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Images for earthquake response; more images...

Articles, UC QuakeStudies

Following the February 2011 earthquake, the Canterbury Branch of the TEU surveyed members to determine the psychological and physical impact of the earthquakes on members, in particular on their working conditions and ability to participate in consultation processes. 90 members responded, and this report gives a summary of the responses to short-answer questions and overall themes.

Images, UC QuakeStudies

A photograph of members of the Wellington Emergency Management Office Emergency Response Team in the hanger of a Royal New Zealand Air Force Hercules. The ERT members are travelling to Christchurch to help out in the emergency response to the 22 February 2011 earthquake. Blankets, tent poles, and other supplies have been stacked in the centre of the hanger.

Images, UC QuakeStudies

Members of the USAID Disaster Assistance Response Team (DART) and the New Zealand Urban Search and Rescue, breaking through the floor of a building which was severely damaged during the 22 February 2011 earthquake.

Images, UC QuakeStudies

A photograph of an ICOM IDAS Repeater next to the information for the Civil Defence Response Team networks. The IDAS is a digital land mobile radio system which retransmits radio signals. It was used by the Civil Defence to extend the range of their digital radios during the emergency response to the 22 February 2011 earthquake.

Audio, Radio New Zealand

Our correspondent Motoko Kakubayashi on Japan's response to the Christchurch earthquake, being that it appears that a number of Japanese students will be counted as fatalities.

Images, UC QuakeStudies

Members of the Disaster Assistance Response Team outside the US headquarters in Latimer Square. Latimer Square was set up as a temporary headquarters for emergency management personnel after the 22 February 2011 earthquake.

Images, UC QuakeStudies

A photograph of a member of SPCA helping a member of Massy University's Veterinary Emergency Response Team (VERT) to load medical supplies into their vehicles. VERT travelled to Christchurch after the 22 February 2011 earthquake in order to assist with caring for animals.

Images, UC QuakeStudies

Members of the USAID Disaster Assistance Response Team (DART) and New Zealand Urban Search and Rescue breaking through the floor of a building which was severely damaged during the 22 February 2011 earthquake.

Images, UC QuakeStudies

Members of the USAID Disaster Assistance Response Team (DART) and New Zealand Urban Search and Rescue breaking through the floor of a building which was severely damaged during the 22 February 2011 earthquake.

Images, UC QuakeStudies

Members of the USAID Disaster Assistance Response Team (DART) photographed with their team leader, Al Dwyer, Prime Minister John Key, and Canterbury Earthquake Recovery Minister Gerry Brownlee, outside the US headquarters in Latimer Square.

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.