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Videos, UC QuakeStudies

A video of interviews with three residents about their Port Hills properties. The video was filmed the day after Earthquake Recovery Minister Gerry Brownlee announced the red-zoning of 285 Port Hills properties. The video includes an interview with Marine Kent (whose house was zoned white to green), Mark Tranter (whose house was zoned white to red), and Tony Ging (whose house is still white-zoned).

Images, Alexander Turnbull Library

A business owner has been allowed into the 'Red Zone' in the Christchurch CBD in order to investigate the damage to his business premises. He is dismayed to discover that he has forgotten his keys; the Civil Defence officer who is with him, looks at him askance as the door is the only part of his premises still standing. Context - Some time after the earthquake of 22 March 2011 business owners were allowed through the cordon to collect belongings and see their premises for themselves. Colour and black and white versions of this cartoon are available Quantity: 2 digital cartoon(s).

Images, Alexander Turnbull Library

A large sign just outside Christchurch's Red Zone reads 'Christchurch RED ZONE - security staff and celebrities only'. A security guard phones through to Check Point One, saying 'Base to check point one - no shop keepers allowed but the queen, Fidel Castro, Tina Turner and Elvis are coming in'. These four people have formed a queue and are allowed to enter the Red Zone. Context - It is now three months past the earthquake of 19 February and shopkeepers and owners of small businesses are becoming very frustrated by the still limited access to the Red Zone business area. Colour and black and white versions available Quantity: 2 digital cartoon(s).

Research papers, University of Canterbury Library

One of the less understood geotechnical responses to the cyclic loading from the MW6.2 Christchurch Earthquake, on the 22nd of February 2011, is the fissuring in the loessial soil-mantled, footslope positions of the north-facing valleys of the Port Hills. The fissures are characterized by mostly horizontal offset (≤500mm), with minor vertical displacement (≤300mm), and they extend along both sides of valleys for several hundred metres in an approximately contour-parallel orientation. The fissure traces correspond to extensional features mapped in other studies. Previous studies have suggested that the fissures are the headscarps of incipient landslides, but the surface and subsurface features are not typical of landslide movement. Whilst there are some features that correlate with landslide movement, there are many features that contradict the landslide movement hypothesis. Of critical importance to this investigation was the fact that there are no landslide flanks, there has been no basal shear surface found, there is little deformation in the so-called ‘landslide body’, and there have been no recorded zones of low shear strength in the soil deposit that are indicative of a basal shear surface. This thesis is a detailed geotechnical study on the fissures along part of Ramahana Road in the Hillsborough Valley, Christchurch. Shallow and deep investigation methods found that the predominant soil is loess-colluvium, to depths of ~20m, and this soil has variable geotechnical characteristics depending on the layer sampled. The factor that has the most influence on shear strength was found to be the moisture content. Direct shear-box testing of disturbed, recompacted loess-colluvium found that the soil had a cohesion of 35-65kPa and a friction angle of 38-43° when the soil moisture content was at 8-10%. However when the moisture content was at 19-20% the soil’s cohesion decreased to 3-5kPa and its friction angle decreased to 33-38°, this moisture content is at or slightly above the plastic limit. An electrical resistivity geophysical survey was conducted perpendicular to multiple fissure traces and through the compressional zone at 17 Ramahana Road. The electrical resistivity line found that there was an area of high resistivity at the toe of the slope, and an area of high conductivity downslope of this and at greater depths. This area correlated to the compressional zone recorded by previous studies. Moisture content testing of the soil in these locations showed that the soil in the resistive area was relatively dry (9%) compared to the surrounding soil (13%), whilst the soil in the conductive area was relatively wet (22%)compared to the surrounding soil (19%). Density tests of the soil in the compressional zone recorded that the resistive area had a higher dry density than the surrounding soil (~1790 kg/m3 compared to ~1650 kg/m3). New springs arose downslope of the compressional zone contemporaneously with the fissures, and it is interpreted that these have arisen from increased hydraulic head in the Banks Peninsula bedrock aquifer system, and earthquake induced-bedrock fracturing. A test pit was dug across an infilled fissure trace at 17 Ramahana Road to a depth of 3m. The fissure trace had an aperture of 450-470mm at the ground surface, but it gradually lost aperture with depth until 2.0-2.1m where it became a segmented fissure trace with 1-2mm aperture. A mixed-colluvium layer was intercepted by the fissure trace at 2.4m depth, and there was no observable vertical offset of this layer. The fissure trace was at an angle of 78° at the ground surface, but it also flattened with depth, which gave it a slightly curved appearance. The fissure trace was at an assumed angle of 40-50° near the base of the test pit. Rotational slide, translational slide and lateral spread landslide movement types were compared and contrasted as possibilities for landslide movement types, whilst an alternative hypothesis was offered that the fissures are tensile failures with a quasi-toppling motion involving a cohesive block of loessial soil moving outwards from the slope, with an accommodating compressional strain in the lower less cohesive soil. The mechanisms behind this movement are suggested to be the horizontal earthquake inertia forces from the Christchurch Earthquake, the static shear stress of the slope, and bedrock uplift of the Port Hills in relation to the subsidence of the Christchurch city flatlands. Extremely high PGA is considered to be a prerequisite to the fissure trace development, and these can only be induced in the Hillsborough Valley from a Port Hills Fault rupture, which has a recurrence interval of ~10,000 years. The current understanding of how the loess-colluvium soil would behave under cyclic loading is limited, and the mechanisms behind the suggested movement type are not completely understood. Further research is needed to confirm the proposed mechanism of the fissure traces. Laboratory tests such as the cyclic triaxial and cyclic shear test would be beneficial in future research to quantitatively test how the soil behaves under cyclic loading at various moisture contents and clay contents, and centrifuge experiments would be of great use to qualitatively test the suggested mode of movement in the loessial soil.

Images, Alexander Turnbull Library

A chimpanzee paints with a palette of colours. Context: After the earthquakes in Christchurch buildings and areas were designated green, blue, red or white depending on the degree of damage. Buildings in the 'red' zone were then examined to ascertain whether they should be demolished or restored and sometimes the land itself was deemed unsafe. There have been many controversial decisions made which is the point the cartoon makes. Quantity: 1 digital cartoon(s).

Images, eqnz.chch.2010

Low tide on the Avon River at New Brighton/Bexley. Note the original bank and the rock wall slipage on right. The white additions were added in March and April 2011 to protect the properties behind from flooding. Ultimately this area was "red zoned" with all houses removed or to be removed and the ground left till a rehabilitation method can ...

Images, Alexander Turnbull Library

In the top frame a man reads a newspaper report that says 'Govt to buy up red stickered homes' and shouts 'That's it - I'm out!' His mate comments that he thought it was his neighbour's house that was munted and that his house was ok. In the lower frame the first man says 'That's right... and I don't want to live next door to a politician?!' Context - A report released 23 June 2011 has divided quake-hit Canterbury into four zones with those in the worst affected residential red zone offered cash to move out. The man in the cartoon thinks that the government is buying up the houses so that politicians can live in them. Colour and black and white versions available Quantity: 2 digital cartoon(s).

Images, Alexander Turnbull Library

In the top frame someone unseen (Murray McCully) in the Beehive says 'John! - There's been a bad reaction to us taking special powers to fix problems in Auckland!' Prime Minister John Key says 'What Murray?' In the lower frame Minister for the Rugby World Cup, Murray McCully, says 'The worst hit parts of Christchurch have declared themselves Fan Zones!' and the PM says 'Oh S..t!' The little Evans man says 'Sounds better than Red Zone!' Context: Refers to the chaos over transport and crowd control in the fanzone when much larger numbers of people flocked to the Rugby World Cup opening and revelry than expected. The government used special powers to take over the management of Queens Wharf fanzone spaces previously managed by an Auckland Council group, thus rather undermining the Mayor, Len Brown and the Auckland City Council. A new plan was signed off under special powers by Murray McCully directly after the fiasco. The Christchurch comment refers to the areas worst hit by the earhquakes. Colour and black and white versions available Quantity: 2 digital cartoon(s).

Images, Alexander Turnbull Library

Text reads 'Bad news for Christchurch playing fields'. On the left is a man wearing the Canterbury colours and carrying a flag; he looks most upset about the 'AMI Stadium' being red stickered. On the right is a woman of the night in fishnet stockings and a very short skirt who looks very upset as she hears that 'Manchester Street' has been red stickered. The little Evans man in the corner says 'Red light, red carded, from the red zone'. Context - The AMI Stadium was supposed to be the venue for the Rugby World Cup in Christchurch - a decision made on 16 March was made that Christchurch was not in a position to host the RWC. With Manchester St on the city side of Bealey Ave cordoned off, street workers have been working from the residential area between Bealey and Purchas St. and residents are furious. Colour and black and white versions of this cartoon are available Quantity: 2 digital cartoon(s).

Images, Alexander Turnbull Library

The cartoon shows three 'Redzone Girls'. The first wears a green tshirt and wears a green 'no restriction' label, the second wears a yellow tshirt and has a yellow 'Limited access' label and the third wears a red tshirt and has a red label that reads 'munted'; she also has a red and white barrier around her. The second and third of the 'girls' are in an increasing state of decrepitude. Behind them is a crumbling brick wall. Context - Christchurch prostitutes aren't letting natural disaster prevent them from plying their trade on the streets despite the dangers of aftershocks in the city. NZPC's Christchurch regional co-ordinator, Anna Reed, said it was a concern sex workers were standing in the shadow of potentially unsafe buildings as the city was shaken by aftershocks, but said the shattered CBD had "left them with no outlet". Christchurch residents are up in arms about the number of prostitutes working in their local neighbourhoods because their usual work areas are out of bounds in the 'red zone'. (Stuff 25 February 2011) Quantity: 1 digital cartoon(s).