Hidden magma pathway revealed by 2025 Santorini crisis
An intense earthquake swarm shook the Santorini–Amorgos region of Greece beginning on January 27, 2025, lasting about 45 days and producing more than 16 000 tremors between 5–15 km (3–9 miles) below the seafloor. A joint seismological study has revealed that the 2025 Santorini crisis was not a typical tectonic swarm. It was the signature of magma moving through a hidden corridor connecting the Santorini and Kolumbo volcanoes, two of the most active systems in the eastern Mediterranean.

