What will Earth look like 250 million years from now? In this video, we journey into the deep future to explore a day on our ...

Subduction zones, where one tectonic plate dives underneath another, drive the world’s most devastating earthquakes and tsunamis. How do these danger zones come to be? A study in Geology presents ...

Beneath Ethiopia, the Earth’s mantle is pulsing like a slow, steady heartbeat, slowly tearing Africa apart and laying the ...

Scientists have identified what could be the oldest rocks on Earth from a rock formation in Canada. The Nuvvuagittuq ...

Research led by Earth scientists at the University of Southampton has uncovered evidence of rhythmic surges of molten mantle ...

The Nuvvuagittuq Greenstone Belt has long been known for its ancient rocks — plains of streaked gray stone on the eastern ...

Researchers mapped a pulsing mantle plume under Afar that channels molten rock upward, stretching Africa’s crust until it ...

The vertical movement of the mantle is one of the driving forces that brings about large-scale geological changes to the ...

Around 252 million years ago, Earth faced a catastrophic event that changed the course of life on our planet forever. This mass extinction event wiped out nearly 96% of marine life, 70% of land ...

Our planet has been asteroid-smashed, melted and eroded, enough that most of its original armor has been long buried. Except ...

Tectonic plates are massive slabs of solid rock that make up Earth’s outer layer, known as the lithosphere. These plates float on the semi-fluid layer beneath them called the asthenosphere.