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Images for CANTERBURY EARTHQUAKE; more images...

Images, UC QuakeStudies

Damage to the Visitors Centre in Kaiapoi, after the September 4th earthquake. The foundation has lifted and there are cracks along the road. Tape and fences bar the public off from access.

Images, Canterbury Museum

One 750ml green wine bottle with red coloured metal screw cap containing Mud House 2010 Marlborough Sauvignon Blanc ‘The Day the Ground Moved Like Jelly’; the front label has a drawing of an earthquake damaged house on a white background by Bella Kingi, while the label on the reverse details the fundraising effort supported by the sale of the bo...

Images, Canterbury Museum

One white cotton t-shirt with black seismograph-like patterns in the shape of ChristChurch Cathedral. Produced to commemorate the 7.1 magnitude earthquake that struck Canterbury at 4.35am on 4 September 2010. This t-shirt was designed and manufactured by Auckland based t-shirt company Mr Vintage in October 2010 to commemorate the 7.1 magnitude ...

Research papers, University of Canterbury Library

A team of earthquake geologists, seismologists and engineering seismologists from GNS Science, NIWA, University of Canterbury, and Victoria University of Wellington have collectively produced an update of the 2002 national probabilistic seismic hazard (PSH) model for New Zealand. The new model incorporates over 200 new onshore and offshore fault sources, and utilises newly developed New Zealand-based scaling relationships and methods for the parameterisation of the fault and subduction interface sources. The background seismicity model has also been updated to include new seismicity data, a new seismicity regionalisation, and improved methodology for calculation of the seismicity parameters. Background seismicity models allow for the occurrence of earthquakes away from the known fault sources, and are typically modelled as a grid of earthquake sources with rate parameters assigned from the historical seismicity catalogue. The Greendale Fault, which ruptured during the M7.1, 4 September 2010 Darfield earthquake, was unknown prior to the earthquake. However, the earthquake was to some extent accounted for in the PSH model. The maximum magnitude assumed in the background seismicity model for the area of the earthquake is 7.2 (larger than the Darfield event), but the location and geometry of the fault are not represented. Deaggregations of the PSH model for Christchurch at return periods of 500 years and above show that M7-7.5 fault and background source-derived earthquakes at distances less than 40 km are important contributors to the hazard. Therefore, earthquakes similar to the Darfield event feature prominently in the PSH model, even though the Greendale Fault was not an explicit model input.

Images, UC QuakeStudies

The Hardie and Thomson building on Sherbourne Street is on a lean, barred off with police tape and road cones, after the 4th September earthquake. The city centre is visible in the distance.

Images, UC QuakeStudies

The Hardie and Thomson building on Sherbourne Street is on a lean, barred off with police tape and road cones, after the 4th September earthquake. The city centre is visible in the distance.

Images, UC QuakeStudies

Workers survey a street in Avonside where there are large cracks, piles of liquefaction dug up from people's houses, fenced off portions of the street and an army vehicle parked, after the September 4th earthquake.

Audio, Radio New Zealand

Eleven million dollars has been donated so far to the Canterbury Earthquake Appeal. It comes as the Government announced early details of a recovery plan for people wanting money to fix their damaged homes or start rebuilding.

Videos, eqnz.chch.2010

At Greendale Faultline on Highfield Road in mid-Canterbury, where the magnitude 7.1 earthquake on 4 September 2010 originated.

Videos, eqnz.chch.2010

At Greendale Faultline on Highfield Road in mid-Canterbury, where the magnitude 7.1 earthquake on 4 September 2010 originated.