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Earth's Core Is Cooling Faster Than We Previously Thought

 New research shows the Earth's core is cooling faster than we previously thought. 

Geologists studied the behavior of a mineral called Bridgmanite present at the boundary of the outer molten core and the inner mantle. 

A molten core is crucial to sustaining geological activity on our planet. Without it, the magnetic field would vanish, and the Earth would become a barren world like Mars or Mercury. 

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