A major earthquake occurred in Christchurch on Tuesday 22 February 2011 at 12:51 p.m. local time. The Mw 6.2 earthquake struck the Canterbury Region in the South Island, centred 6.7 kilometres south-e
Damaged Catholic cathedral two months after the earthquake
Results of liquefaction; the fine washed-up sand solidifies after the water has run off
Liquefaction adjacent to the Avon River / Ōtākaro caused lateral spread in Fitzgerald Avenue, causing severe damage.
115 bodies were recovered from the CTV Building, which collapsed during the quake.
Soil liquefaction occurs when a cohesionless saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress such as shaking during an earthquake or o
2011 Christchurch earthquake
…were badly affected, with damage to buildings and infrastructure already weakened by the 2010 Canterbury earthquake and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was felt across the South Island and parts of the lower and central…
Some effects of soil liquefaction after the 1964 Niigata earthquake
Soil liquefaction allowed this sewer manhole to float upward and breach the pavement during the 2004 Chūetsu earthquake
Soil liquefaction in Christchurch. The 2011 earthquake caused a layer of water and fine sand to collect on the surface of this street.
The Giddy House in Port Royal, Jamaica, which partially sank into the ground during an earthquake in 1907 which produced soil liquefaction, resulting in its distinctive tilted appearance.