Earth’s Outer Core Reversed Its Flow Beneath the Pacific — and Scientists Still Can’t Fully Explain It

Around 2010 the molten outer core beneath the Pacific unexpectedly flipped its flow from west to east. ESA satellite data shows the shift has been fading since 2020 — and the cause is still a mystery.

Roughly 3,000 kilometres beneath our feet lies Earth’s molten outer core — a churning ocean of liquid metal whose motion generates the magnetic field that shields our planet. And according to scientists, something unexpected has been happening down there.

A reversal beneath the Pacific

For a long time the flow of molten metal moved mostly westward. But around 2010, deep under the Pacific Ocean, it suddenly changed direction and began moving east. Researchers still can’t fully explain the flip.

How we can even know this

Nobody sees the core’s movement directly. Scientists infer it from tiny changes in Earth’s magnetic field, measured by satellites — among them the European Space Agency’s Swarm and CryoSat missions. A new analysis combined surface observations and orbital data spanning 1997 to 2025.

Why it matters

The outer core acts as the invisible engine driving Earth’s geomagnetic field. Any change in its flow draws attention, because it is tied to the stability of the magnetic shield that protects us from charged particles streaming off the Sun.

A mystery that is fading

The eastward flow beneath the Pacific strengthened and peaked around 2020. Since then, the latest data shows it has been weakening. What triggered the shift — and why it is now retreating — nobody yet knows for sure. The study was published in spring 2026.

Photo: NASA / Wikimedia Commons (public domain)

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AuthorDaniel Hart

Daniel Hart writes about science, technology and the curious discoveries shaping our world. He focuses on making complex findings clear and quick to read.