New Zealand's South Island. It is officially recognised as a "populated area less than a town". The 2001 New Zealand census gave Glentunnel's population as 129. It is located on State Highway 77 and was served by the Whitecliffs Branch, a branch line railway, from the line's opening on 3 November 1875 through to its closure on 31 March 1962. Few remnants of the railway remain in the town, with the station's platform incorporated into the backyard of a private residence.Industrial activity such as lignite coal mining and the manufacture of pottery and bricks used to take place in the region around Glentunnel. This was the reason the railway was built, but activity declined sharply in the 20th century and has been effectively non-existent since the 1980s.The historic Deans family homestead located in Glentunnel was extensively damaged by the 2010 Canterbury earthquake, so much so that it has been described as being "practically in ruins".It has a general store, and a primary school that caters for years 1-6. A camping ground, garage, golf course and playground are also located in the town.Hororata
Hororata is a small settlement at the northwestern edge of the Canterbury Plains in the South Island of New Zealand. It is located 15 kilometres southwest of Darfield, five kilometres south of Glentunnel, and 50 kilometres west of Christchurch, on the banks of the Hororata River.
Hororata sustained some damage in the 2010 Canterbury earthquake of 4 September 2010. The settlement's most prominent building, the Anglican church of St. John, was badly affected; part of its tower collapsed onto the church's roof.Early European New Zealand pioneer John Studholme and his wife lived here before selling the run to John Hall.
New Zealand 19th century Premier John Hall and his eldest brother George Williamson Hall are buried in the St. John cemetery.Kate Sheppard National Memorial
The Kate Sheppard National Memorial, located in the city of Christchurch, is New Zealand's first memorial to the women's suffrage campaign, and particularly honours the life of one of the country's leading campaigners for women's suffrage, Kate Sheppard.The idea for the memorial was raised in 1989 as part of plans to commemorate the 100th anniversary of women's suffrage in New Zealand in 1993. A committee was formed to select a design for the memorial, and the design of Dutch-born New Zealand artist Margriet Windhausen was chosen.The memorial is a stone aggregate wall, with a life size bronze relief sculpture of Sheppard and five other women's suffrage leaders. Panels on either side of the sculpture depict scenes of everyday women's lives at the end of the nineteenth century, and carry text describing the struggle for women's suffrage. The whole structure is approximately 5 metres (16 ft) wide and 2 metres (6 ft 7 in) tall.
The women featured in the sculpture are (from left to right):
Helen Nicol, a women's suffrage campaigner who lived in Dunedin
Ada Wells, a campaigner for girls' education
Harriet Morison, an advocate for working women, also from Dunedin
Meri Te Tai Mangakāhia of Te Tai Tokerau, who approached Te Kotahitanga (the Māori parliament) for women's suffrage
Amey Daldy of the Auckland Woman's Christian Temperance Union.The group of women are depicted carrying their petition for women's suffrage to Parliament in a wooden cart.
The memorial was unveiled on 19 September 1993, the 100th anniversary of women's suffrage in New Zealand, by Dame Catherine Tizard, the Governor-General of New Zealand. A time capsule containing news articles and information on women's lives in 1993 was placed inside the monument.The memorial is located in a landscaped area known as the Kate Sheppard National Memorial Reserve, beside the Avon River and adjacent to a heritage building, Our City (the Old Municipal Chambers). This building was damaged in the 2010 Canterbury earthquake and the memorial was behind barricades while the building was assessed. In a ceremony presided over by the Mayor of Christchurch, Lianne Dalziel, in June 2014, the memorial was liberated from the barricades and public access was restored.Leeston
Leeston is a town on the Canterbury Plains in the South Island of New Zealand. It is located 30 kilometres southwest of Christchurch, between the shore of Lake Ellesmere and the mouth of the Rakaia River. The town is home to a growing number of services which have increased and diversified along with the population. Leeston has a supermarket, schools (pre-school, primary school and high school), churches, hospital (for the elderly only), gym, cafes, restaurants, medical centre, pharmacy and post office. The Selwyn District Council currently has a service office in Leeston, after the headquarters was shifted to Rolleston.
Leeston had a 2006 population of 1,299 up 8.3%, or 99 people, since the 2001 census. This is significantly above the average population growth rate in New Zealand, though not as high as centres close to Christchurch. The 2013 census returned a population of 1,506, which is 15.9% higher than the 2006 census. Population growth is expected to continue due to people leaving Christchurch as a result of the 2010 Canterbury earthquake and the 2011 Canterbury earthquake.Manchester Courts
Manchester Courts, earlier known as the MLC Building, was a commercial high-rise building in the Christchurch Central City. Built in 1905–1906 for the New Zealand Express Company, it was at the time the tallest commercial building in Christchurch. A Category I heritage building, it suffered serious structural damage in the 2010 Canterbury earthquake and was condemned to be demolished. Demolition began on 19 October, and was completed in February 2011.Marian College, Christchurch
Marian College, Christchurch was founded in 1982 with the merging of two Catholic secondary schools for girls, St Mary’s College (Sisters of Mercy, established in Colombo Street in 1893) and McKillop College (named for Mary MacKillop (St Mary of the Cross)) located in Shirley (founded in 1949 by the Sisters of St Joseph of the Sacred Heart). Both schools provided boarding and day facilities.It was decided to merge these schools into a larger Catholic secondary day school for girls which would be an integrated school under the Private Schools Conditional Integration Act 1975 and to develop it on the McKillop College site in North Parade. The Catholic Bishop of Christchurch is the proprietor of the college.
Marian College was officially opened on 25 March 1982, the feast of the Annunciation of the Lord. The first principal was Sister Eleanor Capper RSJ who left in 1996. In the nearly 30 years which have elapsed, Marian College has extended its facilities to include an assembly hall/gymnasium, a music suite, library, technology rooms’ and new classrooms. The oldest building is the administration block built in 1914 by a Doctor Louisson as a family residence until it was sold to the Sisters of St Joseph in 1949.Because of the effects of the 2010 Canterbury earthquake on 4 September 2010 and the 2011 Christchurch earthquake (the February earthquake) on 22 February 2011, the school was relocated for the 2011 school year to St Bede's College, Christchurch and there was also some cooperation with Shirley Boys' High School which is near the school. As a result of the February earthquake and the June 2011 Christchurch earthquake significant liquefaction occurred on the College site resulting in most buildings suffering differential settlement in many areas of up to 215mm. It was therefore decided to relocate the school to the site of Catholic Cathedral College (which has enough surplus capacity to accommodate the school)122 Barbadoes Street at the beginning of the 2012 school year for a period expected to be between two and four years.Mitre 10 Dream Home (series 11)
The eleventh series of Mitre 10 Dream Home premiered on 2 July 2013 at 7.30 pm on TV2. It was the first new series since the 10th series screened in 2009, with Christchurch broadcaster Simon Barnett replacing Jayne Kiely as the host. The winners were Martyn and Sarah, from the Orange Team.
The series build takes place in Kaiapoi, a satellite town of Christchurch which was badly affected by the 2010 Canterbury earthquake and the subsequent 2011 Christchurch earthquake. In October 2012, unlike previous series, the six finalist families were announced and the public were given a chance to vote for their favourite, with the family that receives the most votes securing a spot on the show. The other family was picked by the three series judges.Due to changes in the building code post-earthquake, the teams couldn't renovate a relocatable house as was done in previous series.. Instead the teams were required to design and build a house from scratch. The team colours were changed in 2013, with an orange team and a black team, consistent with the branding of series sponsor Mitre 10 Mega.Oxford Terrace Baptist Church
Oxford Terrace Baptist Church was located in the Christchurch Central City on a prominent corner property fronting the Avon River. The main building was significantly damaged in the 2010 Canterbury earthquake and collapsed in the subsequent February 2011 Christchurch earthquake. This building had a Category II listing by the New Zealand Historic Places Trust.Queen Elizabeth II Park
Queen Elizabeth II Park was a multi-use stadium in Christchurch, New Zealand, located in a large park of the same name. The stadium had a capacity of 25,000 people and was built in 1973 to host the 1974 British Commonwealth Games, with a temporary 10,000 seat western stand erected for that event to take the capacity to 35,000. The stadium suffered some damage in the September 2010 Canterbury earthquake but was able to reopen, only to be damaged beyond repair in February 2011 Christchurch earthquake. An adjacent swimming complex has also been demolished. Two high schools from the eastern suburbs will be rebuilt in Queen Elizabeth II Park adjacent to a new swimming complex.The Octagon, Christchurch
The Octagon, Christchurch, the former Trinity Church or Trinity Congregational Church designed by Benjamin Mountfort, later called the State Trinity Centre, is a Category I heritage building listed with Heritage New Zealand. Damaged in the 2010 Canterbury earthquake and red-stickered after the February 2011 Christchurch earthquake, the building was threatened with demolition like most other central city heritage buildings. In June 2012, it was announced that the building will be saved, repaired and earthquake strengthened.The Pines Beach
The Pines Beach is a small village situated roughly 4 km east of Kaiapoi in the Canterbury region of the South Island of New Zealand. It is 1 km north of the mouth of the Waimakariri River.
It takes its name from its close proximity to both a pine forest and the beach.
The Pines Beach is a relatively small town. The majority of the area consists of residential housing and a park called "The Pines Beach Oval". The village store was demolished after the September 2010 Canterbury earthquake, along with a considerable number of the houses in the village. Empty green spaces upon entering the village from Beach Road is all that remains of these earlier parts of the settlement.
The Oval is a small section of land in the centre of the town. It is in the shape of an oval and has a playground, basketball court, swings, a skate park and a BMX track. An annual gala is held on the Oval.Village Green, Christchurch
For the Queen Elizabeth Park on the Kapiti Coast, see Queen Elizabeth Park, New ZealandVillage Green is a cricket venue in Christchurch. It is a back-up first-class cricket ground in New Zealand. It was the home of the District's first class cricket team, the State Canterbury Wizards.Village Green is part of the main stadium of Queen Elizabeth II Park, and was often used for inter-provincial competition when the AMI Stadium was unavailable for use.
The stadium had been damaged after the 2010 Canterbury earthquake but was able to reopen; it was severely damaged beyond repair after the February 2011 Christchurch earthquake which has damaged the running track and recreation complex. The stadium and pool complex was demolished in 2012 after engineering reports found it beyond repair.Westpac Canterbury Centre
The Westpac Canterbury Centre (also known as the Westpac Building or Westpac Trust Building) was a landmark tower on the corner of High Street and Cashel Street in the center of Christchurch, New Zealand. Prior to the February 2011 earthquake, it was considered the 9th tallest building in Christchurch, standing at 50 meters tall (14 floors).
The building had a distinct look, with rounded concrete columns on each corner, and a pointed triangular roof. From above, it was shaped like an elongated hexagon.
† indicates earthquake resulting in at least 30 deaths
‡ indicates the deadliest earthquake of the year
Seismic faults of New Zealand