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Images, UC QuakeStudies

Damaged buildings on Manchester Street, seen from the Tuam Street intersection. Police emergency tape cordons off the street. The photographer comments, "This was taken shortly after the 4th September earthquake. Police allowed us free access past the cordon and simply advised us to watch out for falling masonry. The access situation was much different after the February aftershock".

Images, UC QuakeStudies

A chalkboard sign outlining the programme for the evening of April 8th, 2011 at Gap Filler's "Film in the Gap!" project. The sign reads, "Gap Filler: 1st - 10th of April. Free live music and films from 5pm onwards. 5pm: Mundi, 6pm: Lindon Puffin, 7pm: Film - Draquila (90mins). Bring - cushion, chair, blanket, picnic. Coffee from 4:30pm daily. Ex demolition site. Please be safety aware. Proper footwear must be worn!". The sign is stuck to the rear wall of Mitre 10 in Beckenham.

Images, UC QuakeStudies

A chalkboard sign outlining the programme for the evening of April 10th, 2011 at Gap Filler's "Film in the Gap!" project. The sign reads, "Gap Filler: 1st - 10th of April. Free live music and films from 5pm onwards. 5pm: Plasticine Heroes, I gave These Guys 5 Bucks, 6pm: The Eastern, 7pm: Film - Candyman. Bring - cushion, chair, blanket, picnic. Coffee from 4:30pm daily. Ex demolition site. Please be safety aware. Proper footwear must be worn!". The sign was stuck to the rear wall of Mitre 10 in Beckenham.

Images, UC QuakeStudies

A police officer talks to the driver of a NZ Post truck at a cordon across Tuam Street. Military personnel stand nearby. The photographer comments, "this was taken shortly after the 4th September earthquake. Police allowed us free access past the cordon and simply advised us to watch out for falling masonry. The access situation was much different after the February aftershock".

Images, UC QuakeStudies

Two children running across the empty lot in Beckenham that housed Gap Filler's "Film in the Gap!" project. Behind them is a chalkboard sign outlining the programme for the evening of April 2nd, 2011. The sign reads, "Gap Filler: 1st - 10th of April. Free live music and films from 6pm onwards. Saturday: 5pm: The Captain Willis Trio, 6pm: Ed Muzik, 7pm: The Cracks in Everything, 8pm: Film - 4 Houses, 4 Decades (Christchurch Architecture). All welcome! Bring a blanket or cushion. Ex demolition site. Please be safety aware. Proper footwear must be worn!".

Images, UC QuakeStudies

Two men converse on the site of Gap Filler's "Film in the Gap!" project. Behind them is a chalkboard sign outlining the programme for the evening of April 2nd, 2011. The sign reads, "Gap Filler: 1st - 10th of April. Free live music and films from 6pm onwards. Saturday: 5pm: The Captain Willis Trio, 6pm: Ed Muzik, 7pm: The Cracks in Everything, 8pm: Film - 4 Houses, 4 Decades (Christchurch Architecture). All welcome! Bring a blanket or cushion. Ex demolition site. Please be safety aware. Proper footwear must be worn!".

Images, UC QuakeStudies

People walk along Tuam Street carrying bags and boxes. Brick dust covers the street where fallen bricks have been cleared, and on the left emergency tapes cordons off Manchester Street. The photographer comments, "This was taken shortly after the 4th September earthquake. Police allowed us free access past the cordon and simply advised us to watch out for falling masonry. The access situation was much different after the February aftershock".

Images, UC QuakeStudies

Members of the public at Gap Filler's "Film in the Gap!" project. Behind the pair is a chalkboard sign outlining the project's programme for the evening of evening of April 10th, 2011 at Gap Filler's "Film in the Gap!" project. The sign reads, "Gap Filler: 1st - 10th of April. Free live music and films from 5pm onwards. 5pm: Plasticine Heroes, I gave These Guys 5 Bucks, 6pm: The Eastern, 7pm: Film - Candyman. Bring - cushion, chair, blanket, picnic. Coffee from 4:30pm daily. Ex demolition site. Please be safety aware. Proper footwear must be worn!". The sign is stuck to the rear wall of Mitre 10 in Beckenham, facing inwards to the site of the project.

Images, UC QuakeStudies

Two men carry backpacks and shopping bags along Tuam Street, stepping over emergency tape that lies across the road. Brick dust covers the street where fallen bricks have been cleared. The photographer comments, "Two members of our office carrying gear through the cordon. This was taken shortly after the 4th September earthquake. Police allowed us free access past the cordon and simply advised us to watch out for falling masonry. The access situation was much different after the February aftershock".

Videos, UC QuakeStudies

A video of teachers and other staff at Christchurch schools receiving gratitude and flowers from members of the All Right? team. Ciaran Fox and some 'All Righties' (including Donovan Ryan and Jo Scott) arrive at Wainoni School and Shirley Intermediate School assemblies to launch their 'Winter Survival Kit' and share some love with a 'Little Burst of All Right'. The event was supported by BECA and the flowers were donated by Moffatts Flower Company. The Press took photographs and helped to distribute the video. All Right? posted a link to the video on their Facebook Timeline on 1 August 2014 at 4:00pm. They also published the video to YouTube on 20th November 2014.

Research papers, The University of Auckland Library

The city of Christchurch has experienced over 10,000 aftershocks since the 4th of September 2010 earthquake of which approximately 50 have been greater than magnitude 5. The damage caused to URM buildings in Christchurch over this sequence of earthquakes has been well documented. Due to the similarity in age and construction of URM buildings in Adelaide, South Australia and Christchurch (they are sister cities, of similar age and heritage), an investigation was conducted to learn lessons for Adelaide based on the Christchurch experience. To this end, the number of URM buildings in the central business districts of both cities, the extent of seismic strengthening that exists in both cities, and the relative earthquake hazards for both cities were considered. This paper will report on these findings and recommend strategies that the city of Adelaide could consider to significantly reduce the seismic risk posed by URM buildings in future earthquake

Audio, UC QuakeStudies

Part four of the audio that makes up Gap Filler's 29th project, the Transitional City Audio Tour. This part of the tour begins in the Re:Start Mall on Cashel Street and includes commentary on the performance Last Day of Mankind at the Bridge of Remembrance. The tour then moves up Oxford Terrace, along the banks of the Avon River, until it reaches Worcester Boulevard. Turning left, it travels down Worcester Boulevard, past the Christchurch Art Gallery, providing commentary on the new and old art in the area, and the Christchurch Arts Centre. Lastly, it moves up Montreal towards Cranmer Square.

Research papers, Lincoln University

On 4 September 2010, a 7.1 magnitude earthquake struck near Darfield, 40 kilometres west of Christchurch, New Zealand. The quake caused significant damage to land and buildings nearby, with damage extending to Christchurch city. On 22 February 2011, a 6.3 magnitude earthquake struck Christchurch, causing extensive and significant damage across the city and with the loss of 185 lives. Years on from these events, occasional large aftershocks continue to shake the region. Two main entomological collections were situated within close proximity to the 2010/11 Canterbury earthquakes. The Lincoln University Entomology Research Collection, which is housed on the 5th floor of a 7 storey building, was 27.5 km from the 2010 Darfield earthquake epicentre. The Canterbury Museum Entomology Collection, which is housed in the basement of a multi-storeyed heritage building, was 10 km from the 2011 Christchurch earthquake epicentre. We discuss the impacts of the earthquakes on these collections, the causes of the damage to the specimens and facilities, and subsequent efforts that were made to prevent further damage in the event of future seismic events. We also discuss the wider need for preparedness against the risks posed by natural disasters and other catastrophic events.

Research papers, University of Canterbury Library

This poster presents work to date on ground motion simulation validation and inversion for the Canterbury, New Zealand region. Recent developments have focused on the collection of different earthquake sources and the verification of the SPECFEM3D software package in forward and inverse simulations. SPECFEM3D is an open source software package which simulates seismic wave propagation and performs adjoint tomography based upon the spectral-element method. Figure 2: Fence diagrams of shear wave velocities highlighting the salient features of the (a) 1D Canterbury velocity model, and (b) 3D Canterbury velocity model. Figure 5: Seismic sources and strong motion stations in the South Island of New Zealand, and corresponding ray paths of observed ground motions. Figure 3: Domain used for the 19th October 2010 Mw 4.8 case study event including the location of the seismic source and strong motion stations. By understanding the predictive and inversion capabilities of SPECFEM3D, the current 3D Canterbury Velocity Model can be iteratively improved to better predict the observed ground motions. This is achieved by minimizing the misfit between observed and simulated ground motions using the built-in optimization algorithm. Figure 1 shows the Canterbury Velocity Model domain considered including the locations of small-to-moderate Mw events [3-4.5], strong motion stations, and ray paths of observed ground motions. The area covered by the ray paths essentially indicates the area of the model which will be most affected by the waveform inversion. The seismic sources used in the ground motion simulations are centroid moment tensor solutions obtained from GeoNet. All earthquake ruptures are modelled as point sources with a Gaussian source time function. The minimum Mw limit is enforced to ensure good signal-to-noise ratio and well constrained source parameters. The maximum Mw limit is enforced to ensure the point source approximation is valid and to minimize off-fault nonlinear effects.