Volcanic mountains over hot spots in the mantle. Fault-block
The Himalayas is an example of a mountain range formed by the collision of the Indian Plate with the Eurasian Plate. The collision between these two plates has uplifted the region, resulting in the formation of the tallest mountains on Earth.
The Andes Mountains
Mountain chains are primarily formed at convergent tectonic plate boundaries, where two continental plates collide. This collision causes the crust to buckle and fold, leading to the uplift of mountain ranges. An example of this is the Himalayas, which were formed by the collision of the Indian and Eurasian plates.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
At a collision zone, two tectonic plates can form features such as mountains, earthquakes, and volcanic activity. The collision forces the plates to either converge, where one plate subducts below the other, or crumple and fold to create mountain ranges.
They are formed by the continental contienal plates
andean
Major mountain ranges are formed when crustal plates collide. The intense pressure and forces generated by the collision force the Earth's crust to buckle and uplift, forming mountain ranges.
A mountain is formed when tectonic plates converge and push against each other, causing uplift of the Earth's surface. This process can involve the collision of two plates, resulting in the formation of mountain ranges such as the Himalayas.
The Himalayas mountain chain was formed by the collision of the Indian tectonic plate with the Eurasian tectonic plate. This collision continues to push the two plates into each other, causing the Himalayas to still be one of the world's fastest-growing mountain ranges.
Pine Mountain was formed by the tectonic forces associated with the collision of the African and North American plates. The intense compression caused by these forces resulted in the uplifting and folding of the rock layers that make up Pine Mountain.
The collision of the Indo-Australian and Eurasian plates formed the Himalayan mountain range, which includes the Earth's highest elevation, Mount Everest.