Mud volcano to stop 'by decade's end'

Lusi vent Despite the disruption it has brought to the region, the mud volcano has become a tourist attraction

Related Stories

Scientists say the eruption of the Lusi mud volcano in Indonesia should be all but over by the end of the decade - much sooner than previous estimates.

The assessment is based on satellite data that records the rate at which the ground is changing in response to the material spewing up on to the surface.

Researchers say the system is losing pressure rapidly.

The eruption, which began in the Porong subdistrict of Sidoarjo in East Java in 2006, is the largest of its kind.

The gooey, noxious muck has displaced tens of thousands of people with economic costs that exceed $4bn to date.

Initially, more than 100,000 tonnes a day was oozing to the surface. This has decreased tenfold, and an analysis based on Japanese satellite observations of ground subsidence suggests a further tenfold decrease can be expected in the next few years.

"By 2017, it should be more or less over," said Prof Michael Manga from the University of California at Berkeley, US.

"In real numbers, that's 1,000 tonnes a day - a thousand pick-up trucks per day of mud. Small enough that it won't be a hazard, [but] maybe interesting enough still to be a tourist destination," he told BBC News.

"I expect [then] that if the eruption rate drops below some number, that it will just plug itself and stop erupting."

Previous best estimates had indicated Lusi could go on erupting for 25 years or more.

Prof Manga was speaking here in San Francisco at the American Geophysical Union (AGU) Fall Meeting, the world's largest annual gathering of Earth scientists.

He and colleagues have used a technique known as interferometric synthetic aperture radar (InSAR) to assess the evolution of the eruption.

This involved combining a series of repeat images of the volcano acquired from space by Japan's ALOS satellite to measure ground surface height changes around the volcano.

Over the course of several years, the surrounding land is recorded falling tens of centimetres as a result of material deep in the Earth being driven up and out on to the surface. However, the rate of subsidence has declined dramatically, indicating Lusi is losing its vigour.

Map showing Indonesian island of Java (Image: BBC)

And this is reflected in the changed behaviour that can be observed at the surface.

"There isn't a constant eruption there anymore; it's actually pulsing now," said Prof Richard Davies from Durham University, UK. "And that pulsing is a very good sign that the pressure itself has dropped off. What's driving the eruption now is a burping from all the gas that's coming up.

"The gas makes it behave like a geyser, almost - a bit like Old Faithful in Yellowstone National Park. You can almost set your watch by these pulses."

Controversy still surrounds the cause of Lusi. Some scientists suspect it was triggered by a nearby drilling operation that went wrong. Other researchers, however, argue that an earthquake two days prior to the mud volcano's appearance was responsible.

Prof Manga cautions that there will always be some uncertainty about the future course of the eruption, and any forecast is made on the assumption that the system continues to behave in the same way it has in the past. But he adds that the latest evidence ought to be more encouraging for those who live in the region.

"In the scientific literature, for this particular eruption, there are three fundamentally different models for where the mud is coming from, where the flow is coming from, and what's happening," he told BBC News.

"So, even though we have great data available, it's not clear yet whether we understand exactly how this eruption works.

"But with the data we have and the data we will collect in the future, I'm sure we're going to learn more."

Finger points to Lusi vent At some point the eruption rate should fall to a point where the Earth simply plugs itself

This posting was modified from its original form to emphasise that there are alternative models for the eruption's cause. and follow me on Twitter: @BBCAmos

More on This Story

Related Stories

The BBC is not responsible for the content of external Internet sites

More Science & Environment stories



Copyright © 2019 BBC. The BBC is not responsible for the content of external sites. Read more.

This page is best viewed in an up-to-date web browser with style sheets (CSS) enabled. While you will be able to view the content of this page in your current browser, you will not be able to get the full visual experience. Please consider upgrading your browser software or enabling style sheets (CSS) if you are able to do so.