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The cooling of the Earth began shortly after its formation around 4.5 billion years ago, as the planet gradually lost heat from its molten state. This process involved the solidification of the Earth's crust and the cooling of the mantle and core over millions of years. Significant cooling events, such as the onset of glaciation, occurred later, with ice ages evident in the geological record, particularly during the last 2.4 billion years. The most recent major cooling period, known as the Quaternary glaciation, began about 2.58 million years ago and continues to influence the planet's climate today.

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1w ago

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In reality, the interior of the Earth is slowly cooling. In human time perspective, however, this cooling has no impact.


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