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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.

Videos, UC QuakeStudies

A video about the 4 September 2010 earthquake, produced for the anniversary of the earthquake. The video includes footage of the earthquake damage to the Christchurch city centre, Darfield, Rolleston, and Hororata. It also includes footage of diggers clearing stock in the Canterbury Brewery on St Asaph Street, engineers checking buildings in town, and a fire on Worcester Street.

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.

Images, Alexander Turnbull Library

The cartoon shows a man, a woman and a dog all yelling with fright. Refers to the series of severe aftershocks that again rocked Christchurch on January 2nd. The largest was a magnitude-5.5 shake shortly before 6am. All were centred at sea off New Brighton. Mayor Bob Parker said that fear that larger quakes could be triggered had been raised by residents, but the tsunami threat was "highly unlikely". Quantity: 1 digital cartoon(s).

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.