On July 3rd, Italy's Mount Stromboli volcano experienced a crater rim collapse, leading to the generation of a pyroclastic flow. This pyroclastic flow not only entered the Mediterranean Sea, but also travel more than 1000 feet into its waters above it. This video will discuss Stromboli's latest eruption, why pyroclastic flows can be so deadly, and will analyze infrared camera footage.
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YouTube Creative Commons video clips used in this video (CC BY 3.0 license):
[1] [ Ссылка ]
[2] [ Ссылка ]
[3] [ Ссылка ]
[4] [ Ссылка ]
Sources/Citations:
[1] INGVvulcani
[2] Calvari, Sonia & Cannavò, Flavio & Bonaccorso, Alessandro & Spampinato, Letizia & Pellegrino, Alessandra. (2018). Paroxysmal Explosions, Lava Fountains and Ash Plumes at Etna Volcano: Eruptive Processes and Hazard Implications. Frontiers in Earth Science. 6. 10.3389/feart.2018.00107. CC BY 4.0.
[3] Dellino, P., Dioguardi, F., Isaia, R. et al. The impact of pyroclastic density currents duration on humans: the case of the AD 79 eruption of Vesuvius. Sci Rep 11, 4959 (2021). [ Ссылка ], CC BY 4.0.
[4] DYNAMO
[5] UNO
[6] U.S. Geological Survey
0:00 Mount Stromboli Erupts
0:25 Pyroclastic Flow
1:13 Infrared Camera
1:43 Pyroclastic Flow Lethality
3:09 Lava Flow
3:54 What Could Happen Next
