While the cause of the leak remains unknown, as do the consequences for the Earth’s magnetic field, scientists appear to have resolved the decades-old debate about whether the Earth’s core and mantle exchange material or not.
The core is composed of iron and nickel, and with elements like platinum, gold, and tungsten. It reaches temperatures of 5,000 degrees Celsius (9,000 Fahrenheit) and many believe it’s responsible for up to 50 percent of the volcanic heat released around the planet.
The researchers, from French, Canadian, US and Australian universities, found newer mountains and rocks on the Earth’s surface featuring tungsten isotopes which are typically found in the outer core, but no farther up. As a result, the team posits that so-called ‘mantle plumes’ brought core material to the surface. There was no evidence of leaks prior to this recent discovery.
The implications of the research are still unclear. However, we know that the spinning solid part of the core is responsible for the Earth’s magnetosphere which helps protect us from the nastiest particles firing around space. Scientists believe that the liquid part of the core is slowly solidifying and this latest research may provide unique insights into both the evolution of the Earth’s core as well as the origin of our all-important magnetosphere.
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