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Magma rose from deep underground due to pressure building within Etna's magma Plumbing system.

As the magma moved upward, it fractured the surrounding rock, creating long cracks (called fissures) on both the north and south sides of the volcano.

These fissures allowed lava and volcanic gases to escape, triggering the eruption.

The magma movement also produced thousands of earthquakes, some exceeding magnitude 4, as the volcano's eastern flank shifted slightly toward the sea.

The eruption began on 27 October 2002 and was notable because:

It produced spectacular lava fountains and extensive lava flows.

Large ash columns reached several kilometers into the atmosphere, disrupting air travel.

Lava destroyed buildings and ski facilities near Piano Provenzana.

Ashfall affected towns across eastern Sicily and temporarily closed Catania–Fontanarossa Airport.

Why did it happen?

The eruption was not caused by a single earthquake or external event. Instead, it resulted from:

Continuous tectonic forces where the African Plate slowly moves beneath the Eurasian Plate, generating magma beneath Sicily.

Pressure from accumulating magma inside Mount Etna.

Structural weaknesses in the volcano that allowed magma to break through to the surface.

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