(Reuters) - Liquefied soil caused numerous buildings to collapse in the Indonesian city of Palu after Friday’s magnitude 7.5 earthquake, which has killed more than 800 people.
Here’s a brief explanation of liquefaction, how common it is, and where it is likely to happen.
Liquefaction is a phenomenon where saturated sand and silt take on the characteristics of a liquid during the intense shaking of an earthquake, according to the United States Geological Survey website.
It takes place when a quake has increased water pressure in saturated soil and made particles in the soil lose contact with each other, making the soil - particularly sandy soil - act like liquid.
The effect has been likened to slapping a wet, hard beach and the sand beneath your palm becomes jelly.
In the Palu neighborhood of Balaroa, about 1,700 houses were swallowed up when the earthquake caused soil to liquefy, the national rescue agency said.
Satellite images of the Petobo district, south of Palu’s airport, showed another large area of urban development seemingly wiped clear of buildings.
“When the quake hit, the layers below the surface of the earth became muddy and loose,” said Sutopo Purwo Nugroho, spokesman of Indonesia’s national disaster mitigation agency.
“Mud with such large mass volume drowned and dragged the housing complex in Petobo so that most of them became as if they were absorbed. We estimate 744 units of houses are there.”
Amateur video footage appeared to show trees, buildings and even a large communications tower being tossed around in fast-moving landslides. Reuters was unable to verify the footage.
Among those killed were 34 children at a Christian bible study camp that was hit by liquefaction, a Red Cross official said.
GRAPHIC: Catastrophe in Sulawesi - tmsnrt.rs/2OqQlUo
Liquefaction is most likely to happen in reclaimed land. Areas with shallow water tables and close to the sea or rivers are also susceptible to liquefaction.
“Compared with what’s been formed naturally over a long period of time, what’s manmade has been constructed for a short period of time, where soil particles are only loosely connected to each other,” said Toshitaka Kamai, professor at Kyoto University’s Disaster Prevention Research Institute.
The eastern Japanese city of Urayasu, where the majority of land was formed by reclamation, saw 86 percent of its land affected by liquefaction following the massive 2011 earthquake. It took the city six years to repair all the damaged underground sewerage, water and gas facilities.
“It renders underground pipes mangled mess. One of its characteristics is it takes time to recover (from liquefaction damage),” Yoshiharu Yokoyama, an executive at Jibannet Co Ltd, which provides soil analysis services.
Conditions that could lead to liquefaction can be found in many places in Indonesia and throughout Asia, said Mark Quigley, Associate Professor of Earthquake Science at the University of Melbourne.
“People need to live in places that are habitable for a whole bunch of reasons. In the case of Palu it’s on a very nice, natural bay. It’s on a river that would have provided historically a source of water for them. There’s a lot of really mountainous jungle-y terrain all around it, it’s not like they had endless opportunity to just choose whatever site they wanted.”
Earthquake and soil experts say liquefaction is fairly common. It happened after the massive 9.0 magnitude quake that hit eastern Japan in 2011 and numerous other Japanese earthquakes in recent years.
It has also been reported in several previous Indonesian earthquakes, major quakes in Christchurch, New Zealand in 2010 and 2011, and the Great Alaska Earthquake of 1964.
Reporting by Linda Sieg, Malcolm Foster, Kiyoshi Takenaka in TOKYO, Gayatri Suroyo in JAKARTA, Charlotte Greenfield in WELLINGTON.; Editing by Lincoln Feast.