
Ancient Mantle Islands Found Deep Inside Earth Redefine Mantle Dynamics
Two continent-sized regions deep in Earth’s mantle, called Large Low Seismic Velocity Provinces (LLSVPs), lie about 1,200 miles below the surface and rise roughly 620 miles, making them far larger than any surface mountain. They’re hotter and ancient, likely stable for hundreds of millions of years, and their existence suggests the mantle is not as well-mixed as previously thought. Seismic analyses show they dampen waves less than surrounding slabs, a property linked to unusually large mineral grains, reshaping ideas about mantle convection and the origin of mantle plumes.













