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Videos, UC QuakeStudies

A video of interviews with primary and high-school students about their experiences during the 22 February 2011 earthquake. The students interviewed include (Paityn Ower from Avondale Primary School; Leah Temesvari, Ryan Cleaver, Jenna Hayes, and Logan Emery from Kaiapoi High School; Nikora Webster-Epiha, Grace Smith, and Natasha Gordon from Wainoni School; and Harry Loughan, Rebecca Lane, Scott Price, Maltin Tauave, Charlie Kavanagh, and Amy Sisson from Linwood College. This video was part of The Press's 'Christchurch, one year after February 22, 2011' series.

Images, Alexander Turnbull Library

Text across the top of the cartoon reads 'Greener pastures for red zone residents?... A new subdivision named 'Quakehaven' has streets named 'Wobble Way', 'Poopong Parade', 'Turd Tce.', 'Liquefaction Lane' etc. One of a couple visiting the new area says 'I've got a bad feeling about this new subdivision!' Context - Housing after the Christchurch earthquakes. After the first Land Report was delivered on 23rd June people whose houses were in the Red Zone had their properties bought up by the government and now have to move to new subdivisions. The suggestion in the cartoon is that the subdivisions may not be on safe ground. Quantity: 1 digital cartoon(s).

Research papers, University of Canterbury Library

The New Zealand city of Christchurch suffered a series of devastating earthquakes in 2010-11 that changed the urban landscape forever. A new rebuilt city is now underway, largely based on the expressed wishes of the populace to see Christchurch return to being a more people-oriented, cycle-friendly city that it was known for in decades past. Currently 7% of commuters cycle to work, supported by a 200km network of mostly conventional on-road painted cycle lanes and off-road shared paths. The new "Major Cycleways" plan aims to develop approximately 100km of high-quality cycling routes throughout the city in 5-7 years. The target audience is an unaccompanied 10-year-old cycling, which requires more separated cycleways and low-volume/speed "neighbourhood greenways" to meet this standard. This presentation summarises the steps undertaken to date to start delivering this network. Various pieces of research have helped to identify the types of infrastructure preferred by those currently not regularly cycling, as well as helping to assess the merits of different route choices. Conceptual cycleway guidelines have now been translated into detailed design principles for the different types of infrastructure being planned. While much of this work is based on successful designs from overseas, including professional advice from Dutch practitioners, an interesting challenge has been to adapt these designs as required to suit local road environments and road user expectations. The first parts of the new network are being rolled out now, with the hope that this will produce an attractive and resilient network for the future population that leads to cycling being a major part of the local way of life.

Research papers, University of Canterbury Library

Following the 22 February 2011, MW 6.2 earthquake located on a fault beneath the Port Hills of Christchurch, fissuring of up to several hundred metres in length was observed in the loess and loess-colluvium of foot-slope positions in north-facing valleys of the Port Hills. The fissuring was observed in all major valleys, occurred at similar low altitudes, showing a contour-parallel orientation and often accompanied by both lateral compression/extension features and spring formation in the valley floor below. Fissuring locations studied in depth included Bowenvale Valley, Hillsborough Valley, Huntlywood Terrace–Lucas Lane, Bridle Path Road, and Maffeys Road–La Costa Lane. Investigations into loess soil, its properties and mannerisms, as well as international examples of its failure were undertaken, including study of the Loess Plateau of China, the Teton Dam, and palaeo-fissuring on Banks Peninsula. These investigations lead to the conclusion that loess has the propensity to fail, often due to the infiltration of water, the presence of which can lead to its instantaneous disaggregation. Literature study and laboratory analysis of Port Hills loess concluded that is has the ability to be stable in steep, sub-vertical escarpments, and often has a sub-vertically jointed internal structure and has a peak shear strength when dry. Values for cohesion, c (kPa) and the internal friction angle, ϕ (degrees) of Port Hills loess were established. The c values for the 40 Rapaki Road, 3 Glenview Terrace loess samples were 13.4 kPa and 19.7 kPa, respectively. The corresponding ϕ values were thought unusually high, at 42.0° and 43.4°.The analysed loess behaved very plastically, with little or no peak strength visible in the plots as the test went almost directly to residual strength. A geophysics resistivity survey showed an area of low resistivity which likely corresponds to a zone of saturated clayey loess/loess colluvium, indicating a high water table in the area. This is consistent with the appearances of local springs which are located towards the northern end of each distinct section of fissure trace and chemical analysis shows that they are sourced from the Port Hills volcanics. Port Hills fissuring may be sub-divided into three categories, Category A, Category B, and Category C, each characterised by distinctive features of the fissures. Category A includes fissures which display evidence of, spring formation, tunnel-gullying, and lateral spreading-like behaviour or quasi-toppling. These fissures are several metres down-slope of the loess-bedrock interface, and are in valleys containing a loess-colluvium fill. Category B fissures are in wider valleys than those in Category A, and the valleys contain estuarine silty sediments which liquefied during the earthquake. Category C fissures occurred at higher elevations than the fissures in the preceding categories, being almost coincident with bedrock outcropping. It is believed that the mechanism responsible for causing the fissuring is a complex combination of three mechanisms: the trampoline effect, bedrock fracturing, and lateral spreading. These three mechanisms can be applied in varying degrees to each of the fissuring sites in categories A, B, and C, in order to provide explanation for the observations made at each. Toppling failure can describe the soil movement as a consequence of the a three causative mechanisms, and provides insight into the movement of the loess. Intra-loess water coursing and tunnel gullying is thought to have encouraged and exacerbated the fissuring, while not being the driving force per se. Incipient landsliding is considered to be the least likely of the possible fissuring interpretations.

Audio, Radio New Zealand

MARAMA DAVIDSON to the Minister of Housing and Urban Development: Will he commit to ensuring that the 800 tenancies terminated or otherwise affected by Housing New Zealand’s previous approach to meth testing receive compensation that genuinely reflects the level of harm done, and takes account of both direct costs and emotional distress? Hon JUDITH COLLINS to the Minister of Housing and Urban Development: Is it acceptable for Housing New Zealand tenants to smoke methamphetamine in Housing New Zealand houses? Hon PAUL GOLDSMITH to the Minister of Finance: Does he stand by all of the statements, actions, and policies of the Government in relation to the New Zealand economy? RINO TIRIKATENE to the Minister for Māori Crown Relations: Te Arawhiti: What recent announcements has he made on the scope of his new portfolio? Hon Dr NICK SMITH to the Minister of State Services: What are the dates and contents of all work-related electronic communications between former Minister Hon Clare Curran and the Prime Minister since the decision in Cabinet last year “that the CTO be appointed by, and accountable to, the Prime Minister and the Ministers of Government Digital Services and Broadcasting, Communications and Digital Media”? Dr DEBORAH RUSSELL to the Minister of Finance: What is his reaction to the Independent Tax Working Group’s interim report released today? Hon NIKKI KAYE to the Minister of Education: How many communications has she received from teachers or principals in the last three days regarding teacher shortages, relief teacher issues, and increases in class sizes, and is she confident there will be no more primary teacher strikes this year? Hon NATHAN GUY to the Minister for Biosecurity: How many inbound passengers arrived at Auckland International Airport yesterday between 2 a.m. and 5 a.m., and how many dog detector teams worked on the Green Lane at this time? TAMATI COFFEY to the Minister of Housing and Urban Development: What steps is the Government taking to ensure Housing New Zealand is a compassionate landlord focused on tenant well-being? STUART SMITH to the Minister for Courts: Is he confident that the Canterbury Earthquakes Insurance Tribunal will comply with all requirements of the rule of law? SIMEON BROWN to the Minister of Health: When did the Expert Advisory Committee on drugs give its advice that synthetic cannabinoids AMB-FUBINACA and 5F-ADB be scheduled as Class A controlled drugs, and what action has he taken on this advice? ANAHILA KANONGATA'A-SUISUIKI to the Minister of Commerce and Consumer Affairs: What measures has the Government announced to protect the public from unscrupulous wheel-clamping practices?