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Images for earthquake liquefaction; more images...

Images, Canterbury Museum

One landscape colour digital photograph taken on 6 September 2010 showing liquefaction in Hagley Park. Liquefaction is the name of the process where water pushes sand and silt above ground. These puddles of sand and silt are left above ground. Liquefaction caused huge problems when it occurred in residential suburbs as was as likely to push thr...

Images, UC QuakeStudies

Liquefaction-damaged carpets removed from a residential propoerty in Pines Beach, after the September 4th earthquake.

Research papers, University of Canterbury Library

On 4 September 2010, a magnitude Mw 7.1 earthquake struck the Canterbury region on the South Island of New Zealand. The epicentre of the earthquake was located in the Darfield area about 40 km west of the city of Christchurch. Extensive damage was inflicted to lifelines and residential houses due to widespread liquefaction and lateral spreading in areas close to major streams, rivers and wetlands throughout Christchurch and Kaiapoi. Unreinforced masonry buildings also suffered extensive damage throughout the region. Despite the severe damage to infrastructure and residential houses, fortunately, no deaths occurred and only two injuries were reported in this earthquake. From an engineering viewpoint, one may argue that the most significant aspects of the 2010 Darfield Earthquake were geotechnical in nature, with liquefaction and lateral spreading being the principal culprits for the inflicted damage. Following the earthquake, an intensive geotechnical reconnaissance was conducted to capture evidence and perishable data from this event. This paper summarizes the observations and preliminary findings from this early reconnaissance work.