
Over 50 million years ago, the subduction of the Indian tectonic plate and the Eurasian plate collided and formed the Himalayans. As India approached Asia, the Tethys sea began to shrink and slowly pushed upwards. Then disappeared 20 million years ago. The light sedimentary rock and metamorphic rock pushed against Tibet and creating a massive mountain fold..
The Tethys ocean floor was completely subducted with all the sediments of the Indian margin of the floor. So this is considered to be a convergent oceanic- continental. This means that it has a low density and is very thick. It does NOT subduct. So when the two continental plates collide, they just smash all together. Earthquakes and metamorphic rock are created from the force of the collision.

Today, the plates are still moving averaging about 2 cm each year!
https://www.ck12.org/earth-science/continent-continent-convergent-plate-boundaries/lesson/Continent-Continent-Convergent-Plate-Boundaries-MS-ES/
https://www.geolsoc.org.uk/Plate-Tectonics/Chap3-Plate-Margins/Convergent/Continental-Collision
https://www.pbs.org/wnet/nature/the-himalayas-tectonic-motion-making-the-himalayas/6342/
No comments:
Post a Comment