Questions to Ministers
1. GARETH HUGHES to the Minister for Primary Industries: Will he extend the Taranaki set net ban after the recent death of a Maui's dolphin in a fishing net?
2. DAVID BENNETT to the Minister for Economic Development: What actions is the Government taking to boost economic linkages with China?
3. GRANT ROBERTSON to the Prime Minister: Does he stand by his statement that his hour-long show on Radio Live on 30 September 2011 was an "election free zone"?
4. Dr PAUL HUTCHISON to the Minister of Health: What improvements, if any, have been made to the Government's national health targets?
5. Hon LIANNE DALZIEL to the Minister for Canterbury Earthquake Recovery: Did he discuss with the Christchurch City Mayor reported claims that there had been overtures from within The Treasury that there was scope for the city's rates to be increased or for assets to be sold to pay for the quake recovery, and that this could be done under the Canterbury Earthquake Recovery Act before he called him a clown; if not, why not?
6. JACQUI DEAN to the Minister of Local Government: What reports has he received on increases in local government council debt since the Local Government Act 2002 was enacted?
7. DARIEN FENTON to the Minister of Labour: Does she stand by her statement that the new minimum wage announced yesterday "strikes the right balance between protecting low paid workers and ensuring that jobs are not lost."?
8. PESETA SAM LOTU-IIGA to the Minister of Consumer Affairs: What recent announcements has the Government made on protecting consumers from loan sharks?
9. CLARE CURRAN to the Minister of Broadcasting: Is he aware that Stephen McElrea is part of a working group within NZ On Air, which includes a representative of MediaWorks, and which is determining details of a documentary about Whānau Ora?
10. TIM MACINDOE to the Minister for the Community and Voluntary Sector: What recent announcement has she made in her portfolio that will benefit communities?
11. HOLLY WALKER to the Minister for Social Development: Does she consider low family incomes to be a major contributor to childhood vulnerability?
12. Rt Hon WINSTON PETERS to the Prime Minister: Does he still have confidence in all his Ministers?
1. Rt Hon WINSTON PETERS to the Prime Minister: Has he had time to read and digest the judgement of Justice Miller regarding the Crafar farm deal; if so, does he stand by his comments made in the House yesterday?
2. Hon DAVID PARKER to the Minister for Land Information: Does he believe he and the Government have conducted themselves competently and appropriately in relation to the decision to approve the purchase of the Crafar farms by a foreign buyer; if not, what did they do wrong?
3. JONATHAN YOUNG to the Minister of Finance: What reports has the Government issued on the economy?
4. JACINDA ARDERN to the Minister for Social Development: Does she have confidence that Work and Income meets their own "case management approach" expectations?
5. JAN LOGIE to the Minister for Social Development: Does she have concerns that changes to the eligibility for the Training Incentive Allowance are causing single parent beneficiaries to consider working in the sex industry?
6. Dr CAM CALDER to the Minister of Health: What improvements have there been to services for patients as a result of greater collaboration between District Health Boards?
7. Hon CLAYTON COSGROVE to the Minister for State Owned Enterprises: Does he still intend to sell 49 per cent of the four State-owned energy companies?
8. JAMI-LEE ROSS to the Minister of Local Government: What analysis has he received on rate increases across New Zealand's 78 councils following the enactment of new local government legislation in 2002?
9. Hon LIANNE DALZIEL to the Minister for Canterbury Earthquake Recovery: Does he stand by the part of his statement of 27 January, announcing the extension of the red zone offer to retirement villages, that letters of offer would be sent to each resident and CERA would work with village owners as quickly as possible to ensure the residents are assisted; if not, why not?
10. Dr RUSSEL NORMAN to the Minister for Land Information: Did Overseas Investment Office officials meet with Chinese political consul Cheng Lei late last year; if so, did they discuss Shanghai Pengxin's bid for the Crafar farms?
11. CLARE CURRAN to the Minister of Broadcasting: What is the name of the documentary which was withheld in the papers released publicly by NZ On Air titled "Records of decisions made at working group meeting"?
12. Hon TAU HENARE to the Minister for Economic Development: What progress has he made declaring the Volvo Ocean Race Stopover a major event under the Major Events Management Act 2007?
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.
