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Images, UC QuakeStudies

Photograph captioned by Fairfax, "Earthquake Commission Public Meeting at the SBS Events Centre. Reid Stiven, representing the Earthquake Commission (EQC), responds to a query during the meeting, which was held to inform the public about making claims to the EQC relating to the 7.1 magnitude earthquake on 4 September. The meeting was hosted by Rangitata MP Jo Goodhew (left)".

Images, UC QuakeStudies

Photograph captioned by Fairfax, "Earthquake Commission Public Meeting at the SBS Events Centre. Left to right: Rangitata MP Jo Goodhew and Reid Stiven, representing the Earthquake Commission (EQC), listen to a query during the meeting, which was held to inform the public about making claims to the EQC relating the 7.1 magnitude earthquake on 4 September".

Images, UC QuakeStudies

Photograph captioned by Fairfax, "Earthquake Commission public meeting at the SBS Events Centre. Left to right at back: Rangitata MP Jo Goodhew and Reid Stiven, representing the Earthquake Commission (EQC), listen to a query during the meeting, which was held to inform the public about making claims to the EQC relating to the 7.1 magnitude earthquake on 4 September".

Images, UC QuakeStudies

Photograph captioned by Fairfax, "Earthquake Commission Public Meeting at the SBS Events Centre. Reid Stiven, representing the Earthquake Commission (EQC), responds to a query during the meeting, which was held to inform the public about making claims to the EQC relating the 7.1 magnitude earthquake on 4 September. The meeting was hosted by Rangitata MP Jo Goodhew (left)".

Audio, Radio New Zealand

Topics - A couple of New Zealand women, determined to carry on clubbing with kids, have launched the first New Zealand-based"Baby Loves Disco"franchise in Auckland's Viaduct. The"sheer strength and power"of the September the 4th earthquake has more than doubled the number of reported supernatural events in Canterbury, according to a paranormal investigator. The 2010 Census of Women's Participation reveals that female participation in governance, professional and public life is slipping away - erasing gains made in the past decades.

Research papers, University of Canterbury Library

This paper presents site-specific and spatially-distributed ground-motion intensity estimates which have been utilized in the aftermath of the 2010-2011 Canterbury, New Zealand earthquakes. The methodology underpinning the ground motion intensity estimation makes use of both prediction models for ground motion intensity and its within-event spatial correlation. A key benefit of the methodology is that the estimated ground motion intensity at a given location is not a single value but a distribution of values. The distribution is comprised of both a mean and standard deviation, with the standard deviation being a function of the distance to nearby observations at strong motion stations. The methodology is illustrated for two applications. Firstly, maps of conditional peak ground acceleration (PGA) have been developed for the major events in the Canterbury earthquake sequence, which among other things, have been utilized for assessing liquefaction triggering susceptibility of land in residential areas. Secondly, the conditional distribution of response spectral ordinates is obtained at the location of the Canterbury Television building (CTV), which catastrophically collapsed in the 22 February 2011 earthquake. The conditional response spectra provide insight for the selection of ground motion records for use in forensic seismic response analyses of important structures at locations where direct recordings are absent.

Images, eqnz.chch.2010

Rolleston/Burnham, South Island, NZ It's been a busy few weeks! Was away on geology fieldtrips all the previous two weeks, then on Saturday morning 4th September 2010 at 4.35 am we got woken in Westport to a reasonable but very long earthquake. My husband was back in Christchurch at the time and texted me saying "are you ok?". I replied, "yes!"...

Images, UC QuakeStudies

A photograph of a Victim Support poster on a traffic light on Oxford Street. The poster reads, "Looking after yourself in times of crisis. Firstly you have the strength within you to get through this. You are not alone: keep talking to the people around you, use your family, whanau, friends and colleagues and do what you can to help others. Don't ingnore your own emotions and don't be afraid to ask for help when you need it. Keep positive: it is important to keep a positive attitude to events keeping a focus on your strengths and positive coping skills. Do things that will help give you a sense of control. Remaining positive can help reduce stress and anxiety in other people around you, especially children. Reduce stress: you need to keep to routines as much as possible including eating, sleeping, exercise and incorporating those things you enjoy doing as part of your usual daytime activities. Do things that you find comforting as be with people who company you enjoy. It is especially important for children to be participating in normal routine activities as quickly as possible to reduce long term stress factors. You may experience a range of feelings as you move through the crisis and afterwards. Stress, worry, anxiety, fear, uncertainty, anger etc. all are natural responses. Feeling tense and constantly going over events in your mind are also natural responses. It is normal and okay to feel whatever you are feeling. The intensity of uncomfortable thoughts and feelings will lessen as life returns to normal".

Research papers, University of Canterbury Library

A team of earthquake geologists, seismologists and engineering seismologists from GNS Science, NIWA, University of Canterbury, and Victoria University of Wellington have collectively produced an update of the 2002 national probabilistic seismic hazard (PSH) model for New Zealand. The new model incorporates over 200 new onshore and offshore fault sources, and utilises newly developed New Zealand-based scaling relationships and methods for the parameterisation of the fault and subduction interface sources. The background seismicity model has also been updated to include new seismicity data, a new seismicity regionalisation, and improved methodology for calculation of the seismicity parameters. Background seismicity models allow for the occurrence of earthquakes away from the known fault sources, and are typically modelled as a grid of earthquake sources with rate parameters assigned from the historical seismicity catalogue. The Greendale Fault, which ruptured during the M7.1, 4 September 2010 Darfield earthquake, was unknown prior to the earthquake. However, the earthquake was to some extent accounted for in the PSH model. The maximum magnitude assumed in the background seismicity model for the area of the earthquake is 7.2 (larger than the Darfield event), but the location and geometry of the fault are not represented. Deaggregations of the PSH model for Christchurch at return periods of 500 years and above show that M7-7.5 fault and background source-derived earthquakes at distances less than 40 km are important contributors to the hazard. Therefore, earthquakes similar to the Darfield event feature prominently in the PSH model, even though the Greendale Fault was not an explicit model input.

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.

Images, Alexander Turnbull Library

Refers to the government's earthquake response legislation and the Rugby World Cup 2011 (Empowering) Bill. 26 experts in constitutional law from all six of the country's law faculties have penned a letter condemning the Government's earthquake response legislation. No sooner was their work in the public eye than the similarly flawed Rugby World Cup 2011 (Empowering) Bill was reported back from a select committee, with a recommendation that it pass. It also goes far beyond what is required to get things done. In bypassing the normal consent process, the bill says the authority does not have to hold hearings on applications and that its decisions can be challenged in the High Court only on points of law. Effectively, the legislation asks New Zealanders to accept that the Rugby World Cup Minister knows best. It is he who knows how the event must be run. Precisely the same attitude pervades the Canterbury Earthquake Response and Recovery Act. This hands individual Government ministers the power to change almost every law, thereby handing Parliament's normal law-making role to the Executive. Their decisions cannot be challenged in any court'. (NZ Herald editorial - 1 October 2010) Quantity: 1 digital cartoon(s).

Images, Alexander Turnbull Library

Prime Minister John Key stands grinning on a cracked pedestal bearing the words 'Most popular P.M.' In the background is the Beehive flying a skull and crossbones flag. The landscape is a desert with cactus and dried bones and a vulture in a bare tree. A man and a woman comment that it looks as though the quake may have done damage in Wellington after all, that and the crash of the SCF fund. Refers to two major events in the Canterbury area in recent times that have incurred huge government costs; these are the collapse of the South Canterbury Finance Company and the earthquake that struck early Saturday morning 4th September. The South Canterbury Finance Company has been taken into receivership by the government which has guaranteed that all 30,000 fortunate high-risk investors will be paid out $1.6b thanks to the taxpayer. Treasury is assuming that the cost of the earthquake will reach $4 billion, including $2 billion worth of estimated damage to private dwellings and their contents, $1 billion of damage to commercial property, and $1 billion worth of damage to public infrastructure. There is a colour and a black and white version of this cartoon Quantity: 2 digital cartoon(s).