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Home / New Zealand

Wellington earthquake: Capital spared 'direct hit'

Natalie Akoorie
By Natalie Akoorie
Local Democracy Editor·NZ Herald·
21 Jul, 2013 05:30 PM5 mins to read

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People recount their experience of the 6.5 earthquake that was felt across New Zealand.
Damage could have been worse but chance remains of bigger shake, scientist says.

The faultline causing earthquakes in Cook Strait has a history of producing "swarms" of quakes, but none that have been devastating in the hundreds of years since records began.

The earthquakes that shook Wellington three times on Friday and twice yesterday - the highest at magnitude 6.5 last night - and the following aftershocks resulted from the squeezing of the city in the boundary between the Pacific and Australian tectonic plates.

Countdown supermarket in Lower Hutt after the earthquake. Photo / Kim D
Smashed glass along Featherston St in Wellington. Photo / Teuila Fuatai
Broken bottles litter the floor of Regional Wines and Spirits in Wellington after the quake struck. Photo / SNPA
Concrete from a facade on the footpath outside the Featers Tavern in Featherston Street, after the severe quake shook the city. Photo / SNPA
Parts of the wharf are cracked. Photo / Felix Marwick
Fallen concrete on Featherston Street.  Photo / H du Plessis-Allan
Bottles have fallen from shelves at a local wine shop. Photo / @Yorrike
A local deli after the earthquake struck. Photo / @ Yorrike
Fallen concrete on Featherston Street. Photo / Alfonso Bezanilla
Broken windows at The Quest on Willis Street. Photo / @kalena
The ground is cracked at Wellington wharf. Photo / @kirkburgess
People cover under tables at Wellington Airport after a large earthquake. Photo / Greg Bowker
Students examine a crack on the ground on the wharf on the waterfront after a 6.5 magnitude earthquake hit Wellington. Photo / AFP
The entrance to Featherston Street is cordoned off after sustaining earthquake damage. Photo / Getty Images
Broken bottles litter the floor of Regional Wines and Spirits after a 6.5 earthquake shock Wellington. Photo / Ross Setford
Inside the BNZ Harbour building. Photo / Tracey Earl
A damaged house east of Seddon. Photo / Sam Swain
A damaged house east of Seddon. Photo / Sam Swain
Earthquake damage showing large section of seafront collapsed into Lambton Harbour. Photo / M H Pryce
Earthquake damage showing large section of seafront collapsed into Lambton Harbour, including a container, spare Barrett Reef buoy, and two recreational fishing shelters. Photo / M H Pryce
Showing mass of floating debris, but retained by an old oilspill floating boom. Photo / M H Pryce
Damageto a Featherston Street building as a result of the earthquake in Wellington. Photo / Mark MItchell
CentrePort staff inspect the damage as a result of the earthquake in Wellington. Photo / Mark Mitchell
City council workers cleaning up debris from damage as a result of the earthquake in Wellington. Photo / Mark Mitchell
Damage to two Featherston Street buildings as a result of the earthquake in Wellington. Photo / Mark Mitchell
CentrePort staff inspect the damage as a result of the earthquake in Wellington. Photo / Mark Mitchell
CentrePort staff inspect the damage to their reclaimed container wharf as a result of the earthquake in Wellington. Photo / Mark Mitchell
City council workers cleaning up debris from damage as a result of the earthquake in Wellington.  Photo / Mark Mitchell
An empty shipping container sits in the harbour where the land fell into the sea at the Port Wellington Container terminal. Photo / AFP
Large cracks are seen in the road near where the land fell into the sea at the Port Wellington Container terminal. Photo / AFP
Large cracks are seen in the road near where the land fell into the sea at the Port Wellington Container terminal. Photo / AFP
A glazier repairs broken windows in Wellington following an earthquake on July 21. Photo / AFP
Traffic warnings are displayed on a sign along a motorway heading to Wellington. Photo / AFP
The fire service remove loose metal sheeting from the side of a high rise building in Wellington. Photo / AFP
An empty shipping container sits in the harbour where the land fell into the sea at the Port Wellington Container terminal. Photo / AFP
Supermarket workers clean up after a 6.5 magnitude earthquake hit Wellington. Photo / AFP

Image 1 of 39: Countdown supermarket in Lower Hutt after the earthquake. Photo / Kim D

Director of Earthquake Engineering at Beca, Dr Richard Sharpe said he did not expect yesterday's earthquakes to have much effect on buildings, but predicted it would provoke engineering checks.

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"In general New Zealand is very resilient to this type of earthquake. This type of shaking occurring in other countries with very brittle buildings might have caused a lot more mayhem than today," Sharpe said.

Victoria University professor of geophysics Euan Smith said the interface between the overlying Australian and underlying Pacific plates was a significant fault.

"Its potential is that it could have big earthquakes," Smith said.

"We have no historical record and no recent, unequivocal geological record of a big earthquake for many hundreds of years, so we simply don't know how often really big earthquakes may happen on this structure."

Professor Smith said residents should be "sensibly concerned" because a severe earthquake was completely unpredictable.

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However, he said the latest seismic activity was similar to a swarm of smaller earthquakes which struck Wellington in January 1950.

Those 30 earthquakes were above magnitude 3 and also occurred in Cook Strait, about 50km northwest of the current epicentre.

"They could go on as the 1950 swarm did for a month. Or they could be all over, though I think that's very unlikely."

Yesterday there were more than five aftershocks, with one measuring 4.9 on the Richter scale before the magnitude 6.5 hit shortly after 5pm.

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"We're having a succession of breaks of little patches on the same fault."

Professor Smith said a large earthquake could not be ruled out because earthquakes were unpredictable.

However, he thought the chances of a significant event were less than 10 per cent.

The difference between this weekend's earthquakes, centred east of Seddon and at its lowest 11km deep, and Christchurch's devastating 2011 quake which killed 185 people, was that it was a "direct hit".

"If these earthquakes on Friday and today had been centred right under Wellington there would have been some damage.

"These are distinctly smaller than the February 22 earthquake in Christchurch but if they'd been right under our feet instead of 40km away they would have been much nastier."

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Professor Smith said homeowners should properly secure property or possessions which could fall and be damaged or injure someone.

"Earthquakes hurt people when things fall on them."

GNS Science duty seismologist Anna Kaiser called the weekend's activity an "earthquake doublet".

She said there had been several earthquakes over magnitude 5 in the past decade alone, including a swarm pattern in 2005.

"If you go back to 1977 there was a magnitude 6 in a very similar location so it's a known area on our radar in terms of earthquakes."

More or bigger quakes could not be ruled out.

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- Additional reporting Morgan Tait

Wellingtonians in for nervous nights

Registered psychologist Nerys Parry, who lives in Petone, Wellington said yesterday's big quake would leave residents scared and worried.

"I think people will be feeling cautious. Some will be feeling quite frightened and many will be thinking, 'What if?'

"I think some will face sleepless nights. If there's a heavy truck rumbling by, they'll very likely startle and sit up and think, 'Oh my gosh it's happening again'," Ms Parry said.

"People will be taking what precautions they can prior to going to bed and they'll talk to each other about what to do if there's another earthquake during the night. There will also be a lot of nervous laughter."

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Last night, Cantabrians swarmed social networking sites to send their love, support and advice to quake-affected residents further north.

Many provided practical tips such as having an updated earthquake kit, carrying cash, making sure cellphones were charged and sleeping in clothes with shoes next to the bed.

Ms Parry said Wellingtonians should be preparing themselves and making sure their families would be okay in the event of another quake.

Organising a survival kit, having a large water container, making sure pets would be taken care of and keeping a backpack with a change of clothes next to the bed were all practical things people should be doing.

Notable earthquakes

*Wellington 1855 on the Wairarapa Fault, thought to be the magnitude 8.3
*North Canterbury 1888 Hope Fault, 7.3
*Buller 1929 White Creek Fault, 7.8
*Hawkes Bay 1931 overlying Australian plate, 7.8
*Edgecumbe 1987 Edgecumbe fault, 6.3
*Fiordland 2009 underlying Australian plate, 7.8
*Darfield 2010 Greendale Fault, 7.1
*Christchurch 2011 unknown fault under Banks Peninsula, 6.3

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- Vaimoana Tapaleao

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