Switzerland and Iceland
The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.
The Alps does not separate any continents.
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, 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.
Fold mountains are usually formed when two tectonic plates carrying continents collide, causing the crust to buckle and fold, resulting in the formation of mountain ranges. The collision forces the rocks to be pushed upwards, forming large mountain belts with distinct fold patterns. Examples of fold mountains include the Himalayas and the Alps.
The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.
The Alps does not separate any continents.
The Alps does not separate any continents.
The Ural Mountains were formed by the continents of Europe and Asia joining together.
when two cars collided
Africa and North America
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.
The two continents of Africa and Eurasia pushed together and folded the rocks into mountains.
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.
They were formed on the edges of two ancient continental plates that collided with each other in the geological past.
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 Indian subcontinent broke off from Africa over a hundred million years ago. It then moved to the southern coast of Asia. When it collided with Asia, the formation of the Himalaya began.