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Audio, Radio New Zealand

The collapse of the Christchurch Cathedral during the devastating earthquake of February the 22nd struck a powerful blow to the core of Canterbury and New Zealand as a whole.

Images, UC QuakeStudies

A photograph of volunteers from the Wellington Emergency Management Office in Wellington Airport. The volunteers travelled to Christchurch after the 22 February 2011 earthquake to help with the emergency response.

Images, UC QuakeStudies

A stall selling mosaics of broken mirrors in the shape of houses, crosses and cathedrals. The photographer comments, "The Quake Art on sale at the AandP Show in Christchurch".

Images, UC QuakeStudies

A photograph of volunteers from the Wellington Emergency Management Office in Wellington Airport. The volunteers travelled to Christchurch after the 22 February 2011 earthquake to help with the emergency response.

Research papers, The University of Auckland Library

In the early morning of 4th September 2010 the region of Canterbury, New Zealand, was subjected to a magnitude 7.1 earthquake. The epicentre was located near the town of Darfield, 40 km west of the city of Christchurch. This was the country’s most damaging earthquake since the 1931 Hawke’s Bay earthquake (GeoNet, 2010). Since 4th September 2010 the region has been subjected to thousands of aftershocks, including several more damaging events such as a magnitude 6.3 aftershock on 22nd February 2011. Although of a smaller magnitude, the earthquake on 22nd February produced peak ground accelerations in the Christchurch region three times greater than the 4th September earthquake and in some cases shaking intensities greater than twice the design level (GeoNet, 2011; IPENZ, 2011). While in September 2010 most earthquake shaking damage was limited to unreinforced masonry (URM) buildings, in February all types of buildings sustained damage. Temporary shoring and strengthening techniques applied to buildings following the Darfield earthquake were tested in February 2011. In addition, two large aftershocks occurred on 13th June 2011 (magnitudes 5.7 and 6.2), further damaging many already weakened structures. The damage to unreinforced and retrofitted clay brick masonry buildings in the 4th September 2010 Darfield earthquake has already been reported by Ingham and Griffith (2011) and Dizhur et al. (2010b). A brief review of damage from the 22nd February 2011 earthquake is presented here

Audio, Radio New Zealand

Days after Christchurch was devastated by a 6.3 magnitude earthquake, Simon Morton traverses the city, using the Avon River as his route, and finds everyone has a story to tell.