
"Uncovering an Ultra-Low Velocity Zone Beneath the Himalayas"
Researchers from Yale University have discovered an ultra-low velocity zone (ULVZ) beneath the Himalayas, 1,800 miles beneath Earth's surface, using seismic waves to study the structure just above the boundary between Earth's rocky mantle and metallic core. The ULVZ may have been formed by subducted material that had sunk from the surface down to the core-mantle boundary, providing direct evidence for subducted slabs playing a role in driving flow at the base of the mantle. This discovery sheds light on the poorly understood composition and role of ULVZs in mantle dynamics, offering insights into the interconnected processes of the deep mantle and their influence on tectonic plates and surface features.




