Santorini Quakes Tied to Deep Underground Magma, Not Tectonic Faults, Says New Study
Earlier this year, the iconic Greek island of Santorini was rocked by an unusual and persistent series of small earthquakes that left residents and scientists puzzled. The tremors, some occurring every few minutes, lasted over a month, reached magnitudes as high as 5.3, and forced more than 10,000 people to evacuate the area. But new research from a University of Oregon geophysicist suggests the answer lies not in tectonic shifts, but in deep volcanic unrest hidden beneath the island’s surface.
Just days before the seismic swarm began, Dr. Emilie Hooft and her team submitted a study offering new insights into the volcanic plumbing system under Santorini. Their findings now appear to shed light on the true cause of the earthquakes: magma shifting 6 to 9 miles beneath the surface — not di...








