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Videos, UC QuakeStudies

A video of an interview with Rick Hellings, Managing Director of Smiths City Group, about the experiences of businesses in the aftermath of the 2010 and 2011 Canterbury earthquakes. Hellings talks about the changes in regulation and geography in Christchurch after the earthquakes and the importance of managing risks, understanding insurance, and being prepared for change. He also talks about the importance of keeping customers and business partners informed, looking after staff and customers, and reducing costs to offset the increases in rent. This video is part of a series about businesses in Christchurch after the earthquakes.

Audio, Radio New Zealand

Spud Hilton knows what it's like to feel the fear of a large scale earthquake. As the Travel Editor of the San Francisco Chronicle newspaper, he lives in a city on a fault line. Spud Hilton has just published an article in the San Francisco Chronicle about the status of Christchurch as a tourist destination and as a city that must rebuild, rethink and reinvent itself.

Images, UC QuakeStudies

A damaged house perched on the edge of the cliffs above Sumner. The photographer comments, "This house has slowly gone over the edge since the big earthquake in Christchurch in February 2011. Subsequent earthquakes has caused the rock face to crumble more and more".

Images, eqnz.chch.2010

www.youtube.com/watch?v=SPXqb7k4azU Details inside a half demolished theatre in central Christchurch. November, 2012. Christchurch, NZ. (c)Mike Brebner. All rights reserved.

Videos, UC QuakeStudies

A video of an interview with Joe Bennett, columnist and Lyttelton resident, about his experiences during the 22 February 2011 earthquake, and his hopes for post-quake Christchurch. This video was part of The Press's 'Christchurch, one year after February 22, 2011' series.

Research papers, University of Canterbury Library

This paper provides an overview of the salient aspects of the dense array of ground motions observed in the 4 September 2010 Darfield and 22 February 2011 Christchurch earthquakes. Particular attention is given to inferred physical reasons for the observed ground motions, which include: (i) source features such as forward directivity effects; (ii) The effects of the Canterbury Plains sedimentary basin on basin-generated surface waves, and waveguide effects through the region; and (iii) the importance of local site response as evidenced by observations of large long period amplification and liquefaction. The significance of vertical ground motion intensity is also examined.