A video of journalist Charlie Gates introducing the 2014 World Buskers Festival. Gates visits former festival venues in the Christchurch central city and the new performance venues for the 2014 festival, to show how the city has changed since the 2010 and 2011 earthquakes.
Shows a hand lifting a house up from the ground, as the earth shakes and rumbles around it. A voice in the earth says, 'I'm still here'. Refers to ongoing earthquakes and aftershocks following the devastating 2010 and 2011 earthquakes in Canterbury. Quantity: 1 digital cartoon(s).
Rt Hon WINSTON PETERS to the Prime Minister: Does he stand by his statement that "the Government has actively supported the filming of the Hobbit movies in New Zealand because of the enormous economic benefits they are bringing to the country, including the creation of around 3,000 jobs"? DAVID SHEARER to the Prime Minister: Does he stand by all the statements made in his prime ministerial speeches and in his Address in Reply speeches? TODD McCLAY to the Minister of Finance: What will be the focus of the Government's economic programme in 2013? METIRIA TUREI to the Prime Minister: Does he stand by his statement that "I am keen to see New Zealanders be able to afford to buy a home", given that the home ownership rate has continued to decline under his watch and home buying is becoming less affordable? Hon DAVID PARKER to the Minister of Finance: Is he aware that anticipated Core Crown Revenue for the period 2012-2016 decreased by $13.2 billion between the October 2011 PREFU and the December 2012 HYEFU; if so, why has the Government lost $13.2 billion in projected revenue in little over a year? COLIN KING to the Minister for Tertiary Education, Skills and Employment: What recent announcements has the Government made about boosting the number of people being trained in apprenticeships? JACINDA ARDERN to the Prime Minister: Does he stand by his statement "I am deeply concerned about every child in New Zealand who is in poverty"? Dr RUSSEL NORMAN to the Prime Minister: Why didn't he mention climate change yesterday when he outlined his Government's priorities for the year in his statement to Parliament? Hon ANNETTE KING to the Prime Minister: Following his decision to appoint a new Minister of Housing, what new policies, if any, does he expect his new Minister to implement to address the growing housing affordability issues in New Zealand? NICKY WAGNER to the Minister responsible for the Earthquake Commission: What progress has been made in the repair of homes in Canterbury by the EQR Repair Programme? CHRIS HIPKINS to the Minister of State Services: What were the factors that contributed to the strained relations that resulted in the resignation of Lesley Longstone as Secretary of Education? JACQUI DEAN to the Minister of Corrections: What steps is the Government taking to improve prisoner employment training in New Zealand prisons?
The Mѡ=7.1 Darfield (Canterbury) earthquake struck on 4 September 2010, approximately 45 km west of Christchurch, New Zealand. It revealed a previously unknown fault (the Greendale fault) and caused billions of dollars of damage due to high peak ground velocities and extensive liquefaction. It also triggered the Mw=6.3 Christchurch earthquake on 22 February 2011, which caused further damage and the loss of 185 lives. The objective of this research was to determine the relationship between stress and seismic properties in a seismically active region using manually-picked P and S wave arrival times from the aftershock sequence between 8 September 2010-13 January 2011 to estimate shear-wave splitting (SWS) parameters, VP =VS-ratios, anisotropy (delay-time tomography), focal mechanisms, and tectonic stress on the Canterbury plains. The maximum horizontal stress direction was highly consistent in the plains, with an average value of SHmax=116 18 . However, the estimates showed variation in SHmax near the fault, with one estimate rotating by as much as 30° counter-clockwise. This suggests heterogeneity of stress at the fault, though the cause remains unclear. Orientations of the principal stresses predominantly indicate a strike-slip regime, but there are possible thrust regimes to the west and north/east of the fault. The SWS fast directions (ø) on the plains show alignment with SHmax at the majority of stations, indicating stress controlled anisotropy. However, structural effects appear more dominant in the neighbouring regions of the Southern Alps and Banks Peninsula.