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Images, eqnz.chch.2010

Cracks have ripped through external columns of this 7 storey building (corner of Hereford Street / Manchester Street), and efforts are being made to shore up and strengthen it to save it from demolition after it suffered structural damage in the magnitude 7.1 earthquake that struck Christchurch on Saturday 4 September 2010.

Images, eqnz.chch.2010

This is the pedestrian bridge in Kaiapoi close to Christchurch. Not the best angle but the whole bridge on the right hand side is twisted and looks like some kind of rollercoaster. Taken one month after the Quake Twitter |

Images, eqnz.chch.2010

Cracks have ripped through external columns of this 7 storey building (corner of Hereford Street / Manchester Street), and efforts are being made to shore up and strengthen it to save it from demolition after it suffered structural damage in the magnitude 7.1 earthquake that struck Christchurch on Saturday 4 September 2010.

Images, eqnz.chch.2010

Cracks have ripped through external columns of this 7 storey building (corner of Hereford Street / Manchester Street), and efforts are being made to shore up and strengthen it to save it from demolition after it suffered structural damage in the magnitude 7.1 earthquake that struck Christchurch on Saturday 4 September 2010.

Images, UC QuakeStudies

Two men carry backpacks and shopping bags along Tuam Street, stepping over emergency tape that lies across the road. Brick dust covers the street where fallen bricks have been cleared. The photographer comments, "Two members of our office carrying gear through the cordon. This was taken shortly after the 4th September earthquake. Police allowed us free access past the cordon and simply advised us to watch out for falling masonry. The access situation was much different after the February aftershock".

Images, UC QuakeStudies

Photograph captioned by Fairfax, "Christchurch Earthquake. Christchurch was rocked by a large aftershock shortly after 8am this morning. Social Development Minister Paula Bennett has donated money to the thousand of students who have filled the suburbs lending a hand to residents to clean up their properties. Bennett chats to volunteers (L-R) Sophie Cornish, Ashley Cornish, Laura Jackson, Shannon Ronald, Kirsten Glasson and Lauren Baker".

Images, Canterbury Museum

One white cotton t-shirt with black seismograph-like patterns in the shape of ChristChurch Cathedral. Produced to commemorate the 7.1 magnitude earthquake that struck Canterbury at 4.35am on 4 September 2010. This t-shirt was designed and manufactured by Auckland based t-shirt company Mr Vintage in October 2010 to commemorate the 7.1 magnitude ...

Images, eqnz.chch.2010

It would have been a glorious Spring day in Christchurch had it not been for the magnitude 7.1 earthquake at 4:30 am. All the water and silt you can see covering the street in this photo erupted from the ground following the earthquake.

Videos, UC QuakeStudies

A video about the government's financial aid plan for workers affected by the 4 September 2010 earthquake. Prime Minister John Key has travelled to Christchurch to announce the plan. This video includes footage of a press conference with John Key at the Christchurch Art Gallery. It also includes footage of John Key meeting residents at the Civil Defence Centre at Addington Raceway.

Images, UC QuakeStudies

Director of Gap Filler, Coralie Winn, setting up a sign in front of 832 Colombo Street. The sign reads, "Welcome! This site was home to South of the Border (Mexican Restaurant) and Denis Moore, Auto Electrician. Please keep your shoes on! Please be aware that the ground is uneven. Local by-laws applies - no alcohol on the street. For safety, we cannot over-crowd the site. ROAR. Please do buy a coffee, a cake and bring a picnic to enjoy. Thanks. Gap Filler".

Articles, UC QuakeStudies

A post on the NZ Raw blog written by Mark Lincoln on 4 September 2010. Mark says, "This is the first [blog post] I wrote on 4th Sept. I always remember an announcer on the radio having the first on-air interview with Geonet/EQC (obviously only 1 or 2 staff members at that stage!). The announcer asked if the aftershocks would carry on for much longer and the Geonet guy said they could carry on for a few weeks. Radio announcer seemed shocked".

Research papers, University of Canterbury Library

Liquefaction of sandy soil has been observed to cause significant damage to infrastructure during major earthquakes. Historical cases of liquefaction have typically occurred in sands containing some portion of fines particles, which are defined as 75μm or smaller in diameter. The effects of fines on the undrained behaviour of sand are not however fully understood, and this study therefore attempts to quantify these effects through the undrained testing of sand mixed with non-plastic fines sourced from Christchurch, New Zealand. The experimental program carried out during this study consisted of undrained monotonic and cyclic triaxial tests performed on three different mixtures of sand and fines: the Fitzgerald Bridge mixture (FBM), and two Pinnacles Sand mixtures (PSM1 and PSM2). The fines content of each host sand was systematically varied up to a maximum of 30%, with all test specimens being reconstituted using moist tamping deposition. The undrained test results from the FBM soils were interpreted using a range of different measures of initial state. When using void ratio and relative density, the addition of fines to the FBM sand caused more contractive behaviour for both monotonic and cyclic loadings. This resulted in lower strengths at the steady state of deformation, and lower liquefaction resistances. When the intergranular void ratio was used for the interpretation, the effect of additional fines was to cause less contractive response in the sand. The state parameter and state index were also used to interpret the undrained cyclic test results – these measures suggested that additional fines caused less contractive sand behaviour, the opposite to that observed when using the void ratio. This highlighted the dependency on the parameter chosen as a basis for the response comparison when determining the effects of fines, and pointed out a need to identify a measure that normalizes such effects. Based on the FBM undrained test results and interpretations, the equivalent granular void ratio, e*, was identified from the literature as a measure of initial state that normalizes the effects of fines on the undrained behaviour of sand up to a fines content of 30%. This is done through a parameter within the e* definition termed the fines influence factor, b, which quantifies the effects of fines from a value of zero (no effect) to one (same effect as sand particles). The value of b was also determined to be different when interpreting the steady state lines (bSSL) and cyclic resistance curves (bCR) respectively for a given mixture of sand and fines. The steady state lines and cyclic resistance curves of the FBM soils and a number of other sand-fines mixtures sourced from the literature were subsequently interpreted using the equivalent granular void ratio concept, with bSSL and bCR values being back-calculated from the respective test data sets. Based on these interpretations, it was concluded that e* was conceptually a useful parameter for characterizing and quantifying the effects of fines on the undrained behaviour of sand, assuming the fines influence factor value could be derived. To allow prediction of the fines influence factor values, bSSL and bCR were correlated with material and depositional properties of the presented sand-fines mixtures. It was found that as the size of the fines particles relative to the sand particles became smaller, the values of bSSL and bCR reduced, indicating lower effect of fines. The same trend was also observed as the angularity of the sand particles increased. The depositional method was found to influence the value of bCR, due to the sensitivity of cyclic loading to initial soil fabric. This led to bSSL being used as a reference for the effect of fines, with specimens prepared by moist tamping having bCR > bSSL, and specimens prepared by slurry deposition having bCR < bSSL. Finally the correlations of the fines influence factor values with material and depositional properties were used to define the simplified estimation method – a procedure capable of predicting the approximate steady state lines and cyclic resistance curves of a sand as the non-plastic fines content is increased up to 30%. The method was critically reviewed based on the undrained test results of the PSM1 and PSM2 soils. This review suggested the method could accurately predict undrained response curves as the fines content was raised, based on the PSM1 test results. It also however identified some key issues with the method, such as the inability to accurately predict the responses of highly non-uniform soils, a lack of consideration for the entire particle size distribution of a soil, and the fact the errors in the prediction of bSSL carry through into the prediction of bCR. Lastly some areas of further investigation relating to the method were highlighted, including the need to verify the method through testing of sandy soils sourced from outside the Christchurch area, and the need to correlate the value of bCR with additional soil fabrics / depositional methods.

Images, Alexander Turnbull Library

Shows a graph illustrating the 'Growth forecast' for the economy. A large finger representing the 'Reserve Bank' squashes the growth arrow as though it is a fly and it starts to zig-zag crazily downwards. The statement made 16th September looked a shadow of the bright one the Reserve Bank published three months ago. With its forecasts finalised the day before the Canterbury earthquake struck, the Bank has taken secateurs to its economic growth track, and a carving knife to its interest rate path. Instead of GDP growth pushing 4% this year and next, for example, it now struggles to reach 3% in each. It's tempting to think this has been driven by the wobbling international news over recent months. In fact it's been because of a suddenly sombre view around NZ consumer spending and the housing market. (Interest.co.nz) Quantity: 1 digital cartoon(s).

Images, UC QuakeStudies

Alan Hoskin, a member of the University of Canterbury's E-Learning team, in their temporary office in the James Hight building. The photographer comments, "First looks at our new temporary (maybe) office space. Our group will stay here until April or May 2011, then will move to another floor in the Central Library. 700 hall with Alan. The corridor has a small seminar room at the end, and our offices on the right. To the left is the open sitting and reception area; we're trying to think of ways to make use of this".

Images, eqnz.chch.2010

The base of the tower on the right of this picture has sunk about 25cm so that the lower course of bricks have disappeared below ground level. Meanwhile the other end of the building has sunk about 50cm splitting the building into thirds. The sand you can see is what came bubbling up out of the ground due to liquifaction. Unfortunately the build...

Images, eqnz.chch.2010

The base of the tower on the right of this picture has sunk about 25cm so that the lower course of bricks have disappeared below ground level. Meanwhile the other end of the building has sunk about 50cm splitting the building into thirds. The sand you can see is what came bubbling up out of the ground due to liquifaction. Unfortunately the build...

Videos, UC QuakeStudies

A video about the contrasting experiences of business owners in Beckenham after the 4 September 2010 earthquake. The video includes an interview with Fred Arnesen, owner of Beckenham Footware & Engravers, and Fiona Fidow and Jeanie Smith, owners of The Cupcake Collection. The stores are on opposite sides of Colombo Street, with the west side suffering severe damage, and the east side suffering very little. Because of this, the Beckenham Footware & Engravers has had to close, while The Cupcake Collection is able to continue operating.

Images, eqnz.chch.2010

The base of the tower on the right of this picture has sunk about 25cm so that the lower course of bricks have disappeared below ground level. Meanwhile the other end of the building has sunk about 50cm splitting the building into thirds. The sand you can see is what came bubbling up out of the ground due to liquifaction. Unfortunately the build...

Audio, Radio New Zealand

1. AMY ADAMS to the Minister of Finance: What progress has the Government made this year in laying the foundations for a more ambitious and faster growing economy? 2. Hon PHIL GOFF to the Prime Minister: Does he stand by his statement that by early 2010 New Zealand will be coming out of the recession "reasonably aggressively"? 3. ALLAN PEACHEY to the Minister of Education: What feedback has she received about the quality of school reports to parents this year? 4. Hon CLAYTON COSGROVE to the Minister for Canterbury Earthquake Recovery: Is he satisfied that the Canterbury earthquake business support measures undertaken by the Government have worked as intended? 5. Dr KENNEDY GRAHAM to the Minister for Climate Change Issues (International Negotiations): Will the Cancun Agreements achieve the agreed goal of confining global warming to 2 degrees Celsius by 2020; if so, how? 6. Dr PAUL HUTCHISON to the Minister of Health: What reports has he received on improved access to medicines? 7. Hon DAMIEN O'CONNOR to the Prime Minister: Does he stand by his statement that "It's clearly been a large sum of money. But at the end of the day I gave a commitment to the families at Pike River I'd do everything I could to get their men out, I stand by that. I think the Government has done everything it can do so far"? 8. Dr CAM CALDER to the Minister of Corrections: Has she received any progress reports on the Government's Prisoner Skills and Employment Strategy? 9. Hon DAVID PARKER to the Minister for Economic Development: How many additional Cabinet papers has he submitted to Cabinet since he told the House in July "In my capacity as Minster for Economic Development I have submitted 14 papers to Cabinet in the last 6 months"? 10. HONE HARAWIRA to the Minister of Foreign Affairs: What steps has the New Zealand Government taken to denounce the shooting by Chilean forces of indigenous Rapa Nui, during an operation to evict them from stolen ancestral lands that they were seeking to reclaim? 11. Hon JIM ANDERTON to the Minister for ACC: Does he have any concerns about the way ACC in general and claims general manager Denise Cosgrove in particular, is interpreting ACC legislation regarding personal injury claims which are being declined on the basis of degeneration or pre-existing conditions? 12. COLIN KING to the Minister of Fisheries: How will fisheries officers be helping to better protect New Zealand's fisheries this summer?

Images, UC QuakeStudies

A photograph of a green sticker on the window of The Dolls House Shop antique store on Colombo Street. The sticker indicates that the store is safe to enter. The sign reads, "Inspected, no restriction on use or occupancy. This building has received a brief inspection only. While no apparent structural or other safety hazards have been found, a more comprehensive inspection of the exterior and interior may reveal safety hazards". The structural engineer has written on the sign "propping to rear of building inadequate, fire egress also at rear inappropriate, no occupancy to second storey".

Images, UC QuakeStudies

The University of Canterbury's E-Learning team's temporary office in the James Hight building. The photographer comments, "First looks at our new temporary (maybe) office space. Our group will stay here until April or May 2011, then will move to another floor in the Central Library. My desk. I hope to get blinds to cover this internal window. Later - blinds are not allowed, so I rotated the desk 180 degrees. My back is now facing the window, but I'm far enough away that people won't be able to read my screens - and I don't have to look at people looking at me".

Research papers, University of Canterbury Library

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.

Images, Alexander Turnbull Library

The cartoon shows a platter of 'Brownbait patties $2 per kilo'. In the background is a 'contaminated' river. Refers to the contamination of Canterbury's waterways after the earthquake of 4th September which resulted in sewage pipes being damaged thus contaminating the rivers. This means that people should not be attempting to catch whitebait in these rivers during the annual whitebait season which is open between 15 August and 30 November. Quantity: 1 digital cartoon(s).

Articles, UC QuakeStudies

This report provided information on the location and character of the Ostler Fault Zone near Twizel. The fault traces, and associated recommended fault avoidance zones, were mapped in detail for inclusion in a District Plan Change for the Twizel area. The Ostler Fault Zone was mapped in detail because of the higher likelihood of movement on that fault than others in the district, and the potential for future development across the fault zone because of its proximity to Twizel. See Object Overview for background and usage information. The report recommended that the information be incorporated into the District Plan Change and that site-specific investigations be undertaken before development is allowed within the fault avoidance zones. These recommendations were taken up by Mackenzie District Council.