Gas drilling on the Indonesian island of Java has triggered what can be called a “mud volcano” that had killed around 13 people and has made four square miles (ten square kilometers) of countryside uninhabitable for years.
According to a recent report released, a team of British researchers says that the deadly upwelling began when an exploratory gas burst out through a rock of 9,300 feet (2,800 meters) below the ground, letting hot, high-pressure water to escape.
The water along with it carried mud to the surface, where it spread to a region of 2.5 miles (4 kilometers) in diameter in eight months since the eruption began. The mud volcano is similar to a gusher or blowout, which occurs in oil drilling when oil or gas squirt to the surface, according to the team.
Eventhough the eruption isn’t as violent as a typical volcano, around dozen people died in this event. The volcano also known as Lusi, will leave more than 11,000 people permanently displaced.
Human Reasons
Mud volcanoes are caused when pressures deep in the Earth cause the mud to squirt to the surface.
According to Richard Davies, lead author of the study:
“It’s simply an eruption of mud and liquids,” added Davies, who directs the Center for Research into Earth Energy Systems at Durham University. “There are probably a couple of thousand on planet Earth.”
Typically, the eruptions are caused by tectonic forces or by the compaction of sediments at the deltas of large rivers, such as the Mississippi. “They’re very common features,” Davies said.
But even though an earthquake had occurred in the Java region only two days prior to the eruption, the delayed mud release confirms a human cause.
Danger Continues
Another unusual feature of the Indonesian eruption is that it is a very thin, liquid mud, according to another researcher, Richard Swarbrick of Geopressure Technology Ltd. It is unfortunate that it is thin mud because this could flow for long distances, increasing the devastation and destruction.
Another concern is that the mud is getting eroded from deep underground, causing a cavern. This means that the land around the volcano might collapse to form a crater, Swarbrick said.
The duration of the volcano’s activity is of concern. Usually, mud volcanoes erupt quickly, and then become a slow ooze intermingled with the occasional major upwelling. But in Java the flow rate appears to have doubled since the eruption began, Swarbrick said.
At its center, the pancake-like deposit is already about 33 feet (10 meters) thick, Durham University’s Davies added. “It’s carried on for a long time at a high rate, which suggests it’s not going to stop tomorrow,” he said.