Site of a residents' group formed to advocate and protect the rights of red-zoned home owners in the aftermath of the Canterbury earthquakes.
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Media law developments have continued across many areas in the period to mid-2013. In defamation, the New Zealand courts have begun to consider the issue of third party liability for publication on the internet, with cases involving Google searches and comments on a Facebook page. A parliamentary inquiry into a case that restricted parliamentary privilege has recommended a Parliamentary Privilege Act containing a definition of ‘proceedings in Parliament’. A satirical website increased its popularity when it fought off threatened defamation proceedings. In breach of confidence, a government body, the Earthquake Commission, obtained an interim injunction prohibiting publication of information accidentally released that dealt with the repair of earthquake-damaged properties in Christchurch, and a blogger made the information available online in breach of the order.
Knox Church rebuild on a walk around my neighbourhood September 9, 2014 Christchurch New Zealand.
Documents obtained by Radio New Zealand show WorkSafe New Zealand was still grappling to get on top of asbestos dangers in the Christchurch rebuild nearly two years after the February 2011 earthquake.
The idea of a ‘souvenir’, as a physical keepsake of a place or event, is not a new concept. It’s been around for as long as people have been bringing home exotic treasures from far-off lands, or trying to preserve … Continue reading →
This presentation discusses recent empirical ground motion modelling efforts in New Zealand. Firstly, the active shallow crustal and subduction interface and slab ground motion prediction equations (GMPEs) which are employed in the 2010 update of the national seismic hazard model (NSHM) are discussed. Other NZ-specific GMPEs developed, but not incorporated in the 2010 update are then discussed, in particular, the active shallow crustal model of Bradley (2010). A brief comparison of the NZ-specific GMPEs with the near-source ground motions recorded in the Canterbury earthquakes is then presented, given that these recordings collectively provide a significant increase in observed strong motions in the NZ catalogue. The ground motion prediction expert elicitation process that was undertaken following the Canterbury earthquakes for active shallow crustal earthquakes is then discussed. Finally, ongoing GMPE-related activities are discussed including: ground motion and metadata database refinement, improved site characterization of strong motion station, and predictions for subduction zone earthquakes.
A few weeks ago, there was an interesting interview on Radio New Zealand with historian Jock Phillips, on the history of tobacco use in New Zealand. In the interview, Jock talked about the ways in which people consumed tobacco in … Continue reading →
Working in archaeology here in New Zealand we most often encounter the material remains of Māori settlement and colonisation by the British Empire in the 19th century. Groups such as the New Zealand Company and the Canterbury Association laid out … Continue reading →
And when the devastating 6.3 magnitude quake hit Christchurch, people turned to Radio New Zealand for news.
Demolition underway on the old Government Life building on a walk around the city September 7, 2014 Christchurch New Zealand.
This paper develops representative ground motion ensembles for several major earthquake scenarios in New Zealand. Cases considered include representative ground motions for the occurrence of Alpine, Hope, and Porters Pass earthquakes in Christchurch, and the occurrence of Wellington, Wairarapa, and Ohariu, fault ruptures in Wellington. Challenges in the development of ground motion ensembles for subduction zone earthquakes are also highlighted. The ground motions are selected based on the generalized conditional intensity measure (GCIM) approach, ensuring that the ground motion ensembles represent both the mean, and distribution of ground motion intensity which such scenarios could impose. These scenario-based ground motion sets can be used to complement ground motions which are often selected in conjunction with probabilistic seismic hazard analysis, in order to understand the performance of structures for the question “what if this fault ruptures?”
This poster provides a summary of the development of a 3D shallow (z<40m) shear wave velocity (Vs) model for the urban Christchurch, New Zealand region. The model is based on a recently developed Christchurch-specific empirical correlation between Vs and cone penetration test (CPT) data (McGann et al. 2014a,b) and the large high-density database of CPT logs in the greater Christchurch urban area (> 15,000 logs as of 01/01/2014). In particular, the 3D model provides shear wave velocities for the surficial Springston Formation, Christchurch Formation, and Riccarton gravel layers which generally comprise the upper 40m in the Christchurch urban area. Point-estimates are provided on a 200m-by- 200m grid from which interpolation to other locations can be performed. This model has applications for future site characterization and numerical modeling efforts via maps of timeaveraged Vs over specific depths (e.g. Vs30, Vs10) and via the identification of typical Vs profiles for different regions and soil behaviour types within Christchurch. In addition, the Vs model can be used to constrain the near-surface velocities for the 3D seismic velocity model of the Canterbury basin (Lee et al. 2014) currently being developed for the purpose of broadband ground motion simulation.
Following the 2010-2011 earthquakes in Canterbury, New Zealand, the University of Canterbury (UC) was faced with the need to respond to major challenges in its teaching and learning environment. With the recognition of education as a key component to the recovery of the Canterbury region, UC developed a plan for the transformation and renewal of the campus. Central to this renewal is human capital – graduates who are distinctly resilient and broadly skilled, owing in part to their living and rebuilding through a disaster. Six desired graduate attributes have been articulated through this process: knowledge and skills of a recognized subject, critical thinking skills, the ability to interpret information from a range of sources, the ability to self-direct learning, cultural competence, and the recognition of global connections through social, ethical, and environmental values. All of these attributes may readily be identified in undergraduate geoscience field education and graduate field-based studies, and this is particularly important to highlight in a climate where the logistical and financial requirements of fieldwork are becoming a barrier to its inclusion in undergraduate curricula. Fieldwork develops discipline-specific knowledge and skills and fosters independent and critical thought. It encourages students to recognize and elaborate upon relevant information, plan ways to solve complicated problems, execute and re-evaluate these plans. These decisions are largely made by the learners, who often direct their own field experience. The latter two key graduate attributes, cultural competence and global recognition of socio-environmental values, have been explicitly addressed in field education elsewhere and there is potential to do so within the New Zealand context. These concepts are inherent to the sense of place of geoscience undergraduates and are particularly important when the field experience is viewed through the lens of landscape heritage. This work highlights the need to understand how geoscience students interact with field places, with unique implications for their cultural and socio-environmental awareness as global citizens, as well as the influence that field pedagogy has on these factors.
Residents of some Christchurch suburbs could be in for bigger than expected rates rises after the first QV valuations since the earthquakes. The average Christchurch home now has a rating value of 455 thousand dollars, which translates into an annual rates bill of just over two thousand dollars.
Page 5 of Section B of the Christchurch Press, published on Wednesday 8 January 2014.
Page 18 of Section C of the Christchurch Press, published on Saturday 22 February 2014.
Page 3 of Section D of the Christchurch Press, published on Wednesday 10 December 2014.
Page 1 of the Best Bets section of the Christchurch Press, published on Friday 12 December 2014.
Page 9 of Section A of the Christchurch Press, published on Friday 7 February 2014.
Page 24 of Section A of the Christchurch Press, published on Saturday 22 February 2014.
Page 1 of the Zest section of the Christchurch Press, published on Wednesday 26 February 2014.
Page 10 of The Box section of the Christchurch Press, published on Tuesday 11 March 2014.
Page 4 of Section B of the Christchurch Press, published on Friday 14 March 2014.
Page 2 of Section B of the Christchurch Press, published on Monday 17 March 2014.
Page 16 of Section C of the Christchurch Press, published on Saturday 5 April 2014.
Page 2 of Section B of the Christchurch Press, published on Saturday 6 December 2014.
Page 2 of Section D of the Christchurch Press, published on Saturday 13 December 2014.
Page 6 of Section B of the Christchurch Press, published on Saturday 20 December 2014.
Page 18 of Section A of the Christchurch Press, published on Saturday 12 July 2014.