Mountains. And earthquakes.
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.
When two continents collide, it usually forms a convergent boundary. This often leads to the creation of mountain ranges due to the intense pressure and folding of the Earth's crust. Examples include the Himalayas formed by the collision of the Indian Plate with the Eurasian Plate.
Tectonic plates.
Mountain ranges often form when large terrains and continents collide due to the intense tectonic forces that push the Earth's crust upward. The collision causes the crust to buckle and fold, creating towering mountain peaks and ranges. Examples include the Himalayas, Alps, and Andes.
Overlapping portions of two continents are known as continental plates or tectonic plates. These plates can collide, separate, or slide past each other due to the movement of the Earth's tectonic plates.
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.
Mountain chains are formed when continents collide.
Major mountain chains
Tectonic plates.
upward
Himalayas.
When two different air masses collide they form a cloud.
A mountain forms
when continents collide you bum your pet hamster
subduction zone
mountains
Generally, subduction zones are formed when two plates collide and one is heavier than the other. When two continents collide, rather than one sinking, they will both be uplifted because they are light and buoyant.
collide into each other