The are many types of fluids that flow between the deep mantle underlying Yellowstone National Park and the atmosphere above ...

Why should one half of our world be losing its internal heat like a runny kettle, and the other retain it like a snug thermos ...

Amazon dieback”, as this grim scenario is known, is just one example of what climate scientists refer to as a tipping point: a threshold beyond which self-sustaining processes irreversibly push a part ...

Between 50 and 100 kilometers (30–60 miles) above the Earth's surface lies a largely unstudied stretch of the atmosphere, ...

The D'' layer of the mantle flows in a solid state due to post-perovskite alignment, which accelerates seismic waves by 7%.

Have you ever wondered how Earth came to be? In this video, we’ll take you on a fascinating journey through the origins of ...

The seafloor is far thinner than the bulky landmass, and temperature from within Earth is “quenched” by the enormous volume ...

A hot blob of rock beneath New Hampshire may be helping the Appalachian Mountains stand so tall. The rock mass is slowly on ...

The scientists say extremes — including heat and deadly floods — persisted in July despite a slightly lower global average ...

Strong new evidence suggests that primordial material from the planet’s center is somehow making its way out. Continent-size ...

Deep heat beneath the Appalachian Mountains may be linked to an ancient rift with Greenland, helping explain why the range is ...

Another (and, in our view, more important) source of energy for life on Iceheim is the heat coming from its core, underneath ...