Scientists have discovered two enormous structures deep within Earth’s mantle. Research from Utrecht University reveals these regions are hotter and older than the surrounding sunken tectonic plates—at least half a billion years old, possibly older.
This finding challenges the idea that Earth’s mantle is well-mixed and fast-flowing, suggesting less movement in the mantle than previously thought.
Large earthquakes make the Earth vibrate like a bell with different tones. Seismologists study these tones to understand Earth’s interior. If the tones are “out of tune” or quieter, it indicates anomalies, helping to create images of Earth’s interior, similar to X-rays for doctors.