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Images for Rangiora; more images...

Audio, Radio New Zealand

One of the great community initiative's in Canterbury is the Rangiora Earthquake Express - where urgent help is still needed. These Rangiora volunteers have been up and running for sometime now, with daily runs into the Christchurch suburbs most desperately in need of water and other essential supplies.

Audio, Radio New Zealand

The Rangiora Earthquake Express was the brain child of Brendan Malone and his mate Chris who, on Wednesday last week, came up with an idea to help the citizens of East Christchurch.

Audio, UC QuakeStudies

An audio recording of Fr Dan Doyle's interview for the Church in the Quakes Project. The interview was conducted by Melissa Parsons on 31 October 2012. Doyle is a Catholic priest, formerly for the Parish of Rangiora. Currently he is a priest at St Anne's, Woolston.

Audio, Radio New Zealand

There are many tales of generosity beginning in emerge in Christchurch. Evan Coster from Rangiora was working in Harvey Norman when the earthquake struck on Tuesday. He doesn't know if he has a job to go back to and with time on his hands wanted to do something useful. He started visiting local businesses in Rangiora such as Warehouse, Countdown, New World and service stations for donations of cups, coffee, sugar and milk. Then he rallied friends and family together and started delivering refreshments to emergency workers in all of the cordons in the CBD.

Images, UC QuakeStudies

Photograph captioned by Fairfax, "Teddy time: A Whanganui man has sent dozens of teddy bears to Rangiora to be distributed to children affected by the Canterbury earthquake. Ted Cheriton sent the teddies to National MP Kate Wilkinson's office to be distributed. Ms Wilkinson said it was a fantastic gesture. 'I am sure they will be welcome in Kaiapoi and beach settlements where damage from the earthquake has severely affected many families', she said. 'Hopefully these teddies will bring a smile to some young children and cheer them up in what has been a very trying and traumatic time'".

Research papers, University of Canterbury Library

This study contains an evaluation of the seismic hazard associated with the Springbank Fault, a blind structure discovered in 1998 close to Christchurch. The assessment of the seismic hazard is approached as a deterministic process in which it is necessary to establish: 1) fault characteristics; 2) the maximum earthquake that the fault is capable of producing and 3) ground motions estimations. Due to the blind nature of the fault, conventional techniques used to establish the basic fault characteristics for seismic hazard assessments could not be applied. Alternative methods are used including global positioning system (GPS) surveys, morphometric analyses along rivers, shallow seismic reflection surveys and computer modelling. These were supplemented by using multiple empirical equations relating fault attributes to earthquake magnitude, and attenuation relationships to estimate ground motions in the near-fault zone. The analyses indicated that the Springbank Fault is a reverse structure located approximately 30 km to the northwest of Christchurch, along a strike length of approximately 16 km between the Eyre and Ashley River. The fault does not reach the surface, buy it is associated with a broad anticline whose maximum topographic expression offers close to the mid-length of the fault. Two other reverse faults, the Eyrewell and Sefton Faults, are inferred in the study area. These faults, together with the Springbank and Hororata Faults and interpreted as part of a sys of trust/reverse faults propagating from a decollement located at mid-crustal depths of approximately 14 km beneath the Canterbury Plains Within this fault system, the Springbank Fault is considered to behave in a seismically independent way, with a fault slip rate of ~0.2 mm/yr, and the capacity of producing a reverse-slip earthquake of moment magnitude ~6.4, with an earthquake recurrence of 3,000 years. An earthquake of the above characteristics represents a significant seismic hazard for various urban centres in the near-fault zone including Christchurch, Rangiora, Oxford, Amberley, Kaiapoi, Darfield, Rollestion and Cust. Estimated peak ground accelerations for these towns range between 0.14 g to 0.5 g.

Research Papers, Lincoln University

The New Zealand Kellogg Rural Leaders Programme develops emerging agribusiness leaders to help shape the future of New Zealand agribusiness and rural affairs. Lincoln University has been involved with this leaders programme since 1979 when it was launched with a grant from the Kellogg Foundation, USA.At 4.35am on 4th September 2010, Canterbury was hit by an earthquake measuring 7.1 on the Richter scale. On 22nd February 2011 and 13th June 2011 a separate fault line approximately 35km from the first, ruptured to inflict two further earthquakes measuring 6.3 and 6.0 respectively. As a direct result of the February earthquake, 181 people lost their lives. Some commentators have described this series of earthquakes as the most expensive global insurance event of all time. These earthquakes and the more than 7000 associated aftershocks have had a significant physical impact on parts of Canterbury and virtually none on others. The economic, social and emotional impacts of these quakes spread across Canterbury and beyond. Waimakariri district, north of Christchurch, has reflected a similar pattern, with over 1400 houses requiring rebuild or substantial repair, millions of dollars of damage to infrastructure, and significant social issues as a result. The physical damage in Waimakiriri District was predominately in parts of Kaiapoi, and two small beach settlements, The Pines and Kairaki Beach with pockets elsewhere in the district. While the balance of the district is largely physically untouched, the economic, social, and emotional shockwaves have spread across the district. Waimakariri district consists of two main towns, Rangiora and Kaiapoi, a number of smaller urban areas and a larger rural area. It is considered mid-size in the New Zealand local government landscape. This paper will explore the actions and plans of Waimakiriri District Council (WDC) in the Emergency Management Recovery programme to provide context to allow a more detailed examination of the planning processes prior to, and subsequent to the earthquakes. This study looked at documentation produced by WDC, applicable legislation and New Zealand Emergency Management resources and other sources. Key managers and elected representatives in the WOC were interviewed, along with a selection of governmental and nongovernmental agency representatives. The interview responses enable understanding of how central Government and other local authorities can benefit from these lessons and apply them to their own planning. It is intended that this paper will assist local government organisations in New Zealand to evaluate their planning processes in light of the events of 2010/11 in Canterbury and the lessons from WDC.