A photograph of a spray-painted message on a fence reading, "4 sale - handy mans dream. Mild reno's needed. Easy indoor/outdoor flow - with water feature!" The photograph is captioned by Paul Corliss, "New Brighton by QEII Drive".
A photograph of a spray-painted message on a fence reading, "4 sale - handy mans dream. Mild reno's needed. Easy indoor/outdoor flow - with water feature!" The photograph is captioned by Paul Corliss, "New Brighton by QEII Drive".
A photograph of a spray-painted message on a fence reading, "4 sale - handy mans dream. Mild reno's needed. Easy indoor/outdoor flow - with water feature!" The photograph is captioned by Paul Corliss, "New Brighton by QEII Drive".
None
This one was really flowing out of the ground.
A photograph of members of the Wellington Emergency Management Office Emergency Response Team inside a building in the Christchurch central city. Silt and water from liquefaction has covered large sections of the concrete floor.
Photograph captioned by BeckerFraserPhotos, "Mounds of demolition debris at the site of the Copthorne Durham on the corner of Durham and Kilmore Streets being sprayed with water to keep the dust down".
Photograph captioned by BeckerFraserPhotos, "Waygreen Avenue in New Brighton. This residential street was badly impacted by liquefaction and is now red zoned. Stagnant water still rests in several places in the street".
Sullivan Park in Avonside. Liquefaction can be seen running across the park. Two signs have slumped towards each other. Blue pipes carrying a temporary water supply to the neighbourhood have been placed across the park.
Paradise ducks search for food among 'sand volcanoes' in the Heathcote Estuary. The volcanoes were caused by liquefaction where the soil lost its strength and water erupted out of the hole, taking silt with it.
A photograph captioned by BeckerFraserPhotos, "A photograph of a residential property on River Road in Richmond. In the garden is a pipe which is being used to supply water to the property temporarily".
A photograph of members of the Wellington Emergency Management Office examining the car park in the basement of the Copthorne Hotel. The car park has flooded, and water has risen to where they are standing.
A copy of a letter from Hugo Kristinsson which was sent to Helen Beaumont, Manager of the Natural Environment and Heritage Unit at the Christchurch City Council, on 17 June 2014. The letter was sent on behalf of Empowered Christchurch. It is about legislation which, according to Kristinsson, determines land below the mean high water spring to be public land. Kristinsson is concerned that this legislation will cause 'hundred or even thousands' of people to lose their assets. He urges the Council to 'have the land surveyed and to redefine the CMA [Crown Minerals Act] before land claims are settled'.
A view over the top of a cordon fence. A digger sits on a mound of dirt, and water fills the former basement of the ANZ building on Hereford Street. The partially-demolished BNZ building can be seen in the background.
None
These were scattered across the park.
Robbie watches a sand volcano smother his driveway.
A photograph of street art on a building in New Brighton. The artwork includes the phrases "No one is superior, everyone is special", "Occupy Equality Street", and "Love is the child of freedom".
Results from a series of 1D seismic effective stress analyses of natural soil deposits from Christchurch are summarized. The analysed soil columns include sites whose performance during the 2010-2011 Canterbury earthquakes varied significantly, from no liquefaction manifestation at the ground surface to very severe liquefaction, in which case a large area of the site was covered by thick soil ejecta. Key soil profile characteristics and response mechanisms affecting the severity of surface liquefaction manifestation and subsequent damage are explored. The influence of shaking intensity on the triggering and contribution of these mechanisms is also discussed. Careful examination of the results highlights the importance of considering the deposit as a whole, i.e. a system of layers, including interactions between layers in the dynamic response and through pore water pressure redistribution and water flow.
Photograph captioned by BeckerFraserPhotos, "Waygreen Avenue in New Brighton. The homeowners at the end of this drive are staying here until their new homes are available. The stagnant water on their drive is full of algae".
A photograph of street art on the side of the Couplands Bakery on Hawke Street in New Brighton. The artwork includes the tag "Aroha" and a painting of a man and a young child playing in the water.
Study region: Christchurch, New Zealand. Study focus: Low-lying coastal cities worldwide are vulnerable to shallow groundwater salinization caused by saltwater intrusion and anthropogenic activities. Shallow groundwater salinization can have cascading negative impacts on municipal assets, but this is rarely considered compared to impacts of salinization on water supply. Here, shallow groundwater salinity was sampled at high spatial resolution (1.3 piezometer/km²), then mapped and spatially interpolated. This was possible due to a uniquely extensive set of shallow piezometers installed in response to the 2010–11 Canterbury Earthquake Sequence to assess liquefaction risk. The municipal assets located within the brackish groundwater areas were highlighted. New hydrological insights for the region: Brackish groundwater areas were centred on a spit of coastal sand dunes and inside the meander of a tidal river with poorly drained soils. The municipal assets located within these areas include: (i) wastewater and stormwater pipes constructed from steel-reinforced concrete, which, if damaged, are vulnerable to premature failure when exposed to chloride underwater, and (ii) 41 parks and reserves totalling 236 ha, within which salt-intolerant groundwater-dependent species are at risk. This research highlights the importance of determining areas of saline shallow groundwater in low-lying coastal urban settings and the co-located municipal assets to allow the prioritisation of sites for future monitoring and management.
A photograph of the earthquake damage to a property in the Christchurch central city. Part of the roof of the property has collapsed, spilling material onto the balcony below. A sign in the foreground reads, "Wots your councillor doing for your water?".
Water has swept grit and splinters of wood onto the footpath outside the Durham Street Methodist Church. In the background of the photograph a piece of one of the church's roof beams with its steel brace can be seen.
Trees alongside the Avon River in Richmond. The river level is high, and the water is grey with silt. One of the trees is leaning towards the river. The photographer comments, "High river levels because of liquefaction in the Avon. Near 373 River Rd, Richmond".
Sand volcanoes put the silt all over the road.
The earthquake knocked over the bird bath.
Debra points at the beginnings of a sand volcano not long after the big earthquake.
An usual thing to see coming from the ground in Hoon Hay, Christchurch.
A PDF copy of a fact sheet about hydraulic fracturing (fracking) in the South Island created by Anglican Advocacy in 2011. The fact sheet contains information about the possible impacts of fracking on water and the risk of earthquakes.