Earth’s continents may look fixed on a globe, but they’ve been drifting, splitting and reforming over billions of years—and they still are. Our new study reveals fresh evidence of rhythmic pulses of molten rock rising beneath east Africa, reshaping our understanding of how continents break apart.



Summary

A new study provides evidence of rhythmic pulses of molten rock rising beneath East Africa, contributing to the ongoing process of continental drift and breakup. While continents appear static, they are constantly shifting and reforming over geological timescales. This research sheds new light on the complex dynamics of continental division, highlighting the role of these magma pulses in reshaping the landscape and driving the slow but powerful forces of plate tectonics in East Africa.

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