Table of Contents
Context: According to a recent discovery, the Indian Plate is splitting into two, with a portion of it sinking into the mantle.
Indian Continental Plate and Himalayan Formation
- The Indian Plate has been colliding with the Eurasian Plate for the last ~60 million years.
- This ongoing collision is the primary cause of the uplift of the Himalayas and the formation of the Tibetan Plateau.
- Traditionally, tectonic plates were thought to be rigid, but this view is now being challenged.
Delamination of the Indian Plate
- Delamination refers to a vertical tearing and peeling away of the dense lower layer of a tectonic plate.
- The lower part detaches and sinks into the Earth’s mantle, while the upper part may remain in place or move differently.
- Scientists discovered that a portion of the Indian Plate is undergoing delamination.
- This means the plate is splitting into two, and one part is sinking into the mantle.
- Delamination increases earthquake risks by changing how stress builds up in the Earth’s crust.
Areas at Risk
- Tibetan Plateau – already prone to earthquakes.
- Cona-Sangri Rift – a deep geological fracture possibly caused by this ongoing tear, may become a new seismic hotspot.