Cracks along the road in Avonside Drive. The riverbank has slumped towards the river, separating the land from the road and creating these cracks. Road cones warn drivers of the uneven surface. In the distance, a pile of liquefaction can be seen in front of a house.
A photograph of the earthquake damage to the curb of a street in Christchurch. The curb has cracked in two places and slumped, exposing the earth beneath the grass turf.
When the destructive February earthquake hit Christchurch, one of our reporters, Bridget Mills, was recording an interview at the very moment the earth started shaking.
When the destructive February earthquake hit Christchurch, one of our reporters, Bridget Mills, was recording an interview at the very moment the earth started shaking.
Photograph captioned by BeckerFraserPhotos, "The Avon River is at this point on Avonside Drive 10 km from the estuary. At high tide the river now overflows its banks showing that the ground has sunk by about 40 cm".
Photograph captioned by Fairfax, "Locksley Avenue houses in Dallington. Owen Moore, aged 90, and dog Min laugh in the face of this afternoon's aftershock. His house was built on compacted earth alongside the Avon River".
Photograph captioned by Fairfax, "Locksley Avenue houses in Dallington. Owen Moore, aged 90, and dog Min laugh in the face of this afternoon's aftershock. His house was built on compacted earth alongside the Avon River".
Photograph captioned by BeckerFraserPhotos, "The Avon River is at this point on Avonside Drive 10 km from the estuary. At high tide the river now overflows its banks showing that the ground has sunk by about 40 cm".
A photograph captioned by BeckerFraserPhotos, "A section of Avonside Drive shows how the infrastructure is no longer maintained to the same level, with regard to roading, sewage and water services. The houses behind show the crazy angles that the earth movement has left them at".
A digitally manipulated image of a sign reading "A bit of dirt never hurt". The photographer comments, "This was a sign put up on a section of land in the Port of Lyttelton where an earthquake damaged building had been removed. The cliff at the back had collapsed down probably during the demolition process".
When the magnitude-7.8 earthquake shook North Canterbury nearly three years ago, a 3.5-metre high wall of earth formed on Dave and Rebekah Kelly's sheep and beef station. The 'Wall of Waiau' – as it's now known – sits on a faultline that cuts across a scenic hillside.
This is the pedestrian bridge in Kaiapoi close to Christchurch. Not the best angle but the whole bridge on the right hand side is twisted and looks like some kind of rollercoaster. Taken one month after the Quake Twitter |
There are quite a few signs like this around Christchurch after the Quake. This is one of them. Off shot to the right is a leveled patch of ground where the owners furniture restoration shop used to be. Twitter |
Anyone keeping a global tally of recent disasters is likely to be asking: What role will the hazards and disasters of coastal plains play in the lives and economies of 21st century humanity? In this article, we reflect on this question using examples of how different types of coastal land performed during the Christchurch and other earthquake events to examine the complex of coastal-tectonic hazards that are being constructed in the Tokyo megacity
A photograph of road works on a residential street in Christchurch. Two workers in high-visibility vests can be seen, one setting up road cones. A digger is sitting on a pile of dug up gravel and earth. Cordon fences have been placed around the site. In the distance, a dump truck can be seen.
Barbadoes St
Barbadoes St
Fitzgerald Ave
Fitzgerald Panorama
Suburbs
Suburbs
Our Garage
Fitzgerald Ave
Avon River
Fitzgerald Ave
Barbadoes St
Fitzgerald Ave
Fitzgerald Ave
Fitzgerald Ave
A digitally manipulated photograph of twisted reinforcing rods amongst the rubble from the demolition of QEII. The photographer comments, "These rarely seen worms live in the pressurised earth under the foundations of buildings. They need a damp soil and be under at least 100 pounds of pressure per square inch. After the destructive force of an earthquake they swiftly rise to the surface through gaps in the rubble. Unfortunately they quickly die and then crystallise as hard as iron in the dry low pressure air".