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Images, UC QuakeStudies

A photograph submitted by Caroline Oliver to the QuakeStories website. The description reads, "Demoilition of one of the 2 damaged chimneys, Cashmere hills 1920 weatherboard house, in March 2011.".

Images, UC QuakeStudies

A photograph submitted by Caroline Oliver to the QuakeStories website. The description reads, "Demoilition of one of the 2 damaged chimneys, Cashmere hills 1920 weatherboard house, in March 2011.".

Images, UC QuakeStudies

A photograph submitted by Caroline Oliver to the QuakeStories website. The description reads, "Demoilition of one of the 2 damaged chimneys, Cashmere hills 1920 weatherboard house, in March 2011.".

Images, UC QuakeStudies

A photograph submitted by Caroline Oliver to the QuakeStories website. The description reads, "Demoilition of one of the 2 damaged chimneys, Cashmere hills 1920 weatherboard house, in March 2011.".

Images, UC QuakeStudies

A photograph submitted by Caroline Oliver to the QuakeStories website. The description reads, "Demoilition of one of the 2 damaged chimneys, Cashmere hills 1920 weatherboard house, in March 2011.".

Articles, UC QuakeStudies

A digital photograph in PDF format with caption. Image looks south down Kingsford street. Port hills on the horizon with potholes in the foreground that progressively got worse after the Feburary 2011 earthquake.

Images, UC QuakeStudies

A view down Papanui Road to Victoria Street, with the Port Hills in the background. The road is closed at the intersection of Victoria Street and Bealey Avenue, and diggers are working beside a damaged building.

Research Papers, Lincoln University

Numerous rockfalls released during the 2010–2011 Canterbury earthquake sequence affected vital road sections for local commuters. We quantified rockfall fatality risk on two main routes by adapting a risk approach for roads originally developed for snow avalanche risk. We present results of the collective and individual fatality risks for traffic flow and waiting traffic. Waiting traffic scenarios particularly address the critical spatial-temporal dynamics of risk, which should be acknowledged in operational risk management. Comparing our results with other risks commonly experienced in New Zealand indicates that local rockfall risk is close to tolerability thresholds and likely exceeds acceptable risk.