Scientists reveal what triggered Santorini 'earthquake swarm'
Scientists reveal what triggered Santorini 'earthquake swarm' 21 November 2025 Share Save Victoria Gill Science correspondent Share Save getty The "swarm" of tens of thousands of earthquakes near the Greek island of Santorini earlier this year was triggered by molten rock pumping through an underground channel over three months, scientists have discovered.
The islands experienced tens of thousands of earthquakes - many of which were over magnitude 5.
Many tourists fled, and locals feared that the nearby underwater volcano, Kolumbo, might be about to erupt - or that this was a seismic prelude to a larger earthquake, like the devastating, magnitude 7. 7 quake that struck the same region in 1956. The scientists, who published their findings in the journal Science, created a 3D map of the Earth around Santorini. They then mapped the evolving patterns of seismic activity of each tremor and the movement and stress in the crust. This resulted in a detailed model of exactly what drove this months-long seismic swarm. The team found that the event was driven by the horizontal movement of magma - from beneath Santorini and the Kolumbo volcano - through a 30km channel that is more than 10km beneath the seafloor. The researchers estimated that the volume of magma that moved through the crust could have filled 200,000 Olympic-sized swimming pools. These "magma intrusions", as they are known, smashed through layers of rock, triggering thousands of tremors. Lead author on the study, Anthony Lomax, a research geophysicist who develops scientific software to analyse seismic activity, explained: "The tremors act as if we had instruments deep in the Earth, and they're telling us something. "[When we analyse] the pattern those earthquakes make in our 3D model of the Earth, it matches very, very well what we expect for magma moving horizontally. " Does this mean the Santorini unrest is over?
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