Earth Has A Strange Hidden Layer Of Tectonic Plates

Beneath Changbaishan, a dormant volcano on the Chinese-North Korean border, lies a truly ancient tectonic plate. NASA

The base of the regular tectonic plates, at least when they’re “flat” on the surface, is about 200 kilometers (124 miles) down below, so the newly discovered ones are way beneath that. So what’s going on here?

It’s likely that these plates are ancient ones. They would have encountered another tectonic plate during their more shallow existence at a “subduction zone”. Being denser than the other, they would have sunk beneath their colossal opponent, broken off, and drifted down into the mantle.

They likely subducted during the Eocene Epoch, about 50 million years ago. Back then, the age of the dinosaurs had come to a dramatic close, and mammals, crocodiles, turtles and birds - those hardy avian dinosaurs still with us today - proliferated across the globe.

This study suggests that, at the same time, part of the Earth's surface collapsed and drifted below, never to be seen again - until now, that is, thanks to cutting-edge scientific techniques.

The discovery of this new layer of plate tectonics solves a long-standing mystery.

On occasion, incredibly deep-seated earthquakes rock the countries sitting above these plates, but they appeared to be originating from way below any known tectonic plate. You need plates to get quakes, so this has baffling scientists for a while now.

The newly discovered tectonic plates are found within the middle section of the mantle (medium orange). USGS

However, this new research has shown that they are probably coming from this new layer of tectonic plates. They may be semi-detached from the primary plates these days, but these enormous slabs can still bend, buckle, and break – and cause quakes as they do so. Indeed, their ongoing destruction is so energetic that it’s causing powerful shockwaves to make it all the way to the surface.

"Our results suggest that earthquakes can be produced thousands of kilometers away from a subduction zone from lateral movements of still-attached but mobile stagnant slabs within the uppermost ~660 kilometers of the mantle," the team explain in a statement.

The research has yet to be peer-reviewed, but it’s looking likely that, once again, Earth’s hellish depths have been holding back more secrets from us than we’d realized.

[H/T: Guardian]

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