On 28 September 2018, a shallow, large earthquake struck in the neck of the Minahasa Peninsula, Indonesia, with its epicentre located in the mountainous Donggala Regency, Central Sulawesi. The magnitu
The village of Petobo after the earthquake.
Locations of earthquakes and surface traces of main faults near the epicentre. The Palu-Koro fault is shown as two disconnected red lines indicated by arrows.
Shakemap of the 2018 Sulawesi earthquake
President Joko Widodo viewing collapsed buildings in Palu
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
2018 Sulawesi earthquake and tsunami
…an estimated maximum of 4 to 7 metres (13 to 23 ft), striking the settlements of Palu, Donggala and Mamuju along its path. The earthquake caused major soil liquefaction in areas in and around Palu. In two locations this led to mudflows in which many buildings became submerged causing hundreds of deaths with many more…
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.