Last Updated:2025/11/21

The scoriaceous flow cooled rapidly, leaving behind a jagged, vesicular crust that crumbled underfoot.

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The scoriaceous flow cooled rapidly, leaving behind a jagged, vesicular crust that crumbled underfoot.

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そのスコリア状の流れは急速に冷えて、足元で崩れる鋭く多孔質の地殻を残した。

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