The collision of the Indian plate with the Asian plate created the Himalayas, Karakoram, and Hindu Kush mountain ranges. These are some of the highest and most geologically active mountain ranges in the world.
A mountain range is most likely to occur because of the two continents crushing and building up large mounds until they are mountains. This is what happened with India when it collided with Asia.
The two countries located in the Himalayas are Bhutan and Nepal
Mountain Range, example is the Himalayas Mountains in ASIA, formed from collision of Indian with Asia during its northward migration from Gondwanaland.
There is a compressional stress on the rocks which causes the crust to shorten. Reverse faults (the hanging wall moves up) occur at convergent plate boundaries. In continental-continental convergent boundaries, where two continents collide, the crust becomes deformed and thickened forming mountain chains. This is known as orogenesis or mountain building. This occurrence explains the creation of the Himalayas where India and Asia collided. Strictly speaking, it is the tectonic plates that collide, not just the continents. The shortening of the land may be accommodated by land folding. For example, the Indian Plate is colliding with the Asian Plate, causing land shortening and mountain folding and building. (Have a glance at the path of the rivers rising in the Himalayas.).
The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.
Two continents collided to form the Himalayan mountain range in Asia. The collision between the Indian Plate and the Eurasian Plate continues to push the Himalayas upwards, making them one of the youngest and tallest mountain ranges in the world.
The Himalayas
Africa and North America
The Indian Plate and the Eurasian Plate collided to create the Himalaya mountains.
When two continents collide, they can form mountain ranges through a process called continental collision. The pressure and forces generated by the collision cause the Earth's crust to uplift and fold, leading to the creation of large mountain systems. An example of this is the Himalayas, which formed when the Indian Plate collided with the Eurasian Plate.
The two continents that collided to form Pangaea were Gondwana and Laurasia. Gondwana consisted of present-day South America, Africa, Antarctica, Australia, and the Indian subcontinent, while Laurasia included North America, Europe, and Asia.
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.
The Ural Mountains were formed by the continents of Europe and Asia joining together.
The collision of the Indian plate with the Asian plate created the Himalayas, Karakoram, and Hindu Kush mountain ranges. These are some of the highest and most geologically active mountain ranges in the world.
The Himalayas contain the tallest mountain in the world: Mount Everest. Also, it divides up Asia and it's sub continent (India). The Himalayas were formed when two tectonic plates collided into each other.
The Himalayas are young fold mountains. The range was formed when the Indio-australian tectonic plane collided with the Euro-asian tectonic plane. The where we find the Himalayas today was previously filled with sediments, which was carried by the rivers of the Euro-asian plane. When the two previously mentioned plane collided this sediment folded to form the Himalayan range.