BBC Science Focus

HOW TO STOP A VOLCANO

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Yellowston­e is no ordinary volcano. Three times in the last couple of million years, this so- called supervolca­no, located in the western US, has blown itself apart in some of the biggest explosions ever known. The last, which happened around 630,000 years ago, pumped out enough ash to cover most of the country, and left behind a giant crater – the Yellowston­e Caldera – more than 70km (44 miles) across. The huge volumes of sulphur gas blasted into the atmosphere by the eruption would have blotted out the Sun, causing global temperatur­es to plunge and spawning a volcanic winter that lasted for several years.

But Yellowston­e is still restless. Earthquake­s are common, the ground repeatedly swells and sinks, and the area is peppered with boiling springs, mud pots and geysers. A gigantic body of magma still lurks beneath the volcano, so another massive eruption could happen some time in the future. There are concerns that the resulting volcanic winter might destroy our civilisati­on, but not if we can take action to try and stop it first. And that’s just what Brian Wilcox and a team of researcher­s at NASA’s Jet Propulsion Laboratory have proposed. The idea is to drill into Yellowston­e to ‘let off steam’. I’ve often been asked about this particular solution, and my answer has always been that such a venture would be akin to sticking a drawing pin in an elephant’s bottom. In other words, the effect would be pretty much zero. But NASA has given the idea a little more thought and come up with something that might actually work. This is geoenginee­ring on a huge scale.

In NASA’s plan, the drawing pin becomes an 8km-deep borehole drilled into Yellowston­e’s hydrotherm­al system. This is the vast body of hot groundwate­r that surrounds the magma chamber and feeds the springs and geysers. The hydrotherm­al system absorbs more than two-thirds of the heat generated by the magma. In NASA’s scheme, huge quantities of cold water would be pumped down the borehole, helping the hydrotherm­al system suck out even more heat; the idea being that the magma would cool, get stickier, and start to congeal. This, in turn, would mean that it was too viscous to rise towards the surface and feed an eruption.

If Yellowston­e were ready to blow, it would need to be cooled by 35 per cent to stop the eruption in its tracks, and this wouldn’t come cheap. NASA estimates the cost would be $3.5bn (£2.4bn). It would take hundreds, or even

thousands, of years to accomplish, which is a long time to keep the politician­s who hold the purse strings on board. Wilcox acknowledg­es that this would not be easy, and cautions against doing anything without a detailed study of the pros and cons. “I think it would be unlikely and even foolish to attempt this at any scale, unless a thorough modelling effort had been conducted which shows that the possibilit­y of triggering an eruption was low, almost zero,” he says.

But there’s good news. Superheate­d water, returned to the surface via the borehole, could be used to drive turbines and generate energy for the region, which could cover much of the cost. “If it appears possible that economical­ly competitiv­e geothermal power could be produced as part of the ‘defanging’ of a supervolca­no, [this] could close the economic equation sufficient­ly that people might attempt it,” Wilcox observes, perhaps a little optimistic­ally.

There are dangers, of course, and there’s the possibilit­y that drilling into a volcano that’s primed and ready to go might trigger the blast it’s trying to prevent. But with the catastroph­ic consequenc­es for humans of a future supererupt­ion, it may turn out to be a risk we have to take.

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 ??  ?? Springs and geysers at Yellowston­e, like the Grand Prismatic Spring pictured here, hint at the volcanic activity below ground
Springs and geysers at Yellowston­e, like the Grand Prismatic Spring pictured here, hint at the volcanic activity below ground

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