How Earth's wandering poles return home

How Earth’s wandering poles return home

by Tushna Commissariat

A number of times over the past one billion years, the Earth’s surface has “wandered” relative to its rotational axis – before returning to its original position. Now, a team of geophysicists from the US and Canada says it has developed a theory that explains this curious phenomenon of “oscillatory true polar wander”. Understanding the mechanics behind polar wander is crucial, as a shift could tip the Earth over by as far as 50° over a period of 10–100 million years and this would cause profound global environmental and geological changes.

True polar wander (TPW) can be defined as the relative movement between the mantle (and so the surface of the Earth) and the Earth’s spin axis or its rotational axis. Incredibly, researchers believe that over the past one billion years, the Earth’s surface has “tipped over” and then returned to its original location six times along the same axis – this is the process of “oscillatory true polar wander”. Scientists have worked this out by studying magnetism in rocks – a discipline known as “paleomagnetism”. If a rock cools in a magnetic field, it records the magnetic properties of the field and these can be decoded in the lab millions of years later. So, by measuring changes in the orientation of the Earth’s magnetic field that are stored in ancient rocks, scientists can “see” the effects of the oscillatory TPW.

Extreme shifts

“Someone sitting on the Earth would have seen the pole shift up to 50° and then turn around and return close to its original location, all in tens of millions of years,” explains geophysicist Jerry Mitrovica of the Earth and Planetary Science Department at Harvard University. “But an observer floating in space would actually see the rotational axis stay relatively vertical and the Earth’s surface tip over and then back.” Unsurprisingly, these rather extreme and dramatic shifts can be linked to global changes in all large-scale Earth systems such as the carbon cycle, climate and even evolution. “After all, if it happened today, a shift of 50° one way might put Boston [Massachusetts] near the north pole, while a shift in the opposite direction would bring Boston near the equator,” says Mitrovica.

But this in itself is not news – earth scientists have known for a while that TPW does occur and they even know why. They believe that the initial shift of the pole – or the Earth tipping over – is caused by large-scale flows in the Earth’s interior known as “mantle convection”, involving thermal convection currents that carry heat from the Earth’s core to the surface. This is the same process that drives continental drift and plate tectonics. So, mantle convection disturbs the rotational equilibrium of the Earth and the result is a shift in the relative orientation of the Earth’s solid surface and its rotational axis.