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Images for paths; more images...

Images, UC QuakeStudies

A photograph submitted by Scott Thomas to the QuakeStories website. The description reads, "The site that greeted me when I finally managed to beat a path to the washhouse on 24 February 2011.".

Images, UC QuakeStudies

Photograph captioned by BeckerFraserPhotos, "Horseshoe Lake area of Burwood has that name because a loop of the Avon River encircled it in a horseshoe shape. There used to be an attractive walk alongside the loop of the River. Much of the path is now under water as the land level has subsided as a result of the earthquakes".

Images, eqnz.chch.2010

Detail of the Christchurch Anglicain Cathedral viewed from a path between the new Cashel Mall shopping area and Cathedral Square which was opened two weekends ago. This is the first time this section of the city has been open to the public since the 22 February 2011 earthquake. It will be closed off again after 11 December 2011 for the demolitio...

Images, eqnz.chch.2010

Tell me... Why This is the path I'll never tread These are the dreams I'll dream instead This is the joy that's seldom spread These are the tears... The tears we shed This is the fear This is the dread These are the contents of my head And these are the years that we have spent And this is what they represent And this is how I feel Do you know h...

Research papers, The University of Auckland Library

The Christchurch region of New Zealand experienced a series of major earthquakes and aftershocks between September 2010 and June 2011 which caused severe damage to the city’s infrastructure. The performance of tilt-up precast concrete buildings was investigated and initial observations are presented here. In general, tilt-up buildings performed well during all three major earthquakes, with mostly only minor, repairable damage occurring. For the in-plane loading direction, both loadbearing and cladding panels behaved exceptionally well, with no significant damage or failure observed in panels and their connections. A limited number of connection failures occurred due to large out-of-plane panel inertia forces. In several buildings, the connections between the panel and the internal structural frame appeared to be the weakest link, lacking in both strength and ductility. This weakness in the out-of-plane load path should be prevented in future designs.

Research papers, University of Canterbury Library

This manuscript provides a critical examination of the ground motions recorded in the near-source region resulting from the 22 February 2011 Christchurch earthquake. Particular attention is given to reconciling the observed spatial distribution of ground motions in terms of physical phenomena related to source, path and site effects. The large number of near-source observed strong ground motions show clear evidence of: forward-directivity, basin generated surface waves, liquefaction and other significant nonlinear site response. The pseudo-acceleration response spectra (SA) amplitudes and significant duration of strong motions agree well with empirical prediction models, except at long vibration periods where the influence of basin-generated surface waves and nonlinear site response are significant and not adequately accounted for in empirical SA models. Pseudo-acceleration response spectra are also compared with those observed in the 4 September 2010 Darfield earthquake and routine design response spectra used in order to emphasise the amplitude of ground shaking and elucidate the importance of local geotechnical characteristics on surface ground motions. The characteristics of the observed vertical component accelerations are shown to be strongly dependent on source-to-site distance and are comparable with those from the 4 September 2010 Darfield earthquake, implying the large amplitudes observed are simply a result of many observations at close distances rather than a peculiar source effect.