BeckerFraserPhotos October 2010 photograph 002

Images, UC QuakeStudies

New re-locatable classrooms being readied for use at Halswell School.

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Images, UC QuakeStudies

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.

BeckerFraserPhotos September 2010 photograph 094

Images, UC QuakeStudies

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.

BeckerFraserPhotos September 2010 photograph 092

Images, UC QuakeStudies

A gap between two walls at Halswell Primary School. The gap was caused by two buildings separating during the 4 September earthquake.

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Images, UC QuakeStudies

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.

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Images, UC QuakeStudies

Tape reading, "Danger Keep Out" on the gate to Halswell Primary School. A sign has been stabled to the tape reading, "No unauthorised entry".

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Images, UC QuakeStudies

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.

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Images, UC QuakeStudies

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.

BeckerFraserPhotos September 2010 photograph 093

Images, UC QuakeStudies

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.

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Images, UC QuakeStudies

Broken pavement in the Halswell Primary School grounds. Silt from liquefaction can also be seen.

Ray Whelan WEMO Photograph 36

Images, UC QuakeStudies

A photograph of large cracks in the pavement in front of St Paul's School in Dallington.

BeckerFraserPhotos October 2010 photograph 001

Images, UC QuakeStudies

One of several containers now on the Halswell School grounds while reconstruction takes place.

Ray Whelan WEMO Photograph 38

Images, UC QuakeStudies

A photograph of large cracks in the pavement in front of St Paul's School in Dallington. Liquefaction silt can also be seen. Police tape has been draped across the entrance of the building to the left.

Nic Johns and Mark Osborne WEMO Photograph 104

Images, UC QuakeStudies

A photograph of displaced bricks in one of the walls of St Paul's School on Gayhurst Road.

Deb Robertson's Blog 24/09/2010: Let the wild rumpus, I mean the school ho…

Articles, UC QuakeStudies

An entry from Deb Robertson's blog for 24 September 2010 entitled, "Let the wild rumpus, I mean the school holidays begin...".

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Images, UC QuakeStudies

Road damage between St Paul's School and Gayhurst Road bridge. The road has slumped near the curb, probably due to liquefaction.

Nic Johns and Mark Osborne WEMO Photograph 105

Images, UC QuakeStudies

A photograph of volunteers from the Wellington Emergency Management Office standing outside St Paul's School on Gayhurst Road. There are cracks in the asphalt in front, and liquefaction on the ground.