
A photograph of a garage which has sunk into liquefaction on one side. The photograph is captioned by BeckerFraserPhotos, "New Brighton Road".
A photograph of several earthquake-damaged houses on Chester Street East. A pile of liquefaction silt is on the footpath in the foreground.
A photograph of a hole in the footpath outside St Paul's Church where liquefaction has forced its way up.
Part of the forecourt at the Shell Shirley petrol station has lifted above the rest, after the underground petrol tanks were pushed upwards by liquefaction. Liquefaction silt covers the lower part of the forecourt.
A photograph of a garage which has sunk into liquefaction on one side. The photograph is captioned by BeckerFraserPhotos, "New Brighton Road".
A photograph captioned by BeckerFraserPhotos, "The rear of 14 Waygreen Avenue showing liquefaction nearly a metre deep around the clothes line".
A photograph captioned by BeckerFraserPhotos, "The rear of 14 Waygreen Avenue showing liquefaction nearly a metre deep around the clothes line".
A photograph captioned by BeckerFraserPhotos, "Road cones mark two mounds of liquefaction at Liggins Street in the Horseshoe Lake area".
A photograph of a damaged residential property at Seabreeze Close in Bexley. The yard is covered with weeds and silt from liquefaction.
On February 22, 2011, a magnitude Mw 6.2 earthquake affected the Canterbury region, New Zealand, resulting in many fatalities. Liquefaction occurred across many areas, visible on the surface as ‘‘sand volcanoes’’, blisters and subsidence, causing significant damage to buildings, land and infrastructure. Liquefaction occurred at a number of sites across the Christchurch Boys High School sports grounds; one area in particular contained a piston ground failure and an adjacent silt volcano. Here, as part of a class project, we apply near-surface geophysics to image these two liquefaction features and determine whether they share a subsurface connection. Hand auger results enable correlation of the geophysical responses with the subsurface stratigraphy. The survey results suggest that there is a subsurface link, likely via a paleo-stream channel. The anomalous responses of the horizontal loop electromagnetic survey and electrical resistivity imaging highlight the disruption of the subsurface electrical properties beneath and between the two liquefaction features. The vertical magnetic gradient may also show a subtle anomalous response in this area, however the results are inconclusive. The ground penetrating radar survey shows disruption of the subsurface stratigraphy beneath the liquefaction features, in particular sediment mounding beneath the silt ejection (‘‘silt volcano’’) and stratigraphic disruption beneath the piston failure. The results indicate how near-surface geophysics allow the characteristics of liquefaction in the subsurface to be better understood, which could aid remediation work following liquefaction-induced land damage and guide interpretation of geophysical surveys of paleoliquefaction features.
A photograph of police and members of the public people standing near the earthquake damaged Smiths City car park after the 22 February 2011 earthquake. Liquefaction covers the right side of the footpath.
Corcoron French Lawyers on Williams Street in Kaiapoi. Liquefaction has caused the building to sink on the right side. This is shown by the fence which now sits at an angle.
Students from the University of Canterbury lining up for a barbeque lunch. The students have volunteered to dig up liquefaction as part of the Student Volunteer Army.
Students from the University of Canterbury lining up for a barbeque lunch. The students have volunteered to dig up liquefaction as part of the Student Volunteer Army.
Students from the University of Canterbury lining up for a barbeque lunch. The students have volunteered to dig up liquefaction as part of the Student Volunteer Army.
A member of the Student Volunteer Army heading home with his shovel on his shoulder after spending a day clearing liquefaction from Christchurch properties.
Students from the University of Canterbury lining up for a barbeque lunch. The students have volunteered to dig up liquefaction as part of the Student Volunteer Army.
Students from the University of Canterbury lining up for a barbeque lunch. The students have volunteered to dig up liquefaction as part of the Student Volunteer Army.
Students from the University of Canterbury returning to Burwood Park after a day of clearing liquefaction from Christchurch properties as part of the Student Volunteer Army.
Students from the University of Canterbury returning to Burwood Park after a day of clearing liquefaction from Christchurch properties as part of the Student Volunteer Army.
Students from the University of Canterbury returning to Burwood Park after a day of clearing liquefaction from Christchurch properties as part of the Student Volunteer Army.
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 of police and members of the public people standing near the earthquake damaged Smiths Citys car park after the 22 February 2011 earthquake. Liquefaction covers the right side of the footpath.
A photograph captioned by BeckerFraserPhotos, "A damaged residential property at Seabreeze Close in Bexley. The yard is covered with weeds and silt from liquefaction".
Photograph captioned by BeckerFraserPhotos, "Subsidence under the New Brighton Road electrical substation, a result of the extensive liquefaction in the eastern suburbs".
Building rubble and liquefaction on the footpath outside the former Public Library on the corner of Hereford Street and Cambridge Terrace.
A photograph of a felled tree, liquefaction, and flooding in a residential street in Christchurch. Road cones have been placed around hazards to warn road and footpath users.
Photograph captioned by BeckerFraserPhotos, "23 Seabreeze Close, Bexley. The view through the window shows how much liquefaction collected in the garage".
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.
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.