The climax involves a building being filled with fast-moving, highly fluid lava due to the eruption of Mt. Vesuvius. Vesuvius does not erupt in this manner; as a composite volcano it erupts in Plinean or Peléan fashion, which is characterized partially by thick, slow, viscous lava flows that often doesn't even make it all the way down the mountainside.
Scritto da il 05/03/2025 alle ore 08:04

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