Search

found 97150 results

Images for New Zealand; more images...

Images, UC QuakeStudies

Detail of damage to the former Princess Cinema in New Brighton. Bricks have fallen from the wall, exposing the interior. The photographer comments, "This is the side view of the back of the old Princess Cinema in New Brighton after the earthquake in Christchurch, New Zealand on 22 February. The bricks seem to be just about to fall, but stayed in place after several big aftershocks. This building has now been knocked down as it was so dangerous".

Research papers, University of Canterbury Library

A zone of active tectonism occurs in mid and north Canterbury, from the Rakaia to the Waipara Rivers, which coincides with seismicity concentrations and several Quaternary surface anomalies and is here defined as the Porters Pass Tectonic Zone. Although parallel to the Marlborough faults to the north, the lack of regional definition suggests this zone is much younger in its inception reflecting a southward movement of the plate rotation vector. The objectives of this study were to map the structures associated with this zone in the segment between the Rakaia and Waimakariri Rivers with detailed analysis concentrated in the upper Kawai Valley. Quaternary offsets on the main lineament of the Porters Pass Fault were traced through the area and evidence for the rate of movement, probable magnitudes and return periods of related seismic events was sought. The basement was found to be complicated by pre-existing deformation structures in Torlesse Group rocks which have been subsequently been re-activated or rotated by recent fault movement probably beginning in the Pleistocene. This phase is dominantly thrusting and uplift has lead to the erosion of most of the overlying sedimentary cover. Remnants of the Cret-Tertiary sediments still remain as fault-bounded packets. Evidence suggests that a change to development of a regional lateral shear associated with the Porters Pass Tectonic Zone transects the thrust system with complex interaction between the older reverse and new strike-slip faults. Offset rates along the segments of the Porters Pass Fault are not well constrained but are believed to be approximately in the range of 11-13 mm/year for at least the last 130,000 years. This rate is similar to other large faults in the Marlborough region. Two earthquake events have been identified and dated at 600 and 2000 years ago, with a magnitude of greater than 6.5. Evidence suggests characteristic earthquakes along the Porters Pass Fault are greater than Magnitude 7. This result has some major ramifications for the expected seismic hazards for nearby Christchurch.

Images, UC QuakeStudies

A photograph of equipment from the New Zealand Fire Service Urban Search and Rescue team on display in the Canterbury Quakes exhibition at the Canterbury Museum. The equipment was used during the emergency response to the 22 February 2011 earthquake.

Audio, Radio New Zealand

Fiona Farrell has been awarded the $100,000 Creative New Zealand Michael King Writer's Fellowship to research and write twin books, one fiction and one non-fiction, inspired by her experiences of the Canterbury earthquakes and the rebuilding of the city.

Images, Alexander Turnbull Library

The text 'Rugby World Cup' runs across the top of the cartoon. Below is a poster depicting the shape of a rugby ball with a double koru design and the year '2011'. It is accompanied by the words 'Rugby New Zealand (well not quite all New Zealand)' Someone off screen kicks a rugby ball that represents 'Christrch' across the frame. Context - Christchurch has been told that they will not be able to host any Rugby World Cup games because of the damage to the city after the earthquakes 4 September 2010 and 22 February 2011. Quantity: 1 digital cartoon(s).

Images, eqnz.chch.2010

Here's Prarie, outside our flat, the day after the 7.1 earthquake hit Christchurch. You see the damage to the street, which continued through our flat. We were forced to move out once an engineer examined the cracks in our balcony, walls, floors, and ceilings, and told us the building was unsafe for living. One crack ran from the street, pres...

Research papers, University of Canterbury Library

New Zealand has a long tradition of using light timber frame for construction of its domestic dwellings. After the most recent earthquakes (e.g. Canterbury earthquakes sequence), wooden residential houses showed satisfactory life safety performance which aligns with New Zealand design codes requirements. However, poor performance was reported in terms of their seismic resilience that can be generally associated with community demands. Future expectations of the seismic performance of wooden-framed houses by homeowners were assessed in this research. Homeowners in the Wellington region were asked in a survey about the levels of safety and expected possible damage in their houses after a seismic event. Findings bring questions about whether New Zealand code requirements are good enough to satisfy community demands. Also, questions whether available information of strengthening techniques to structurally prepare wooden-framed houses to face future major earthquakes can help to make homeowners feel safer at home during major seismic events.

Audio, Radio New Zealand

The government's looking overseas to get more hands on deck to help with the rebuild from Cyclone Gabrielle. A new short-term Recovery Visa will bring in specialist foreign workers through a similar pathway used after the Christchurch and Kaikoura earthquakes. The visas will be fast-tracked with officials aiming to get applications through within seven days. Corn Dann spoke with immigration minister Michael Wood.

Articles, Christchurch uncovered

It’s been a busy month for Underground Overground Archaeology as we’ve been actively involved in New Zealand Archaeology Week 2018 running displays, historical tours, and talks – all of them highly successful thanks to history and archaeology lovers across the … Continue reading →

Articles, Christchurch uncovered

It’s very easy to think of 19th century New Zealand as being a place isolated from the rest of the world. Yet as we research and investigate colonial Christchurch, we are constantly being reminded of the connections that existed between … Continue reading →

Images, UC QuakeStudies

A digger being loaded onto the back of a truck. The photographer comments, "After clearing away the remains of a building in Christchurch, New Zealand destroyed by the February 22 earthquake the digger can now be transported to its next destination for destruction".

Images, UC QuakeStudies

Road damage and liquefaction in a residential street. The photographer comments, "A great gouge in the road caused by liquefaction undermining the road surface and a car driving over it. This was the earthquake in Christchurch, New Zealand on 22 February 2011".

Articles, Christchurch uncovered

“It must have been a happy household,” was the remark made by one of our team members when she saw the artefact assemblage we are discussing on today’s blog post. Whilst children’s artefacts are relatively common finds on New Zealand … Continue reading →

Articles, Christchurch uncovered

Some of the most common archaeological finds related to the European settlement of New Zealand during 19th century are usually from residential occupation. Features like rubbish pits, underfloor deposits, wells (brick and artesian), cesspits, soak pits, post holes and drainage … Continue reading →

Audio, Radio New Zealand

Maurice and I tells the surprisingly moving story of two of the most successful architects in New Zealand - Sir Miles Warren and Maurice Mahoney - their life, their times, and their struggle to save their most famous building after the 2011 Christchurch earthquake.

Research papers, University of Canterbury Library

Small, tight-knit communities, are complex to manage from outside during a disaster. The township of Lyttelton, New Zealand, and the communities of Corsair Bay, Cass Bay, and Rapaki to the east, are especially more so difficult due to the terrain that encloses them, which caused them to be cut-off from Christchurch, the largest city in the South Island, barely 10 km away, after the Mw 7.1 Darfield Earthquake and subsequent Canterbury Earthquake Sequence. Lyttelton has a very strong and deep-rooted community spirit that draws people to want to be a part of Lyttelton life. It is predominantly residential on the slopes, with retail space, service and light industry nestled near the harbour. It has heritage buildings stretching back to the very foundation of Canterbury yet hosts the largest, modern deep-water port for the region. This study contains two surveys: one circulated shortly before the Darfield Earthquake and one circulated in July 2011, after the Christchurch and Sumner Earthquakes. An analytical comparison of the participants’ household preparedness for disaster before the Darfield Earthquake and after the Christchurch and Sumner Earthquakes was performed. A population spatiotemporal distribution map was produced that shows the population in three-hourly increments over a week to inform exposure to vulnerability to natural hazards. The study went on to analyse the responses of the participants in the immediate period following the Chrsitchurch and Sumner Earthquakes, including their homeward and subsequent journeys, and the decision to evacuate or stay in their homes. Possible predictors to a decision to evacuate some or all members of the household were tested. The study also asked participants’ views on the events since September 2010 for analysis.