Pozzuoli SPLITS Open as 8KM Fault RUPTURES — Campi Flegrei Magma SURGES, Vesuvius Link CONFIRMED!

Описание: Pozzuoli has become the epicenter of an escalating geological emergency as a newly identified 8-kilometer subterranean fracture cuts deep beneath the Campi Flegrei caldera, signaling a dangerous reorganization of southern Italy’s volcanic systems. What began as localized ground deformation is now understood as a major structural corridor capable of redistributing tectonic stress beneath one of Europe’s most densely populated regions.

Scientists analyzing recent seismic swarms and bradyseismic uplift confirm that the fracture penetrates far into the crust, potentially linking pressure systems beneath Campi Flegrei and Mount Vesuvius. While long treated as separate volcanoes, both are embedded within the same tectonic framework, and new data suggests their subsurface behavior may be becoming synchronized. Rising magma pressures, persistent uplift, gas flux anomalies, and clusters of micro-earthquakes indicate that stress is no longer confined to a single reservoir—but shared across an interconnected system threatening 3.5 million residents in the Naples metropolitan area.

Advanced monitoring by Italy’s National Institute of Geophysics and Volcanology (INGV), including satellite radar, AI-assisted seismic analysis, and ground-deformation sensors, reveals accelerating instability beneath Pozzuoli. Experts warn that even without an imminent eruption, this evolving fracture could amplify eruption potential, intensify ground collapse, and trigger cascading failures across the region’s volcanic arc—reshaping hazard models not just for Italy, but for the entire Mediterranean basin.

Pozzuoli fracture zone, Campi Flegrei unrest 2026, Vesuvius linked systems, Naples volcanic risk, bradyseism Pozzuoli, Italy seismic corridor, magma pressure redistribution, Mediterranean volcanic threat

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