A pdf copy of a SCIRT school visit feedback form from Richmond Primary School.
A gap between two walls at Halswell Primary School. The gap was caused by two buildings separating during the 4 September earthquake.
Broken pavement in the Halswell Primary School grounds. Somebody has pulled apart the broken pavement and placed it in a pile in the middle of a netball court.
Broken pavement in the Halswell Primary School grounds. Silt from liquefaction can also be seen.
Tape reading, "Danger Keep Out" on the gate to Halswell Primary School. A sign has been stabled to the tape reading, "No unauthorised entry".
Cracking along the pavement at Halswell Primary School. The ground has risen and fallen in places leaving an uneven surface where the children usually play.
An entry from Sue Davidson's blog for 21 October 2013 entitled, "Classes underway at Shirley Primary School".
New re-locatable classrooms being readied for use at Halswell School.
The playground at Halswell School.
Heart-shaped notes on the fence of Burwood Primary School. The notes express appreciation for the efforts of the civil defence, fire service, volunteers and council workers from the students of Burwood Primary.
A tree stump at Halswell School.
A sand volcano in the Halswell Primary School grounds near the playground. Sand volcanoes were caused by liquefaction where the soil loses its strength during the earthquake and the silt rises upwards, ejecting out of a hole like magma in a volcano.
A sand volcano in the Halswell Primary School grounds. Sand volcanoes were caused by liquefaction where the soil loses its strength during the earthquake and the silt rises upwards, ejecting out of a hole like magma in a volcano.
A photograph of the gates of Halswell School.
A muddy patch on the grass at Halswell School.
The stump of an oak tree in the Halswell Primary School grounds. The oak tree had the be cut down after it broke during the earthquake and was hanging at a angle. The person who cut down the tree has carved "1870 - 16:9:2010" into the stump, the year that the tree was planted, and then the day that it broke and fell.
Photograph captioned by BeckerFraserPhotos, "Halswell School shows few signs of the earthquake damage it suffered in September 2010".
A reassuring sign hangs on the gate at Lyttelton Main primary school. It reads, 'School is safe, have a good day'.
A presentation given to St Martin's primary school students about SCIRT work in Opawa and Hillsborough.
Children play on the netball court at Lyttelton Main primary school. The surface of the court has been warped by the earthquakes.
An aerial photograph of Central New Brighton School in New Brighton.
A typical "sand volcano" caused by liquefaction where the soil loses its strength during the earthquake and the silt rises upwards, ejecting out of a hole like magma in a volcano.
One of several containers now on the Halswell School grounds while reconstruction takes place.
Heart-shaped notes on the fence of Burwood Primary School. The notes express appreciation for the efforts of the civil defence, fire service, volunteers and council workers from the students of Burwood Primary.
Heart-shaped notes on the fence of Burwood Primary School. The notes express appreciation for the efforts of the civil defence, fire service, volunteers and council workers from the students of Burwood Primary.
Photograph captioned by BeckerFraserPhotos, "Porta Showers set up in Burwood Primary School for the community".
A banner on the fence of Burwood Primary School expressing the student's appreciation for the efforts of the civil defence, fire service, volunteers and council workers with a banner on their school fence. On each heart-shape note is a personal message from the students.
A sign outside a community showering facility set up at the Burwood Primary School. The sign reads, "Community Shower. Open 7am to 7pm".
An aerial photograph of St Paul's School in Dallington. The photograph has been captioned by BeckerFraserPhotos, "St Pauls School, 17 Gayhurst Road, suffered badly from liquefaction in the September earthquake. This area is all red zoned".
A video of a presentation by Professor David Johnston during the fourth plenary of the 2016 People in Disasters Conference. Johnston is a Senior Scientist at GNS Science and Director of the Joint Centre for Disaster Research in the School of Psychology at Massey University. The presentation is titled, "Understanding Immediate Human Behaviour to the 2010-2011 Canterbury Earthquake Sequence, Implications for injury prevention and risk communication".The abstract for the presentation reads as follows: The 2010 and 2011 Canterbury earthquake sequences have given us a unique opportunity to better understand human behaviour during and immediately after an earthquake. On 4 September 2010, a magnitude 7.1 earthquake occurred near Darfield in the Canterbury region of New Zealand. There were no deaths, but several thousand people sustained injuries and sought medical assistance. Less than 6 months later, a magnitude 6.2 earthquake occurred under Christchurch City at 12:51 p.m. on 22 February 2011. A total of 182 people were killed in the first 24 hours and over 7,000 people injured overall. To reduce earthquake casualties in future events, it is important to understand how people behaved during and immediately after the shaking, and how their behaviour exposed them to risk of death or injury. Most previous studies have relied on an analysis of medical records and/or reflective interviews and questionnaire studies. In Canterbury we were able to combine a range of methods to explore earthquake shaking behaviours and the causes of injuries. In New Zealand, the Accident Compensation Corporation (a national health payment scheme run by the government) allowed researchers to access injury data from over 9,500 people from the Darfield (4 September 2010) and Christchurch (22 February 2011 ) earthquakes. The total injury burden was analysed for demography, context of injury, causes of injury, and injury type. From the injury data inferences into human behaviour were derived. We were able to classify the injury context as direct (immediate shaking of the primary earthquake or aftershocks causing unavoidable injuries), and secondary (cause of injury after shaking ceased). A second study examined people's immediate responses to earthquakes in Christchurch New Zealand and compared responses to the 2011 earthquake in Hitachi, Japan. A further study has developed a systematic process and coding scheme to analyse earthquake video footage of human behaviour during strong earthquake shaking. From these studies a number of recommendations for injury prevention and risk communication can be made. In general, improved building codes, strengthening buildings, and securing fittings will reduce future earthquake deaths and injuries. However, the high rate of injuries incurred from undertaking an inappropriate action (e.g. moving around) during or immediately after an earthquake suggests that further education is needed to promote appropriate actions during and after earthquakes. In New Zealand - as in US and worldwide - public education efforts such as the 'Shakeout' exercise are trying to address the behavioural aspects of injury prevention.