The Himalayas wereformed as a result of the collision between the Indian Plate and Eurasian Plate. ... As a result of this collision, the sedimentary rocks which were settled in the large-scale depression in the Earth's crust called Tethys were folded and formed the Himalayas ...

Formation of the Himalayas
The Himalayas, one of the youngest mountain ranges on Earth, were formed around 50 million years ago through the collision of the Indian and Eurasian tectonic plates. This collision led to the uplifting of the Earth's crust, resulting in the formation of the majestic Himalayan mountain range.

Plate Tectonics
- The Indian plate, moving northwards at a rate of about 5 cm per year, collided with the Eurasian plate.
- The immense pressure and force generated by this collision caused the crust to crumple and fold, leading to the formation of the Himalayas.

Subduction and Uplift
- As the Indian plate continued to move northwards, it was forced beneath the Eurasian plate in a process known as subduction.
- This subduction caused the Indian plate to melt and release magma, which then rose to the surface and solidified, contributing to the growth of the Himalayan range.
- The intense pressure and heat generated by the subduction also led to the uplift of the Earth's crust, further contributing to the elevation of the Himalayas.

Continued Growth
- The Himalayas continue to grow even today, albeit at a slower rate, as the Indian plate continues its northward movement.
- The ongoing collision between the Indian and Eurasian plates results in the formation of new mountain ranges and peaks within the Himalayan range.
In conclusion, the formation of the Himalayas is a result of the complex interplay of plate tectonics, subduction, and uplift processes, which have shaped this iconic mountain range over millions of years.