Earthquake in New Zealand
The 2016 Kaikōura earthquake was a 7.8 earthquake in the South Island of New Zealand that occurred two minutes after midnight on 14 November 2016 NZDT (11:02 on 13 November UTC). Ruptures occurred on multiple faults and the earthquake has been described as the "most complex earthquake ever studied". It has been subsequently modelled as having a megathrust component set off by an adjacent rupture on the Humps Fault. It was the second largest earthquake in New Zealand since European settlement.
The earthquake started at about north-east of Culverden and south-west of the tourist town of Kaikōura and at a depth of approximately . The complex sequence of ruptures lasted about two minutes. The cumulative magnitude of the ruptures was 7.8, with the largest amount of that energy released far to the north of the epicentre.
Over 45,000 insurance claims were received, resulted in a loss of NZ$2.27 billion (US$1.62 billion). There were two deaths, in Kaikōura and Mount Lyford.
Earthquake.
A complex sequence of ruptures with a combined magnitude of 7.8 started at 00:02:56 NZDT on 14 November 2016 and lasted approximately two minutes. The hypocentre (the point where the ruptures started) was at a depth of . The epicentre (the point on the Earth's surface above the hypocentre) was north-east of Culverden and from Christchurch. From the hypocentre associated with the Humps Fault, ruptures ripped northwards at a speed of , over a distance of up to . The largest amount of energy released did not occur at the epicentre, rather to the north near Seddon. Initial field surveys indicated ruptures on at least six faults, while more detailed studies confirmed ruptures on twenty-five faults. This is considered a world record for the greatest number of faults to rupture in a single earthquake event.
The earthquake was assessed as the 'most complex earthquake ever studied' and prompted the reassessment of a number of assumptions about earthquake processes. For example, the likely contribution of underground overpressured fluid to the propagation observed, required data collection and reanalysis with new earthquake models, not available to initial researchers.
There was motion on the Kekerengu Fault of up to ±, movement on the linkage Hundalee Fault of up to vertically and horizontally , a newly identified fault in Waipapa Bay, as well as minor motion on the Seaward segment of the Hope Fault, and rupture on the Humps Fault and in the Emu Plains area. The offshore continuation of the Kekerengu Fault to the north east, known as the Needles Fault, ruptured as well. NIWA marine geologist Philip Barnes said the length of the Kekerengu–Needles Fault rupture may extend for about , consisting of on land and under the sea.
Cape Campbell, at the north-eastern tip of the South Island, moved to the north-north-east by more than two metres – putting it that much closer to the North Island – and rose almost one metre. Kaikōura moved to the north-east by nearly one metre, and rose seventy centimetres. The east coast of the North Island moved west by up to five centimetres, and the Wellington Region moved two to six centimetres to the north. Christchurch moved two centimetres to the south.
Tsunami.
The tsunami that followed the Kaikōura earthquake reached a peak height of about 7 metres. The tsunami was found to be highest at Goose Bay, with data indicating a maximum run-up height above tide level at the time of the tsunami of 6.9m ±0.3m. At Oaro, the height was 5.3m ±0.3m. Marine and freshwater flora and fauna were later found scattered across the Oaro River flood plain, extending inland from the high tide mark on the day of the survey.
Immediately after the earthquake, the tide level at the Kaikōura tide gauge started dropping. Over 25minutes, it dropped about 2.5m, a classic warning sign of a tsunami. During the next 15minutes, the water level rose from its lowest level by about 4m. That was followed by a series of waves over several hours. The water level at the Kaikōura gauge rose 2.5m higher than it would have been. This was made up of a 1.5m rise measured on the gauge, and a rise of about 1m of the gauge itself, as the seabed and surrounding land rose by that amount. Some other tide gauges that recorded the tsunami were in Wellington Harbour, Castlepoint, Christchurch, and the Chatham Islands.
A tsunami estimated at five metres high struck the north-facing Little Pigeon Bay on Banks Peninsula. The bay contained only one building, an unoccupied holiday house that was pushed off its foundations and heavily damaged. In neighbouring Pigeon Bay, the tsunami was observed at about 2 am but caused no damage.
Casualties and damage.
Kaikōura and North Canterbury.
Two people died in the earthquake. A man was crushed and died when the historic Elms Farm homestead near Kaikōura collapsed. Two other people were rescued from the rubble of the house, including the man's 100-year-old mother. A woman died in a log house that was damaged at Mount Lyford. Early reports said her cause of death was a heart attack, but an autopsy later indicated it was a head injury suffered during the earthquake.
Many major roads were closed in the South Island because of slips and damage to bridges, including State Highway 1 between Picton and Waipara, and State Highway 7 between Waipara and Springs Junction (SH 65 turnoff). Most roads were cleared within 24 hours, but SH 1 between Seddon and Cheviot via Kaikōura and the Inland Kaikōura Road were closed longer. The closure of SH1, the Inland Kaikōura Road and the Main North Line railway effectively cut off all land routes into Kaikōura.
On the morning of 19 November, Kaikōura remained cut off by road due to landslides, damaged bridges and infrastructure, road subsidence, and the risk of falling debris. The NZ Transport Agency said that State Highway 1 would take months to repair, while repairs to the rail line, a key freight connection between Wellington and Christchurch, were likely to take more than a year. Parts of the diversion route via State Highways 63, 6, 65 and 7 were carrying four times their usual traffic volume.
Mains water supply was mostly restored to Kaikōura township by 19 November, but supply was in a "fragile state" and conservation was necessary. The sewage system was "severely damaged" and unusable.
On 30 November 2016, the Inland Kaikōura Road, redesignated "Kaikōura Emergency Access Road", was reopened to civilian drivers holding a permit and for restricted times of the day. Twenty-five crews had worked to clear 50 landslips on that highway alone. It reopened unrestricted to all traffic on 19 December 2016.
State Highway 1 south of Kaikōura reopened two days later on 21 December 2016, albeit only during daylight hours. Repair of the highway north of Kaikōura took substantially longer, with the repaired highway opening over a year later on 15 December 2017. The long term closure of State Highway 1 north of Kaikōura (between Mangamaunu and Clarence) resulted in a detour through the Lewis Pass being the only major route from Picton to Christchurch. This highway had to be upgraded significantly due to this increased usage.
The section of the Main North Line rail link from Picton south to Lake Grassmere reopened on 16 January 2017. The complete railway from Picton to Christchurch was not restored until 15 September 2017, though service was limited thereafter by continued landslides and repair work; passenger service did not resume until 1 December 2018.
In late 2020 the road and rail between Clarence and Oaro was finished being rebuilt and strengthened, which cost NZ$1.25 billion (US$890 million).
Three cows became stranded on an island after the surrounding ground had swept away. They made international news and have been described as celebrities. In 2017 the cows' owner published a children's book about them.
Ecological disturbance.
Uplift along the coast at Kaikōura (up to 6 metres) exposed the intertidal zone, which resulted in a large-scale die off of many organisms including "Durvillaea" bull kelp. The loss of "Durvillaea" kelp caused ecological disturbance, significantly affecting the biodiversity of the local intertidal community. Aerial drone imaging two years after the earthquake indicated that "Durvillaea" abundance remained low on reefs with significant uplift, but it revealed offshore refuge populations less frequently detected by field researchers. Genomic research sampling "D. antartica" populations before and after the 2016 earthquake indicates that the original populations have managed to survive and are dominating the initial recolonisation process along the newly formed intertidal coastline. However, "D. antarctica" remains sparse and further change in genetic diversity is possible over the next coming decades.
The Hutton's shearwater ("Puffinus huttoni") colony in the Seaward Kaikōura ranges was extensively damaged by the earthquake. Large landslides buried up to 20% of the existing colony areas. Extensive shaking damaged the integrity of many burrows in the remaining shingle and soil tussock-covered habitat used by these alpine nesting seabirds. The birds were at the peak of egg laying in mid-November and with the quake happening at midnight there would have been considerable losses of birds nesting within breeding burrows. The earthquake also buried one of the two boulders remaining inhabited by the eyelash seaweed, with the condition of the other 4 km away being unknown. The species has not been found in the wild since the earthquake, and it may now be extinct.
Wellington.
In the city of Wellington, buildings were damaged, several beyond repair. Damage to docks briefly halted ferry traffic across Cook Strait; more significantly, container shipping did not resume for over ten months. The Wellington City Council was given special powers to require reports from building owners, and there were doubts about application of the rules. Several buildings were closed temporarily because of doubts about stairwells. In Lower Hutt, a cinema complex and part of the carpark in the Queensgate Shopping Centre were deemed unsafe and were demolished. At Ava railway station, one of the pedestrian access ramps was damaged and was removed during the weekend of 17 and 18 December, leaving the station without wheelchair access; the ramp was rebuilt and reopened in October 2018.
A 54-year-old nine-storey office block, the former ICI Building at 61 Molesworth Street, was demolished during December 2016 after fears that it could collapse. The damaged Reading Cinema parking building off Courtenay Place was demolished during January 2017. Both building failures resulted in part of the adjacent streets (Molesworth Street and Tory Street) being closed off for a period. The Courtenay Central Reading Cinema complex closed due to minor damage, reopened in March 2017 then closed again on 5 January 2019 after further assessment. As of July 2024 it is still standing but closed.
By February 2017, business insurance claims had passed NZ$900 million (US$641 million). The Wellington Region had two thirds (65%) of the total losses, followed by the upper South Island at 25%, Canterbury at 8% and the remaining 2% from elsewhere in the North Island.
In 2016 and 2017 it was decided that several other buildings would be demolished, not repaired: the Figaro Block of the Malvina Major Retirement Village in Burma Road, Johnsonville, the eleven year old, seven-storey NZDF headquarters, and Statistics House owned by CentrePort and built in 2005 on the waterfront. Several buildings failed because of unsatisfactory design features or collapse of building services in buildings constructed only in the previous decade.
BNZ Harbour Quays, a large building on Waterloo Quay leased to the BNZ, was badly damaged in the earthquake and in 2018 the building's owner CentrePort announced that it would be demolished. This building was opened in 2009 and demolished during 2019. BNZ then sued the Wellington City Council for negligence for granting building consents and issuing code compliance certificates, since concerns about the building's design had been raised by reviewing engineers before construction began. The building had previously suffered damage during the 2013 Seddon earthquake.
Wellington Central Library was not damaged during the Kaikōura earthquake but closed suddenly on 19 March 2019 after engineers reassessed it in light of new understanding about building performance gained from the 2016 quake. As of March 2023, the building has been gutted and strengthened and is expected to reopen in 2026.
Demolition of the Civic Administration Building in Te Ngākau Civic Square started in April 2024.
Christchurch.
Several houses in the coastal suburb of New Brighton in Christchurch were looted after the occupants left because of tsunami risk.
Regional effects.
Schools and universities across the region were told to remain closed until the situation could