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Why Earth’s Pacific Side Is Cooling So Much Faster

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 ...
A recent study published in Communications Earth & Environment has unveiled an extraordinary discovery: the solid rock deep ...
The D'' layer of the mantle flows in a solid state due to post-perovskite alignment, which accelerates seismic waves by 7%.
Strong new evidence suggests that primordial material from the planet’s center is somehow making its way out. Continent-size ...
If this “Dani plume” truly is a ghost plume, it would be the first one ever detected, and could possibly lead scientists to re-examine just how much heat is moving from the core-mantle ...
By simulating the movement of two continent-sized Big Lower-Mantle Basal Structures, or BLOBs, researchers may have uncovered the magmatic engine behind Earth’s most devastating eruptions.
According to the collected data, the plume is likely to be around 200–300 kilometers in diameter and as much as 100–300 °C (212–540 °F) hotter than the surrounding mantle.
The latest research also strengthens the case made in previous work that some mantle plumes incorporate material from Earth’s core, said the University of Copenhagen’s Waterton.