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Images for Soil liquefaction; more images...
Grant Wilson Liquefaction Photograph 039
Images, UC QuakeStudies
A photograph of liquefaction and water-logged soil near Anzac Drive in Bexley.
Grant Wilson Liquefaction Photograph 042
Images, UC QuakeStudies
A photograph of liquefaction and water-logged soil near Anzac Drive in Bexley.
Grant Wilson Liquefaction Photograph 043
Images, UC QuakeStudies
A photograph of liquefaction and water-logged soil near Anzac Drive in Bexley.
Grant Wilson Liquefaction Photograph 040
Images, UC QuakeStudies
A photograph of liquefaction and water-logged soil near Anzac Drive in Bexley.
Natalie Kerschner WEMO Photograph 114
Images, UC QuakeStudies
A photograph of a silt volcano. Silt volcanoes are caused by liquefaction, when the soil loses its strength during the earthquake and the silt rises upwards, ejecting out of a hole like magma in a volcano.
Sonja Farmer Photograph 58
Images, UC QuakeStudies
A photograph of a crack in the pavement of a residential street in Christchurch. The crack was caused by liquefaction erupting out of the soil underneath.
BeckerFraserPhotos June 2011 photograph 335
Images, UC QuakeStudies
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.
BeckerFraserPhotos June 2011 photograph 334
Images, UC QuakeStudies
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.
BeckerFraserPhotos June 2011 photograph 338
Images, UC QuakeStudies
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.
BeckerFraserPhotos June 2011 photograph 339
Images, UC QuakeStudies
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.
BeckerFraserPhotos June 2011 photograph 333
Images, UC QuakeStudies
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.
BeckerFraserPhotos June 2011 photograph 332
Images, UC QuakeStudies
A "sand volcano" in the Heathcote Estuary. The volcano was caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
BeckerFraserPhotos October 2010 photograph 003
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.
Farmland Rehabilitation Photograph 21
Images, UC QuakeStudies
A photograph of liquefaction emerging from freshly-harrowed soil on a farm near River Road in Lincoln.
Farmland Rehabilitation Photograph 22
Images, UC QuakeStudies
A photograph of liquefaction emerging from freshly-harrowed soil on a farm near River Road in Lincoln.
Farmland Rehabilitation Photograph 24
Images, UC QuakeStudies
A photograph of liquefaction emerging from freshly-harrowed soil on a farm near River Road in Lincoln.
Farmland Rehabilitation Photograph 23
Images, UC QuakeStudies
A photograph of liquefaction emerging from freshly-harrowed soil on a farm near River Road in Lincoln.
BeckerFraserPhotos June 2011 photograph 337
Images, UC QuakeStudies
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.
Photograph by Neil Macbeth 055
Images, UC QuakeStudies
People walking amongst silt in Hagley Park shortly after the 22 February 2011 earthquake. These silt deposits were caused by the soil liquefying during the 22 February 2011 earthquake. The water flowed out, bringing sand with it.
Photograph by Neil Macbeth 056
Images, UC QuakeStudies
People walking amongst silt in Hagley Park shortly after the 22 February 2011 earthquake. These silt deposits were caused by the soil liquefying during the 22 February 2011 earthquake. The water flowed out, bringing sand with it.
Farmland Rehabilitation Video 05
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is pulling a power harrow over a liquefaction blister. This was one of several soil-remediation techniques tested on farms affected by the 4 September 2010 earthquake.
Farmland Rehabilitation Video 04
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is pulling a power harrow over a liquefaction blister. This was one of several soil-remediation techniques tested on farms affected by the 4 September 2010 earthquake.
Farmland Rehabilitation Video 10
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is making several passes over a liquefaction blister with a rotary hoe. This was one of several soil-remediation techniques tested on farms affected by the 4 September 2010 earthquake.
Farmland Rehabilitation Video 06
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is making a second pass over a liquefaction blister with a power harrow. This was one of several soil-remediation techniques tested on farms affected by the 4 September 2010 earthquake.
BeckerFraserPhotos September 2010 photograph 090
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 088
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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