A hazard board for a house being demolished in Richmond. Hazards listed are dust, noise, excavator, trucks, visitors and danger from equipment working. The photographer comments, "The end of 393 River Rd".
A photograph captioned by BeckerFraserPhotos, "A hazard sign on Gloucester Street".
A photograph of a hazard board on a cordon fence on Cambridge Terrace.
An entry from Jennifer Middendorf's blog for 25 April 2011 entitled, "I'm back (sort of)".
Information board and hazard notices for the Riccarton House earthquake repairs and strengthening project.
Photograph captioned by BeckerFraserPhotos, "The All Saints Church in Sumner. The traditional building materials and style of this church makes it look older than 1963. At the moment it is hidden behind a long line of containers protecting the road from potential rock fall hazards".
Hazard boards for a house being demolished in Richmond. The photographer comments, "Safety warning signs".
Photograph captioned by BeckerFraserPhotos, "Wakefield Avenue in Sumner".
A photograph captioned by Paul Corliss, "Redzoned houses between Wattle Drive and Anzac Drive".
Photograph captioned by BeckerFraserPhotos, "The cliffs above Wakefield Avenue in Sumner".
An entry from Deb Robertson's blog for 24 September 2015 entitled, "Journalists at Work {Part 3(3) COMS 304}".The entry was downloaded on 3 November 2016.
Photograph captioned by BeckerFraserPhotos, "Temporary fence to close the track due to rockfall hazard, Taylors Mistake".
Photograph captioned by BeckerFraserPhotos, "Heberden Avenue, Sumner".
A photograph of a Fulton Hogan hazard sign on a cordon fence. The photograph is captioned by Paul Corliss, "Central city".
The latest two great earthquake sequences; 2010- 2011 Canterbury Earthquake and 2016 Kaikoura Earthquake, necessitate a better understanding of the New Zealand seismic hazard condition for new building design and detailed assessment of existing buildings. It is important to note, however, that the New Zealand seismic hazard map in NZS 1170.5.2004 is generalised in effort to cover all of New Zealand and limited to a earthquake database prior to 2001. This is “common” that site-specific studies typically provide spectral accelerations different to those shown on the national map (Z values in NZS 1170.5:2004); and sometimes even lower. Moreover, Section 5.2 of Module 1 of the Earthquake Geotechnical Engineering Practice series provide the guidelines to perform site- specific studies.
A photograph of a hazard board outside a damaged house. The photograph is captioned by Paul Corliss, "Fitzgerald Avenue, alongside Avon Loop".
A photograph of a hazard board outside a house being demolished. The photograph is captioned by Paul Corliss, "47 Major Hornbrook Road, Mount Pleasant".
A photograph of a hazard board outside a house being demolished. The photograph is captioned by Paul Corliss, "47 Major Hornbrook Road, Mount Pleasant".
This thesis presents an assessment of historic seismic performance of the New Zealand stopbank network from the 1968 Inangahua earthquake through to the 2016 Kaikōura earthquake. An overview of the types of stopbanks and the main aspects of the design and construction of earthen stopbanks was presented. Stopbanks are structures that are widely used on the banks of rivers and other water bodies to protect against the impact of flood events. Earthen stopbanks are found to be the most used for such protection measures. Different stopbank damage or failure modes that may occur due to flooding or earthquake excitation were assessed with a focus on past earthquakes internationally, and examples of these damage and failure modes were presented. Stopbank damage and assessment reports were collated from available reconnaissance literature to develop the first geospatial database of stopbank damage observed in past earthquakes in New Zealand. Damage was observed in four earthquakes over the past 50 years, with a number of earthquakes resulting in no stopbank damage. The damage database therefore focussed on the Edgecumbe, Darfield, Christchurch and Kaikōura earthquakes. Cracking of the crest and liquefaction-induced settlement were the most common forms of damage observed. To understand the seismic demand on the stopbank network in past earthquakes, geospatial analyses were undertaken to approximate the peak ground acceleration (PGA) across the stopbank network for ten large earthquakes that have occurred in New Zealand over the past 50 years. The relationship between the demand, represented by the peak ground acceleration (PGA) and damage is discussed and key trends identified. Comparison of the seismic demand and the distribution of damage suggested that the seismic performance of the New Zealand stopbank network has been generally good across all events considered. Although a significant length of the stopbank networks were exposed to high levels of shaking in past events, the overall damage length was a small percentage of this. The key aspect controlling performance was the performance of the underlying foundation soils and the effect of this on the stopbank structure and stability.
Photograph captioned by BeckerFraserPhotos, "792 Colombo Street".
A photograph captioned by Paul Corliss, "Mobil station reconstruction, corner Bealey Avenue and Barbadoes Street".
A photograph captioned by Paul Corliss, "Mobil station reconstruction, corner Bealey Avenue and Barbadoes Street".
A message spray painted on the footpath outside the National Radiation Laboratory on Victoria Street. The message reads, NZRT2, not checked, hazards, 23rd".
A message spray painted on the footpath outside the National Radiation Laboratory on Victoria Street. The message reads, NZRT2, not checked, hazards, 23rd".
The term resilience‘’is increasingly being used in a multitude of contexts. Seemingly the latest buzz‘’word, it can mean many things to many people, in many different situations. In a natural hazard context, the terms sustainable planning‘’, and resilience‘planning are now’being used, often interchangeably. This poster provides an overview of resilience and sustainability within a land use planning and natural hazard context, and discusses how they are interrelated in the situation of the earthquake impacted city of Christchurch, New Zealand.
Photograph captioned by BeckerFraserPhotos, "Houses on Richmond Hill Road in Sumner, now close to the edge of the cliff".
Numerous rockfalls released during the 2010–2011 Canterbury earthquake sequence affected vital road sections for local commuters. We quantified rockfall fatality risk on two main routes by adapting a risk approach for roads originally developed for snow avalanche risk. We present results of the collective and individual fatality risks for traffic flow and waiting traffic. Waiting traffic scenarios particularly address the critical spatial-temporal dynamics of risk, which should be acknowledged in operational risk management. Comparing our results with other risks commonly experienced in New Zealand indicates that local rockfall risk is close to tolerability thresholds and likely exceeds acceptable risk.
A story submitted by Brenda Greene to the QuakeStories website.
A story submitted by Rochelle to the QuakeStories website.
A photograph of a felled tree, liquefaction, and flooding in a residential street in Christchurch. Road cones have been placed around hazards to warn road and footpath users.