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Ice age cycles explain why the Earth cools, warms, and whether another freeze is coming
While the Milankovitch Cycles operate on timescales far longer than human lifespans, their effects are always at play.
Earth’s path around the Sun is not a fixed racetrack but a slowly shifting orbit, and those subtle changes have a long history of reshaping the planet’s climate. As astronomers refine how these ...
Around 12,000 years ago, the last Ice Age ended, global temperatures rose and the early Holocene began, during which time human societies became increasingly settled. A new study published in Nature ...
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