A video of Lianne Dalziel talking about her vision for the Christchurch residential red zone. Dalziel talks about turning the Travis Wetlands and some of the residential red zone into the largest natural wetlands within a city boundary.
A photograph looking north along the footpath of Bangor Street. To the right there are the former sites of several houses. The houses were demolished after the land was zoned Red.
A photograph of the former site of Donna Allfrey's house at 406 Oxford Terrace. Allfrey's house was demolished after her land was zoned Red.
A photograph of the former sites of several houses on Bangor Street. The houses were demolished after the land was zoned Red.
A photograph of the former site of Doug Sexton's house at 378 Oxford Terrace. Sexton's house was demolished after his land was zoned Red.
A photograph of the former site of Doug Sexton's house at 378 Oxford Terrace. Sexton's house was demolished after his land was zoned Red.
A photograph of the former site of Donna Allfrey's house at 406 Oxford Terrace. Allfrey's house was demolished after her land was zoned Red.
A photograph of the former site of Siobhan Murphy's house at 436 Oxford Terrace. Murphy's house was demolished after her land was zoned Red. Grass has grown over the site.
A photograph of the former site of Siobhan Murphy's house at 436 Oxford Terrace. Murphy's house was demolished after her land was zoned Red. Grass has grown over the site.
A photograph of the former site of Siobhan Murphy's house at 436 Oxford Terrace. Murphy's house was demolished after her land was zoned Red. Grass has grown over the site.
A photograph of the former site of Siobhan Murphy's house at 436 Oxford Terrace. Murphy's house was demolished after her land was zoned Red. Grass has grown over the site.
A photograph of the former site of Siobhan Murphy's house at 436 Oxford Terrace. Murphy's house was demolished after her land was zoned Red. Grass has grown over the site.
A photograph of the former site of Doug Sexton's house at 378 Oxford Terrace. Sexton's house was demolished after his land was zoned Red. Grass has begun to grow in the site.
A photograph of the former site of Robin Duff's house at 386 Oxford Terrace. Duff's house was demolished after his land was zoned Red. Grass has begun to grow on the site.
A photograph of the former site of Doug Sexton's house at 378 Oxford Terrace. Sexton's house was demolished after his land was zoned Red. Grass has begun to grow in the site.
A photograph of the former site of Robin Duff's house at 386 Oxford Terrace. Duff's house was demolished after his land was zoned Red. Grass has begun to grow on the site.
A photograph of the former site of the Locke family's house at 392 Oxford Terrace. The Locke's house was deconstructed after their land was zoned Red. Wire fencing has been placed around the outside of the neighbouring property. The photographer comments, "The house was deconstructed and rebuilt on another site".
A photograph of the former site of the Locke family's house at 392 Oxford Terrace. The Locke's house was deconstructed after their land was zoned Red. Wire fencing has been placed around the outside of the neighbouring property. The photographer comments, "The house was deconstructed and rebuilt on another site".
A photograph of the former site of a house at 57 Bangor Street. The house was demolished after the land was zoned Red. The houses in the background have also been demolished, so that Oxford Terrace is visible in the distance.
A photograph looking east along Oxford Terrace from outside the former site of Donna Allfrey's house. Allfrey's house was demolished after her land was zoned Red. The sites of many other demolished houses can be seen to the left.
A photograph of the former site of Donna Allfrey's house on Oxford Terrace. Allfrey's house was demolished after her land was zoned Red. The photographer comments, "Large section of the front fence has been stolen by looters".
A photograph of the former site of a house at 58 Bangor Street. The house was demolished after the land was zoned Red. The grass has begun to grow over the site. The house behind has also been demolished, so that Oxford Terrace is now visible in the distance.
A photograph of a wire fence at the border of 406 Oxford Terrace. 406 Oxford Terrace is the former site of Donna Allfrey's house which was demolished after her land was zoned Red. In front of the fence, gravel has been spread over the ground.
A photograph of a wire fence that has been placed at the border of 406 Oxford Terrace. 406 Oxford Terrace is the former site of Donna Allfrey's house which was demolished after her land was zoned Red. Behind the fence, gravel has been spread over the ground.
This report to RCP Ltd and University of Canterbury summarises the findings of a 5 month secondment to the CERA Port Hills Land Clearance Team. Improvement strategies were initiated and observed. The Port Hills Land Clearance Programme is the undertaking of the demolition of all built structures from the Crown’s compulsory acquired 714 residential red zoned properties. These properties are zoned red due to an elevated life risk as a result of geotechnical land uncertainty following the 2011 Canterbury Earthquakes.
The 2010 and 2011 earthquakes in the region of Canterbury, New Zealand caused widespread damage and the deaths of 185 people. Suburbs on the eastern side of Christchurch and in the satellite town of Kaiapoi, 20 kilometres north of Christchurch, were badly damaged by liquefaction. The Canterbury Earthquake Recovery Authority (CERA), a government organisation set up in the wake of the earthquakes, began to systematically zone all residential land in 2011. Based on the possibility for land remediation, 7860 houses in Christchurch and Kaiapoi were zoned red. Those who were in this zone were compensated and had to buy or build elsewhere. The other zone examined within this research – that of TC3 – lies within the green zone. Residents, in this zone, were able to stay in their houses but land was moderately damaged and required site-specific geotechnical investigations. This research sought to understand how residents’ senses of home were impacted by a disaster and the response efforts. Focusing on the TC3 and red zone of the eastern suburbs and the satellite town of Kaiapoi, this study interviewed 29 residents within these zones. The concept of home was explored with the respondents at three scales: home as a household; home as a community; and home as a city. There was a large amount of resistance to the zoning process and the handling of claims by insurance companies and the Earthquake Commission (EQC) after the earthquakes. Lack of transparency and communication, as well as extremely slow timelines were all documented as failings of these agencies. This research seeks to understand how participant’s sense of home changed on an individual level and how it was impacted by outside agencies. Homemaking techniques were also focused on showing that a changed sense of home will impact on how a person interacts with a space.
Millions of urban residents around the world in the coming century will experience severe landscape change – including increased frequencies of flooding due to intensifying storm events and impacts from sea level rise. For cities, collisions of environmental change with mismatched cultural systems present a major threat to infrastructure systems that support urban living. Landscape architects who address these issues express a need to realign infrastructure with underlying natural systems, criticizing the lack of social and environmental considerations in engineering works. Our ability to manage both society and the landscapes we live in to better adapt to unpredictable events and landscape changes is essential if we are to sustain the health and safety of our families, neighbourhoods, and wider community networks. When extreme events like earthquakes or flooding occur in developed areas, the feasibility of returning the land to pre-disturbance use can be questioned. In Christchurch for example, a large expanse of land (630 hectares) within the city was severely damaged by the earthquakes and judged too impractical to repair in the short term. The central government now owns the land and is currently in the process of demolishing the mostly residential houses that formed the predominant land use. Furthermore, cascading impacts from the earthquakes have resulted in a general land subsidence of .5m over much of eastern Christchurch, causing disruptive and damaging flooding. Yet, although disasters can cause severe social and environmental distress, they also hold great potential as a catalyst to increasing adaption. But how might landscape architecture be better positioned to respond to the potential for transformation after disaster? This research asks two core questions: what roles can the discipline of landscape architecture play in improving the resilience of communities so they become more able to adapt to change? And what imaginative concepts could be designed for alternative forms of residential development that better empower residents to understand and adapt the infrastructure that supports them? Through design-directed inquiry, the research found landscape architecture theory to be well positioned to contribute to goals of social-ecological systems resilience. The discipline of landscape architecture could become influential in resilience-oriented multi disciplinary collaborations, with our particular strengths lying in six key areas: the integration of ecological and social processes, improving social capital, engaging with temporality, design-led innovation potential, increasing diversity and our ability to work across multiple scales. Furthermore, several innovative ideas were developed, through a site-based design exploration located within the residential red zone, that attempt to challenge conventional modes of urban living – concepts such as time-based land use, understanding roads as urban waterways, and landscape design and management strategies that increase community participation and awareness of the temporality in landscapes.
Prognostic modelling provides an efficient means to analyse the coastal environment and provide effective knowledge for long term urban planning. This paper outlines how the use of SWAN and Xbeach numerical models within the ESRI ArcGIS interface can simulate geomorphological evolution through hydrodynamic forcing for the Greater Christchurch coastal environment. This research followed the data integration techniques of Silva and Taborda (2012) and utilises their beach morphological modelling tool (BeachMM tool). The statutory requirements outlined in the New Zealand Coastal Policy Statement 2010 were examined to determine whether these requirements are currently being complied with when applying the recent sea level rise predictions by the Intergovernmental Panel on Climate Change (2013), and it would appear that it does not meet those requirements. This is because coastal hazard risk has not been thoroughly quantified by the installation of the Canterbury Earthquake Recovery Authority (CERA) residential red zone. However, the Christchurch City Council’s (CCC) flood management area does provide an extent to which managed coastal retreat is a real option. This research assessed the effectiveness of the prognostic models, forecasted a coastline for 100 years from now, and simulated the physical effects of extreme events such as storm surge given these future predictions. The results of this research suggest that progradation will continue to occur along the Christchurch foreshore due to the net sediment flux retaining an onshore direction and the current hydrodynamic activity not being strong enough to move sediment offshore. However, inundation during periods of storm surge poses a risk to human habitation on low lying areas around the Avon-Heathcote Estuary and the Brooklands lagoon similar to the CCC’s flood management area. There are complex interactions at the Waimakariri River mouth with very high rates of accretion and erosion within a small spatial scale due to the river discharge. There is domination of the marine environment over the river system determined by the lack of generation of a distinct river delta, and river channel has not formed within the intertidal zone clearly. The Avon-Heathcote ebb tidal delta aggrades on the innner fan and erodes on the outer fan due to wave domination. The BeachMM tool facilitates the role of spatial and temporal analysis effectively and the efficiency of that performance is determined by the computational operating system.