Pink diamonds are extremely rare. Most—about 90 percent—have come from one location: the Argyle mine in Australia. Now scientists think they know how the rosy gems ended up there.
Diamonds form when the element carbon (C) is exposed to intense pressure in Earth’s interior. Normally, the stones are clear. But if the crystals—solids whose atoms are arranged in a repeating pattern—are bent, they become pink. The sideways force required to bend diamonds’ crystal structure only occurs when there is a collision between tectonic plates—the slow-moving slabs of rock that make up Earth’s crust, or outer layer.