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Articles, Lost Christchurch

In response to the loss of our inner city of Christchurch, we were inspired to create this website, Lost Christchurch, as a freely accessible archive of photographs, social history and memories of …

Articles, Lost Christchurch

On this summer’s day in 1906, the ten o’clock morning tram to Sumner is about to depart from outside the Royal Exchange in Cathedral Square. An excursion to Sumner was a popular outing …

Articles, UC QuakeStudies

A patient information sheet outlining practical issues affecting members of the diabetes community in Christchurch after the 22 February 2011 earthquake. This information sheet was given to diabetes patients after the earthquake to help them manage their condition.

Articles, UC QuakeStudies

Following the February 2011 earthquake, the Canterbury Branch of the TEU surveyed members to determine the psychological and physical impact of the earthquakes on members, in particular on their working conditions and ability to participate in consultation processes. 90 members responded, and this report gives a summary of the responses to short-answer questions and overall themes.

Articles, UC QuakeStudies

Following the February 2011 earthquake, the Canterbury Branch of the TEU surveyed members to determine the psychological and physical impact of the earthquakes on members, in particular on their working conditions and ability to participate in consultation processes. 90 members responded, and this report gives a summary of the percentage of responses received for each survey question.

Articles, UC QuakeStudies

A post on the NZ Raw blog written by Mark Lincoln on 3 March 2011. Mark says, "Sydenham Church - this is the one that was demolished and then suddenly everyone started asking why it was demolished - somewhere along the line there was a communication error and a demolition company knocked down the church without speaking to the Heritage Trust".

Articles, UC QuakeStudies

A post on the NZ Raw blog written by Mark Lincoln on 24 February 2011. Mark says, "I think this is the first post I wrote after the Feb 2011 earthquake. That first photo was my first view after coming out of the office. There's a popular wide panoramic photo that someone took from the Port Hills of all of the dust rising up from the city - the photo in the blog post shows what it looked like from within the dust cloud! There are people gathering further down the street where a building has collapsed".

Articles, UC QuakeStudies

The previously unknown Greendale Fault ruptured to the ground surface, causing up to 5 metres horizontal and 1 metre vertical permanent offset of the ground, during the September 2010 Darfield (Canterbury) earthquake. Environment Canterbury commissioned GNS Science, with help from the University of Canterbury, to define a fault avoidance zone and to estimate the fault recurrence interval. There is little evidence for past movement on the fault in the past 16,000 years. However, because of the uncertainties involved, a conservative approach was taken and the fault has been categorised as a Recurrence Interval Class IV fault (a recurrence interval of between 5,000 and 10,000 years). A PhD study by a University of Canterbury student will work towards refining the Recurrence Interval Class over the next three years. Taking a risk-based approach, the Ministry for the Environment Active Fault Guidelines recommend that normal residential development be allowed within the fault avoidance zone for faults of this Recurrence Interval Class, but recommends restrictions for larger community buildings or facilities with post-disaster functions. The report is assisting Selwyn District Council in granting consents for rebuilding houses on or near the Greendale Fault that were damaged by permanent distortion of the ground due to the fault rupture in the September 2010 earthquake. The report provides specific recommendations for building on or close to the Greendale Fault, which are being implemented by Selwyn District Council. See Object Overview for background and usage information.