Clinopyroxenes - a Clue to Predicting Eruptions?
A correspondent has sent me THIS LINK concerning a paper about clinopyroxenes in rocks erupted in La Palma in the Canary Islands. The authors have examined, in excruciating detail clinopyroxenes erupted in three different eruptions. The research is also covered in "The Conversation" - see HERE.
These articles are all based on THIS PAPER in Nature. The authors have examined the crystals and have deduced an eruptive history of them by analysing the "growth rings" around the original core and from this deduce the following:- (this is an excerpt from a Google Gemini summary)
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Stagnant "Mush" Zones in the Upper Mantle: Deep beneath the island, around 18 to 25 kilometers (11–15 miles) down in the Earth’s upper mantle, magma sits in a cool (~1,000 to 1,025 °C), highly crystallized state known as a crystal "mush" (a sponge-like mix of mineral crystals and trapped liquid).
Recharge as an Unlocking Mechanism: At least one week prior to an eruption, fresh, hotter (~1,100 to 1,150 °C) magma surges up from deeper in the mantle. This hot recharge injects energy into the cool, sticky crystal mush, melting parts of it, unlocking the dense structure, and forcing the slushy mixture upward toward the surface.
Brief Stalling and Eruption: As the remobilized magma ascends, it may briefly pause in shallower crustal reservoirs (5–10 km depth) before erupting.
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The first thing which strikes me is the number of analyses - such a thing would have been impossible only a few years ago and unimaginable when I was a student. I also like them calling 1,000⁰ to 1,025⁰C cool!
They suggest that what they have found in the Canaries is applicable to other volcanic island and that the recharge - the second phase above - has a seismological signature which may be used to predict an eruption.
