Paper

Dyke intrusion and stress-induced collapse of volcano flanks: The example of the 2018 event at Mt. Etna (Sicily, Italy)

Published Apr 14, 2020 · E. Giampiccolo, O. Cocina, P. De Gori

Scientific Reports

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Abstract

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Rigorous Journal

Study Snapshot

The 2018 Mt. Etna eruption was driven by magma intrusion through a dyke and local stress increase at the unstable flank, leading to flank collapse and episodic brittle faulting.

PopulationOlder adults (50-71 years)

Sample size24

MethodsObservational

OutcomesBody Mass Index projections

ResultsSocial networks mitigate obesity in older groups.

Dyke intrusion and stress-induced collapse of volcano flanks: The example of the 2018 event at Mt. Etna (Sicily, Italy)

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