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Continental plate clashes usually lead to the formation of mountains and mountain ranges due to the impact caused by the collision.

Researchers at ETH Zurich have been able to demonstrate how well a mineral that can be found at the boundary between the Earth's core and mantle successfully conducts heat. This discovery led to a growing body of evidence, suggesting that the Earth is cooling faster than previously believed.

Researchers have discovered that Earth's "solid" inner core is actually a bit soft. The scientific world believed that Earth's inner core was a solid ball of compressed iron alloy which a liquid outer core covered for more than half a century. However, according to a recent study, the planetary ball's hardness varies from hard to semisoft to liquid metal.

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