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Images, UC QuakeStudies

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

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Images, UC QuakeStudies

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

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Images, UC QuakeStudies

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

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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

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

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.

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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

A private driveway in Halswell Junction Road with cracking in the concrete.

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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.

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Images, UC QuakeStudies

A footpath in Halswell where the pavement has cracked and uplifted due to liquefaction.

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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

A private driveway off Halswell Road with extensive cracking. The driveway has slumped into the creek due to liquefaction from the earthquake.

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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.

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Images, UC QuakeStudies

Cracks along the edge of Halswell Road. The footpath has slumped towards the creek on the left due to liquefaction, causing the crack in the road.

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Images, UC QuakeStudies

Road cones along the side of Halswell Road where the road has been repaired and sealed after slumping. There are still cracks in the footpath and curb.

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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 collapsed brick wall on Halswell Junction Road. A stack of bricks have been saved by the tree which has grown in a curve and is resting on the wall, holding the bricks in place. A pile of bricks can be seen on the ground where they fell.

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Images, UC QuakeStudies

A crack next to the Avon River caused by the ground slumping after the 4 September earthquake. A blue pipe has been laid over the crack. Many kilometres of these temporary water pipes have been run overground in Avonside to supply houses with water.

ELM Offices Level 7 Library - Photograph 14

Images, UC QuakeStudies

Members of the University of Canterbury's E-Learning team admire the view from their temporary office in the James Hight building. The photographer comments, "First looks at our new temporary (maybe) office space. Our group will stay here until April or May 2011, then will move to another floor in the Central Library. South window of our office. Our view looks out to the Port Hills and around to the south west, towards Halswell and Lincoln".