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Images, Alexander Turnbull Library

A weather map of New Zealand is shown beset with dreadful weather conditions that include cyclones and lightning strikes; there is also earthquake activity round the Canterbury region. Text reads 'Mother Nature's wild child... but who's the father?' Refers to the Canterbury earthquake of 4th September 2010 and the spring storms with wind, rain and snow in recent weeks. Quantity: 1 digital cartoon(s).

Images, Alexander Turnbull Library

A weather map of New Zealand is shown beset with dreadful weather conditions that include cyclones and lightning strikes; there is also earthquake activity around the Canterbury region. Text reads 'Now all we need is a plague of locusts...' Refers to the Canterbury earthquake of 4th September 2010 and the spring storms with wind, rain and snow in recent weeks. Quantity: 1 digital cartoon(s).

Images, Alexander Turnbull Library

Two huge wrestlers, one representing 'Port Hills fault' and the other 'Greendale fault' struggle together over a broken Christchurch. Another wrestler, representing 'Other faults' appears in the distance yelling 'Is it my turn yet?' Context - Christchurch has now had three major earthquakes and thousands of aftershocks. It now appears likely that the Christchurch quakes resulted from activity on a fault extending directly eastward from the Alpine fault that remained unknown until last year, says Roger Musson, a seismologist at the British Geological Survey in Edinburgh. The new fault first came to light last September (4th) when a stronger but less calamitous quake shook Darfield, 40 kilometres west of Christchurch. Musson says the latest quake (Feb 22, 2011) probably resulted from an eastward continuation of activity on the same fault. "It has probably not moved for tens of thousands of years, so lots of strain built up," says Musson. The third major quake happened on 13th June 2011. (New Scientist - February 22, 2011) Quantity: 1 digital cartoon(s).

Research Papers, Lincoln University

There is a critical strand of literature suggesting that there are no ‘natural’ disasters (Abramovitz, 2001; Anderson and Woodrow, 1998; Clarke, 2008; Hinchliffe, 2004). There are only those that leave us – the people - more or less shaken and disturbed. There may be some substance to this; for example, how many readers recall the 7.8 magnitude earthquake centred in Fiordland in July 2009? Because it was so far away from a major centre and very few people suffered any consequences, the number is likely to be far fewer than those who remember (all too vividly) the relatively smaller 7.1 magnitude Canterbury quake of September 4th 2010 and the more recent 6.3 magnitude February 22nd 2011 event. One implication of this construction of disasters is that seismic events, like those in Canterbury, are as much socio-political as they are geological. Yet, as this paper shows, the temptation in recovery is to tick boxes and rebuild rather than recover, and to focus on hard infrastructure rather than civic expertise and community involvement. In this paper I draw upon different models of community engagement and use Putnam’s (1995) notion of ‘social capital’ to frame the argument that ‘building bridges’ after a disaster is a complex blend of engineering, communication and collaboration. I then present the results of a qualitative research project undertaken after the September 4th earthquake. This research helps to illustrate the important connections between technical rebuilding, social capital, recovery processes and overall urban resilience.

Audio, Radio New Zealand

Fran Vertue is a Clinical Psychologist with experience in truama counselling. She speaks about how to handle children dealing with the trauma of the Canterbury earthquake.