Stable parts of the Earth's crust may not be as immovable as previously thought. While much of the crust is affected by plate tectonic activity, certain more stable portions have remained unchanged ...
With findings on Earth’s polar extremes and its innermost core, scientists shaped how we look at the planet in 2025 in ...
Scientists have recently unearthed a significant discovery, revealing unexpected movements occurring deep within the Earth’s crust, specifically 2,700km beneath the surface. This discovery has shed ...
In 2025, scientists discovered that gold is escaping from Earth's core and the world's oldest rocks may be located in Quebec, ...
Earth's continental configurations have changed dramatically over its billions of years' history, transforming not only their positions across the planet, but also their topography as expansion and ...
From Earth’s oldest rocks to glowing swamp lights and hidden ocean life, scientists in 2025 uncovered clues beneath our feet ...
Emerging evidence suggests that plate tectonics, or the recycling of Earth's crust, may have begun much earlier than previously thought — and may be a big reason that our planet harbors life. When you ...
Our planet was born around 4.5 billion years ago. To understand this mind-bendingly long history, we need to study rocks and the minerals they are made of. The oldest rocks in Australia, which are ...
Movement of the crust isn’t the only factor shaping Earth’s topography. Credit: Nachoman-au via Wikimedia Commons, CC BY-SA 3.0 Movement of the crust isn’t the only factor shaping Earth’s topography.
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Why one side of the Earth is cooling faster and what scientists think it reveals about our planet
Researchers are exploring the idea that one hemisphere of Earth, dominated by the Pacific Ocean, is losing internal heat faster than the continental s ...
ANN ARBOR—As anyone with a smattering of geological knowledge knows, Earth’s crust is made up of plates that creep over the planet’s surface at a rate of several inches per year. But why do they move ...
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