Deep beneath the Earth’s surface, scientists have discovered massive formations that could redefine our understanding of planetary evolution. These structures, known as large low-velocity provinces (LLVPs), may hold remnants of a lost planet that collided with Earth billions of years ago. As researchers delve into this theory, the implications for our planet’s history are profound.
- LLVPs may be remnants of lost planet Theia.
- Structures located 2,900 kilometers deep.
- LLVPs disrupt seismic waves, indicating density.
- Theia's collision formed the Moon 4.5 billion years ago.
- Findings could influence Earth's geodynamic behavior.
- Research may apply to other planetary bodies.
Located around 2,900 kilometers beneath the surface, these LLVPs are denser than the surrounding mantle and disrupt seismic waves. A recent study, published on 2025-05-25 15:30:00, suggests that these anomalies could be fragments of Theia, a Mars-sized planet believed to have collided with Earth, leading to the formation of the Moon. Could these remnants influence Earth’s geological processes?
This discovery raises intriguing questions about the origins of our planet’s internal structures. How did these dense regions form, and what role have they played in Earth’s development? Key points include:
- LLVPs are located near the core-mantle boundary.
- They could influence mantle convection and plate tectonics.
- The findings may apply to other planetary bodies like Mars and Venus.
As scientists continue to explore these ancient remnants, we may uncover more about the violent origins of our planet and its geological behavior. This research not only enhances our knowledge of Earth but also paves the way for understanding other celestial bodies in our solar system.
