Pole Flips Tied to Plate Tectonics: Continental Clumps Could Lead to Reversals in Magnetic Field

Article excerpt

Continents moving over millions of years in the slow-motion geologic jigsaw puzzle known as plate tectonics could trigger the occasional swapping of the north and south magnetic poles.

Assumed to be caused by random fluctuations in the circulation of the molten iron core, the flips may actually be tied to what's going on at Earth's surface. At times when landmasses have bunched together on one side of the equator, the Earth's magnetic field has begun flipping soon thereafter, suggests a study to appear in Geophysical Research Letters.

"What we see clearly is that the surface positions of the continents are linked with the frequency of the reversals," says group member Francois Petrelis, a geophysicist at the French research agency CNRS in Paris.

Other scientists aren't so sure, cautioning that more work needs to be done to confirm any such link.

Computer simulations have shown how molten iron in the spinning outer core can generate magnetic fields that spontaneously flip direction every so often, so that a compass that once pointed north would suddenly begin pointing south. The last reversal happened around 780,000 years ago. Before that there were periods with no flips for tens of millions of years, and others with lots of flips.

Curious about what drove these changes, Petrelis and his colleagues mathematically probed the way liquid iron flows in the core. In earlier work, they found that if the flow is interrupted so that it no longer moves symmetrically with respect to the equator, the planet's magnetic field soon reverses. …