New Hazard Caused by Volcanic Eruptions Discovered

Research has identified, for the first time, a new type of hazard caused by explosive volcanic eruptions.

hazard
Scientists approach the broken, steaming ground around the Cordón Caulle vent, which was hugely uplifted during the 2011 eruption. Little of the slope seen behind the black lava flow would have been visible before the uplift occurred. Courtesy of Dr Hugh Tuffen.

It’s remarkable that such a large volume of magma was injected so close to the surface during an eruption. The magma is likely to remain hot for many years and could be reactivated, so hazard assessments must take this into account.

Dr Hugh Tuffen

 

The study, published in Nature Communications, found that the eruption of Cordón Caulle, Chile, in 2011 caused a large volume of magma – called a laccolith – to rapidly collect perilously close to the earth’s surface, causing dramatic doming of the overlying rocks.

The ability of explosive eruptions to swiftly generate such laccoliths is important for hazard assessments because magma stored at such shallow depths – only hundreds of metres – is prone to trigger further explosions.

Explosive volcanic eruptions, which occur when thick pressurised magma bursts out violently through a vent, are caused by intrusions of magma from the earth’s mantle building up into a high-pressure reservoir kilometres beneath the surface.

Scientists have long thought that magma intrusions such as pancake-shaped laccoliths precede and feed volcanic eruptions.

However, the team, from Lancaster University and the University of Mainz, have used satellite imagery and digital terrain models from before and after the 2011 eruption to show that the laccolith at Cordón Caulle formed during, rather than before the eruption.

The laccolith caused an area of several square kilometres around the volcano to bulge upwards by as much as 200 metres over one month.

This happened when the channel through which erupting magma rose to the surface became blocked, forcing it to instead inject sideways into the neighbouring rocks at a depth of only around 200 metres.

Dr Hugh Tuffen, of Lancaster University’s Environment Centre, a co-author of the study, explained: “It’s remarkable that such a large volume of magma was injected so close to the surface during an eruption. The magma is likely to remain hot for many years and could be reactivated, so hazard assessments must take this into account. The discovery that laccoliths can be fed by eruptions turns conventional thinking on its head and will force us to reappraise how eruptions and intrusions are linked”.

The study has implications for our understanding of volcanism on the Moon, Mars and Mercury, where laccoliths are also thought to have formed.

The full study, led by Professor Jonathan Castro from the University of Mainz, can be found here.