There’s So Much Pressure at the Earth’s Core, it Makes Iron Behave in a Strange Way

New observations of the atomic structure of iron reveal it undergoes "twinning" under extreme stress and pressure. Image Credit: SLAC National Accelerator Laboratory

It’s one of nature’s topsy-turvy tricks that the deep interior of the Earth is as hot as the Sun’s surface. The sphere of iron that resides there is also under extreme pressure: about 360 million times more pressure than we experience on the Earth’s surface. But how can scientists study what happens to the iron at the center of the Earth when it’s largely unobservable?

With a pair of lasers.

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