Unveiling the Dynamic Dance of Iron Atoms in Earth's Inner Core
Scientists have discovered that the iron atoms in Earth's solid inner core are not stationary, but rather move within a hexagonal lattice structure. Using computer simulations and lab experiments, researchers found that the iron atoms switch positions without disrupting the overall structure, making the core more malleable and softer than previously thought. This newfound understanding sheds light on the dynamic processes and evolution of Earth's inner core.
