the rocky mountains
The Himalayas were formed by the collision of the Indian continental plate and the Eurasian plate. This collision began around 50 million years ago and is ongoing, causing the Himalayas to continue to rise in height each year.
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).
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.
The mountains on the west coast of North America, such as the Cascade Range and Sierra Nevada, were mainly formed by the movement of tectonic plates. The collision of the Pacific Plate with the North American Plate caused compression and uplift, leading to the formation of the mountain ranges we see today. Additionally, volcanic activity played a significant role in shaping these mountain ranges over millions of years.
The Himalayas were formed through the collision of the Indian Plate and the Eurasian Plate. This collision began around 50 million years ago and is ongoing, resulting in the uplift of the Himalayan mountain range. The immense pressure and forces created by the two plates pushing against each other caused the land to rise and form the highest mountain range in the world.
A continent-continent collision occurs when two continental plates converge and push against each other. This collision can lead to mountain building, as seen in the collision between the Indian Plate and the Eurasian Plate that formed the Himalayas.
A basic mountain should be formed from the collision of continental crust and oceanic crustAnswerWhen an oceanic and a continental crust collide, the heavier oceanic crust tends to subduct under the lighter continental crust. Because of the collision and corresponding compression and also because of volcanism related to dehydration and melting of the subducted plate a mountain range is formed. The Andes mountain range is a, if not the, most typical example.
A mountain range can be formed by the collision of an oceanic plate and a continental plate. This creates a subduction zone which eventually leads to the formation of a range of mountains.
Andes - continental oceanic aleutians - oceanic oceanic North American cordillera - arc continent Appalachians - continental continental
the andes mountains were formed by a continental collision
An oceanic plate colliding with a continental plate formed the Sierra Nevada. That collision is no longer happening, though, as that oceanic plate. the Farallon Plate, is mostly gone, with remnants to the north and south.
Continental Collision Boundary
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).
Most of the large mountain ranges formed as a result of continental drift/collision, some of the smaller ranges were formed in other ways.
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.
There are mainly two kinds of mountains, namely fold mountains and block mountains. Fold mountains are formed when a continental plate collides with either another continental plate or an oceanic plate. One example of a continental-continental collision is the collision of the Eurasian plate and the Indo-Australian plate, forming the Himalayas fold mountains range which contains Mt. Everest and K2. One example of a oceanic continental collision is the collision of the Nazca plate and the South American plate, forming the Andes mountains. ---- Block mountains are formed when two plate diverge from each other and sink downwards, leaving a highland in the middle of them. That is a block mountain. You might find this useful, http://en.wikipedia.org/wiki/Mountains.
Its when the oceanic crust and the continental crsut colide together.
False! When two continental plates converge a mountain range is formed. This is what formed and is continuing to "build" the Himalayan mountain chain.Subduction zones form where oceanic crust converges with and is forced under continental crust, or younger more buoyant oceanic crust.