Earth's continents are slowly moving across the planet's surface due to plate tectonics, culminating in regions of crustal expansion and collision. In the latter case, high temperatures and pressures ...

Himalaya, represents a continuous geological record from the Jurassic to Eocene period (≈201 to 34 million years ago).

The geology of the Himalayas is a record of the most dramatic and visible creations of the immense mountain range formed by plate tectonic forces and sculpted by weathering and erosion. The Himalayas, ...

This belt, known as the Ladakh Magmatic Arc, is now extinct, but once produced enormous amounts of molten rock deep beneath ...

Himalayas formed one of the most glamorous and youngest ranges in the world. They lie between the Indo-Gangetic Plains, in the south and the Tibetan Plateau, in the north to create a natural barrier ...

Astronauts onboard the International Space Station (ISS) shot these photographs of the Himalayas, the Tibetan Plateau, and the Indo-Gangetic plain. A team of researchers at the Stanford Doerr School ...

How were the Himalayan mountains shaped? Surprisingly, long before the collision between what is now India and Central Asia. To understand the mechanisms, geologists from the University of Adelaide ...

Beneath the feet of dinosaurs 165 million years ago, a green fuzz of mossy vegetation was surviving the crush. As the Indian landmass began to slam into Asia 65 million years ago, eventually thrusting ...

Research from the Indian Institute of Technology (IIT) Guwahati have developed a predictive framework to identify the locations where glacial lakes are likely to form in the Eastern Himalayan ...