Damage to TJ's Kazbah in New Brighton. The east and north walls and part of the upper floor have collapsed, tipping rubble and the contents of the rooms out onto the street. The photographer comments, "The occupants of the business and rooms all managed to escape alive. A digger was used to make the building safe and then used to sift through the rubble for any surviving belongings. It was a very emotional time for the ex-occupants".
Christchurch’s new $92m central city library opened today – replacing the former library which was damaged in the Canterbury earthquakes. But as Logan Church discovers, with sewing suites, a TV wall and a music studio, this library is home to more than rows and rows of books.
More than 600 Christchurch home-owners face a wait of up to 18 months before its decided who foots the bill for earthquake repairs that could cost hundreds of millions of dollars. The problem - first revealed on Checkpoint in March - is that owners bought homes thinking all quake damage had been identified and fixed - only to find more problems that weren't addressed. The people affected cannot claim on their insurance - because the damage pre-dates them buying the house - and any grant from the Earthquake Commission is capped. EQC has publicly apologised to those affected but the Minster, Megan Woods, says it's unclear who will pay for the needed repairs.
Canterbury mayors say their ratepayers are already paying for earthquake recovery, roading, water and storm water infrastructure, so a shiny new Christchurch stadium is way down the priority list.
The former Christchurch East Labour Party MP, Lianne Dalziel, is now the Mayor of Christchurch and, as such, is set to work much more closely with her former political foe, Earthquake Minister Gerry Brownlee.
An entry from Roz Johnson's blog for 22 May 2012 entitled, "Giving New Life".
The popular bar, restaurant and music venue was a fixture of the city's Arts Centre for decades before the 2011 earthquake.
Residents of Christchurch's coastal suburbs around New Brighton are being promised they won't have to wait another decade for an urgently needed new bridge. The existing one is a critical emergency escape route but is almost 100 years old and suffered significant damage in the 2011 earthquake. And as Timothy Brown reports, plans for an upgrade are grinding slowly ahead.
Nature has endowed New Zealand with unique geologic, climatic, and biotic conditions. Her volcanic cones and majestic Southern Alps and her verdant plains and rolling hills provide a landscape as rugged and beautiful as will be found anywhere. Her indigenous fauna and flora are often quite different from that of the rest of the world and consequently have been of widespread interest to biologists everywhere. Her geologic youth and structure and her island climate, in combination with the biological resources, have made a land which is ecologically on edge. These natural endowments along with the manner in which she has utilized her land, have given New Zealand some of the most spectacular and rapid erosion to be found. It is quite evident that geologic and climatic conditions combine to give unusually high rates of natural erosion. Present topographic features indicate the past occurrence of large-scale flooding as well. Prior to the arrival of the Maori, it is very likely that most of the land mass of New Zealand below present bush lines was covered with indigenous bush or forest. Forest fires of a catastrophic nature undoubtedly occurred as a result of lightning, and volcanic eruptions. The exposed soils left by these catastrophes contributed to natural deterioration. While vast areas of forest cover were destroyed, they probably were healed by nature with forest or with grass or herbaceous cover. Further, it is probable that large areas in the mountains were, as they are now, subject to landslides and slipping due to earthquakes and excessive local rainfall. Again, the healing process was probably rapid in most of such exposed areas.
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 occurred to unreinforced masonry buildings throughout the region during the mainshock and subsequent large aftershocks. Particularly 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. 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, a geotechnical reconnaissance was conducted over a period of six days (10–15 September 2010) by a team of geotechnical/earthquake engineers and geologists from New Zealand and USA (GEER team: Geo-engineering Extreme Event Reconnaissance). JGS (Japanese Geotechnical Society) members from Japan also participated in the reconnaissance team from 13 to 15 September 2010. The NZ, GEER and JGS members worked as one team and shared resources, information and logistics in order to conduct thorough and most efficient reconnaissance covering a large area over a very limited time period. This report summarises the key evidence and findings from the reconnaissance.
Base isolation is an incredibly effective technology used in seismic regions throughout the world to limit structural damage and maintain building function, even after severe earthquakes. However, it has so far been underutilised in light-frame wood construction due to perceived cost issues and technical problems, such as a susceptibility to movement under strong wind loads. Light-frame wood buildings make up the majority of residential construction in New Zealand and sustained significant damage during the 2010-2011 Canterbury earthquake sequence, yet the design philosophy has remained largely unchanged for years due to proven life-safety performance. Recently however, with the advent of performance based earthquake engineering, there has been a renewed focus on performance factors such as monetary loss that has driven a want for higher performing residential buildings. This research develops a low-cost approach for the base isolation of light-frame wood buildings using a flat-sliding friction base isolation system, which addresses the perceived cost and technical issues, and verifies the seismic performance through physical testing on the shake table at the University of Canterbury. Results demonstrate excellent seismic performance with no structural damage reported despite a large number of high-intensity earthquake simulations. Numerical models are subsequently developed and calibrated to New Zealand light-frame wood building construction approaches using state-of-the-art wood modelling software, Timber3D. The model is used to accurately predict both superstructure drift and acceleration demand parameters of fixed-base testing undertaken after the base isolation testing programme is completed. The model development allows detailed cost analyses to be undertaken within the performance based earthquake engineering framework that highlights the monetary benefits of using base isolation. Cost assessments indicate the base isolation system is only 6.4% more compared to the traditional fixed-base system. Finally, a design procedure is recommended for base isolated light-frame wood buildings that is founded on the displacement based design (DBD) approach used in the United States and New Zealand. Nonlinear analyses are used to verify the DBD method which indicate its suitability.
Still awaiting a repair, but with so many bridges closed or partially closed we are lucky this one had what maybe minor damage.
Prior to the earthquakes the stone wall at right was near road level. Now it is about 1.5m (4-5ft) lower.
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Eighty years and then the damage was done. Result of the earthquake on 22/02/11.
A new survey shows New Zealand insurers are worried the industry's reputation could be ruined if it does not deal well with the huge number of claims from the Christchurch earthquakes.
Under the caption, young people carrying their baggage flutter into the air, away from Canterbury and toward 'Oz'. In September GNS Earth Sciences reported that after the earthquakes, the Greendale and associated faults were still moving as they settled into a new configuration. At the same time the young were leaving Canterbury (and New Zealand) for a better future in Australia. The population of New Zealand was moving into a new configuration. Quantity: 1 digital cartoon(s).
Photograph captioned by Fairfax, "A unit of about 15 New Zealand Territorial Army soldiers prepare to sandbag a broken pumping station in New Brighton to stop water pouring into neighbouring properties. The pumping station on the corner of Palmers Road and New Brighton Road was badly damaged and water was pouring onto both streets".
Photograph captioned by Fairfax, "A unit of about 15 New Zealand Territorial Army soldiers prepare to sandbag a broken pumping station in New Brighton to stop water pouring into neighbouring properties. The pumping station on the corner of Palmers Road and New Brighton Road was badly damaged and water was pouring onto both streets".
The public at the inaugural New Zealand Sandcastle competition held at New Brighton beach. The organisers of the Christchurch sandcastle competition hope the event will bring cheer to the earthquake-hit city.
The public at the inaugural New Zealand Sandcastle competition held at New Brighton beach. The organisers of the Christchurch sandcastle competition hope the event will bring cheer to the earthquake-hit city.
The public at the inaugural New Zealand Sandcastle competition held at New Brighton beach. The organisers of the Christchurch sandcastle competition hope the event will bring cheer to the earthquake-hit city.
A map showing the earthquake epicentre and new faultline trace.
A map showing the earthquake epicentre and new faultline trace.
Graphs comparing residential property prices across Christchurch and New Zealand.
Graphs comparing residential property prices across Christchurch and New Zealand.
Graphs comparing residential property prices across Christchurch and New Zealand.
Graphs comparing residential property prices across Christchurch and New Zealand.
A graphic giving the status of North New Brighton School.
Graphs comparing residential property prices across Christchurch and New Zealand.