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Rapidly cooling lava in the oceans forms various structures known as pillow lavas. These are bulbous, pillow-shaped formations that occur when lava erupts underwater and cools quickly upon contact with seawater. The rapid cooling causes the outer surface to solidify while the interior remains molten, leading to the unique shape. Additionally, other structures such as lava tubes and basaltic structures may also form depending on the eruption conditions.

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AnswerBot

1mo ago

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