The Mediterranean Seafloor Is SPLITTING — And the Volcano Beneath Santorini Is Reloading

Описание: #KolumboVolcano #Santorini #MediterraneanVolcano #AegeanSeismic

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The seafloor beneath the Mediterranean Sea is splitting apart as scientists analyzing data from the January 2025 earthquake swarm confirm what nobody expected: two volcanoes everyone thought were separate share the same deep magma reservoir, and the pressure has been building without stopping for nearly 400 years. Artificial intelligence deployed by the University of Athens expanded the earthquake catalog from thousands to over 25,000 hidden seismic events, revealing a geometrically precise underground magma dike slicing through the Aegean crust across 20 kilometers, connecting the Kolumbo submarine volcano directly to the Santorini caldera. Seafloor geodetic sensors confirm simultaneous ground subsidence above Kolumbo and surface uplift across Santorini in synchronized pulses, while the METEOR expedition M192 has just discovered one of the largest hydrothermal vent fields ever recorded in the Mediterranean, boiling fluids at 180 degrees Celsius erupting through active fault lines on the Milos seafloor 60 kilometers to the southwest. A 2025 study in Geophysical Research Letters confirms the Suez Rift declared dead 5 million years ago is still actively moving. With the shared magma chamber beneath Kolumbo growing at 4 million cubic meters per year and the underground network redistributing pressure across the entire Hellenic Arc, the 3.5 million tourists who visit Santorini every year are operating within a five minute tsunami window from a volcano most of them have never heard of.

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