Banner
    A Common Trigger For Earth's Largest Volcanic Eruptions
    By News Staff | October 13th 2012 10:57 AM | Print | E-mail | Track Comments

    The Las Cañadas volcanic caldera on Tenerife in the Canary Islands has generated at eight major eruptions during the last 700,000 years, catastrophic events which resulted in eruption columns of over 10 miles high and expelled widespread pyroclastic material over 60 miles.

    For comparative purposes, even the smallest of those Tenerife eruptions expelled over 25 times more material than the 2010 eruption of Eyjafjallajökull, Iceland.  The Las Cañadas volcano is an IAVCEI (International Association of Volcanology and Chemistry of the Earth's Interior) Decade Volcano – identified by the international community as being worthy of particular study in light of their history of large, destructive eruptions and proximity to populated area.

    By analyzing crystal cumulate nodules, which are gneous rocks formed by the accumulation of crystals in magma, in pyroclastic deposits of major eruptions, the scientists found that pre-eruptive mixing within the magma chamber – where older cooler magma mixed with younger hotter magma – appears to be the repeating trigger in large-scale eruptions. 

    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 found that the nodules provide a record of the changes occurring in the magma plumbing right through to the moment the volcano erupted.

    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 found that the nodules provide a record of the changes occurring in the magma plumbing right through to the moment the volcano erupted.

    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." 

    The diagram shows the repeating development of the Las Cañadas magma chamber..Credit: Tom Gernon

    Co-author of the study, Dr Tom Gernon, Lecturer in Ocean and Earth Science at the University of Southampton, said, "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."

    Gernon, who is based at the National Oceanography Centre at Southampton's waterfront campus with Dr Taylor, added, "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."