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Farmland Rehabilitation Photograph 16
Images, UC QuakeStudies
A photograph of a dug-out soil pit on a farm near River Road in Lincoln, showing saturated sand between the topsoil and the subsoil where the grass roots end.
Farmland Rehabilitation Photograph 04
Images, UC QuakeStudies
A photograph of a dug-out soil pit on a farm near River Road in Lincoln, showing saturated sand between the topsoil and the subsoil where the grass roots end.
This is an Earthquake Not a Wide Angle Shot
Images, UC QuakeStudies
A badly damaged house in Burwood. Parts of the house have moved in different directions, leaving walls and doors misaligned. The photographer comments, "Although this looks like an extreme wide angle shot it is actually a house tilted in every direction at the same time. The earthquake caused the ground to vibrate and compress so much that the sandy soil liquefied and caused the ground to collapse under this modern home".
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.
Farmland Rehabilitation Photograph 13
Images, UC QuakeStudies
A photograph of Peter Almond (wearing high visibility jacket), Derrick Moot and contractor Tony Fisher of Fisher Agricultural Ltd. inspecting a dug-out soil pit on a farm near River Road in Lincoln.
Sunday is a Day of Rest
Images, UC QuakeStudies
The head of a digger resting on a pile of soil next to QEII Stadium. The photographer comments, "The deconstruction of the QEII stadium in Christchurch pauses on a Sunday".
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.
Access All Areas
Images, UC QuakeStudies
A digitally manipulated image of the head of a digger resting on a pile of soil. The photographer comments, "You can go anywhere you like when you are a rock star".
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 12
Images, UC QuakeStudies
A photograph of Professor Derrick Moot inspecting a dug-out soil pit on a farm near River Road in Lincoln. There is a thick layer of saturated sand between the topsoil and the subsoil where the grass roots end.
Farmland Rehabilitation Photograph 11
Images, UC QuakeStudies
A photograph of Professor Derrick Moot inspecting a dug-out soil pit on a farm near River Road in Lincoln. There is a thick layer of saturated sand between the topsoil and the subsoil where the grass roots end.
Farmland Rehabilitation Photograph 10
Images, UC QuakeStudies
A photograph of Professor Derrick Moot inspecting a dug-out soil pit on a farm near River Road in Lincoln. There is a thick layer of saturated sand between the topsoil and the subsoil where the grass roots end.
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.
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.
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.
Farmland Rehabilitation Photograph 06
Images, UC QuakeStudies
A photograph of contractor Tony Fisher of Fisher Agricultural Ltd. inspecting a dug-out soil pit on a farm near River Road in Lincoln. There is a thick layer of saturated sand between the topsoil and the subsoil where the grass roots end.
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.
Embassy Science Fellowship Program Focuses on Earthquake Research
Articles, UC QuakeStudies
A blog post from US Ambassador to New Zealand and Samoa, David Huebner, titled, "Embassy Science Fellowship Program Focuses on Earthquake Research".
Farmland Rehabilitation Video 07
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is making a several passes over a sand volcano 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 09
Videos, UC QuakeStudies
A video of a tractor on a farm near River Road in Lincoln. The tractor is passing over a large sand volcano 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.
Terra Probe
Images, UC QuakeStudies
Workers operate a drilling rig inside a Terra Probe truck, which has been raised on jacks to make it stable. The photographer comments, "Another completely different company testing what is below the surface to determine what type of foundations new houses will need. This is in one the blue/green area of earthquake shaken Christchurch. Strangely this is 3 metres away from where the other testing was done".
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.