Trigger for Volcanic Eruption Uncovered

The scientists identified crystal cumulate nodules discovered in pyroclastic deposits of major eruptions. The cumulate nodules are nothing but the igneous rocks formed by the accumulation of crystals in magma. They discovered that in pyroclastic deposits of major eruptions there was a pre-eruptive mixing within the magma chamber. This appears to be the repeating trigger in large-scale eruptions. 

A flashback at some of the destructive eruptions, the most disastrous eruption is The Las Candas volcanic caldera on Tenerife, in the Canary Islands. It has generated at least eight major eruptions during the last 700,000 years. These catastrophic events have resulted in eruption columns of over 25km high and expelled widespread pyroclastic material over 130km. Even the smallest of these eruptions expelled over 25 times more material than the 2010 eruption of Eyjafjallajokull, Iceland.

Now, the scientists have found a repeating trigger for the largest explosive volcanic eruption on Earth. This was done by the scientists from the University of Southampton.

The scientists identified crystal cumulate nodules discovered in pyroclastic deposits of major eruptions. The cumulate nodules are nothing but the igneous rocks formed by the accumulation of crystals in magma. They discovered that in pyroclastic deposits of major eruptions there was a pre-eruptive mixing within the magma chamber. This appears to be the repeating trigger in large-scale eruptions. Pre-eruptive mixing is where older cooler magma mixed with younger hotter magma. These nodules trapped and preserved the final magma beneath the volcano immediately before eruption.

Dr Rex Taylor, Senior Lecturer in Ocean and Earth Science at the University of Southampton, investigated nodules and their trapped magma to see what caused the eruptions.  He noticed that the nodules provide a record of the changes occurring in the magma plumbing right through to the moment the volcano erupted.

Dr Taylor says: "These nodules are special because they were ripped from the magma chamber before becoming completely solid -- they were mushy, like balls of coarse wet sand. Rims of crystals in the nodules grew from a very different magma, indicating a major mixing event occurred immediately before eruption. Stirring young hot magma into older, cooler magma appears to be a common event before these explosive eruptions."

Co-author of the study, Dr Tom Gernon, Lecturer in Ocean and Earth Science at the University of Southampton, says: "The analysis of crystal nodules from the volcano documents the final processes and changes immediately prior to eruption -- those triggering the catastrophic eruptions. The very presence of mushy nodules in the pyroclastic deposits suggests that the magma chamber empties itself during the eruption, and the chamber then collapses in on itself forming the caldera."

Dr Gernon, who is based at the National Oceanography Centre at Southampton's waterfront campus with Dr Taylor, adds: "Our findings will prove invaluable in future hazard and risk assessment on Tenerife and elsewhere. The scale of the eruptions we describe has the potential to cause devastation on the heavily populated island of Tenerife and major economic repercussions for the wider European community."

The paper was published in the latest issue of the open access journal Scientific Report.