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Images for responses; more images...

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team working on the corner of Tuam and High Streets. In the background a large section of a building has collapsed and the bricks and other rubble have spilled onto the road. Wire fencing has been placed around the building as a cordon.

Images, UC QuakeStudies

A photograph of members of the Clandeboye Emergency Response Team and the Red Cross working on High Street near the intersection of Manchester Street. A digger is parked on the street in front of the workers. Behind the digger is a large pile of rubble from the ANZ Bank building.

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team examining an earthquake-damaged building on Acton Street. The closest section of the outer wall has collapsed, and the bricks and other rubble have fallen onto the pavement in front. A boat which was being stored inside has toppled over and is now sticking out of the building.

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team examining an earthquake-damaged building on Acton Street. The closest section of the outer wall has collapsed, and the bricks and other rubble have fallen onto the pavement in front. A boat which was being stored inside has toppled over and is now sticking out of the building.

Images, UC QuakeStudies

A photograph of a map used by the Wellington Emergency Management Office Emergency Response Team. The block of buildings between Montreal, Acton, St Asaph, and Antigua Streets has been outlined in red. Halkett Street has also been coloured in red. Various buildings around these areas have been highlighted in orange and blue.

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team walking down Gloucester Street towards Latimer Square. To the right, shipping containers have been stacked beside the square. A cordon of wire fences and road cones have also been used to cordon off the street in the distance.

Images, UC QuakeStudies

A photograph of a map used by the Wellington Emergency Management Office Emergency Response Team. The block of buildings between Montreal, Acton, St Asaph, and Antigua Streets has been outlined in red. Halkett Street has also been coloured in red. Various buildings around these areas have been highlighted in orange and blue.

Images, UC QuakeStudies

A photograph of the earthquake damage to the Edward Gibbon building on Madras Street. Sections of the top storey have collapsed and the bricks have spilled onto the road in front, damaging the awning and smashing several cars. In the foreground members of the Wellington Emergency Management Office Emergency Response Team are standing on the road.

Images, UC QuakeStudies

A poster created by Empowered Christchurch to advertise their submission to the CERA Draft Transition Recovery Plan on social media.The poster reads, "Submission. CERA Draft Transition Recovery Plan. After nearly five years of 'Emergency Response' where sustainability has been sacrificed in the interests of speed, we can assume that this phase is now behind us. We see no reason why this period should be extended until April 2016. Lessons must be learned from the past. It is time to move into the 'Restoration Phase'. Once seismic and building standards are corrected, and risks are notified, mapped and accepted, sustainability will be ensures. We need a city that is driven by the people that live in it, and enabled by a bureaucracy that accepts and mitigates risks, rather than transferring them to the most vulnerable residents. We support option 3+."

Research papers, University of Canterbury Library

In 2010 and 2011 a series of earthquakes hit the central region of Canterbury, New Zealand, triggering widespread and damaging liquefaction in the area of Christchurch. Liquefaction occurred in natural clean sand deposits, but also in silty (fines-containing) sand deposits of fluvial origin. Comprehensive research efforts have been subsequently undertaken to identify key factors that influenced liquefaction triggering and severity of its manifestation. This research aims at evaluating the effects of fines content, fabric and layered structure on the cyclic undrained response of silty soils from Christchurch using Direct Simple Shear (DSS) tests. This poster outlines preliminary calibration and verification DSS tests performed on a clean sand to ensure reliability of testing procedures before these are applied to Christchurch soils.

Images, UC QuakeStudies

A photograph of members of the Clandeboye Emergency Response Team and the Red Cross Team working on High Street near the intersection with Manchester Street. In the background is a large pile of rubble from the ANZ Bank building. In the foreground the members have placed their bags on a group of outdoor chairs and tables still on the footpath.

Images, UC QuakeStudies

A photograph of a member of the Wellington Emergency Management Office Emergency Response Team inside an earthquake-damaged house. The wall to the left has collapsed and has been covered with plastic sheeting. Bricks and other rubble cover the floor of the room. A chest of drawers with clothing still inside has toppled to the left and is resting on the rubble.

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team standing in front of an earthquake-damaged building on Lichfield Street. A section of the roof and the façade on the top storey of the building have collapsed and the bricks and other rubble have spilled onto the footpath and street below. USAR codes have been spray-painted on one of the bottom-storey windows and the front door.

Images, UC QuakeStudies

A photograph of the Wellington Emergency Management Office Emergency Response Team posing for a photograph on Lichfield Street. In the background is the earthquake-damaged John Burns & Co. Ltd Building. The top storey of the side wall of the building has collapsed and the rubble has spilled into the car park below. Several cars which were crushed by the falling rubble have been stacked next to the building.

Images, UC QuakeStudies

A photograph of a member of the Wellington Emergency Management Office Emergency Response Team climbing a ladder up the back of a house on Gloucester Street. The ladder has been placed against the house so that the ERT members can enter the building through the open window. To the right a section of the house next door has collapsed and the bricks have spilled onto the shed below.

Images, UC QuakeStudies

A photograph looking south down Manchester towards the intersection of Lichfield Street. In the distance members of the Wellington Emergency Management Office Emergency Response Team are standing next to a police car on Lichfield Street. Behind this there is a group of earthquake-damaged buildings which have spilled rubble onto Manchester Street. An excavator is parked on top of this rubble.

Research papers, University of Canterbury Library

In response to the February 2011 earthquake, Parliament enacted the Canterbury Earthquake Recovery Act. This emergency legislation provided the executive with extreme powers that extended well beyond the initial emergency response and into the recovery phase. Although New Zealand has the Civil Defence Emergency Management Act 2002, it was unable to cope with the scale and intensity of the Canterbury earthquake sequence. Considering the well-known geological risk facing the Wellington region, this paper will consider whether a standalone “Disaster Recovery Act” should be established to separate an emergency and its response from the recovery phase. Currently, Government policy is to respond reactively to a disaster rather than proactively. In a major event, this typically involves the executive being given the ability to make rules, regulations and policy without the delay or oversight of normal legislative process. In the first part of this paper, I will canvas what a “Disaster Recovery Act” could prescribe and why there is a need to separate recovery from emergency. Secondly, I will consider the shortfalls in the current civil defence recovery framework which necessitates this kind of heavy governmental response after a disaster. In the final section, I will examine how

Research papers, University of Canterbury Library

This research investigates the validation of simulated ground motions on complex structural systems. In this study, the seismic responses of two buildings are compared when they are subjected to as-recorded ground motions and simulated ones. The buildings have been designed based on New Zealand codes and physically constructed in Christchurch, New Zealand. The recorded ground motions are selected from 40 stations database of the historical 22 Feb. 2011 Christchurch earthquake. The Graves and Pitarka (2015) methodology is used to generate the simulated ground motions. The geometric mean of maximum inter-story drift and peak floor acceleration are selected as the main seismic responses. Also, the variation of these parameters due to record to record variability are investigated. Moreover, statistical hypothesis testing is used to investigate the similarity of results between observed and simulated ground motions. The results indicate a general agreement between the peak floor acceleration calculated by simulated and recorded ground motions for two buildings. While according to the hypothesis tests result, the difference in drift can be significant for the building with a shorter period. The results will help engineers and researchers to use or revise the procedure by using simulated ground motions for obtaining seismic responses.