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The most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.
The Himalayas were formed at a convergent plate margin where the Indian Plate collided with the Eurasian Plate. This collision resulted in the uplift of the Himalayan mountain range.
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
The Indian plate did not subduct when it collided with the Eurasian plate because the Indian plate is less dense than the Eurasian plate, causing it to be pushed upwards and form the Himalayan mountain range instead of being forced beneath the Eurasian plate.
The Himalayas mountain range was created when the Indian plate crashed into the European plate. The softer Indian plate was pushed under (a process known as subduction), lifting and forming the Himalayas (which is still growing).
India has it's own tectonic plate. It is not tectonically connected to the Eurasian plate. When the India plate crashed into the Eurasian plate, this formed the Himalayan Mountains. India is still moving closer to into the Eurasian plate today, and this is how the Himalayas are still growing.
The Himalayas are on the boundary between the Eurasian Plate and the Indo-Australian Plate.
The Himalayas were formed through a process of Convergent Plate Boundaries colliding together. The Indo-Australian and Eurasian plate collided together, to be specific.
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 Himalayas were lifted by the subduction of the Indian tectonic plate under the Eurasian Plate,
The Himalayas are the youngest Mountain range in the world.
Appalachian Mountains: Formed when the North American Plate collided with the African Plate. Himalayas: Created by the collision of the Indian Plate with the Eurasian Plate. Andes Mountains: Resulted from the subduction of the Nazca Plate beneath the South American Plate. Alps: Formed where the African Plate collided with the Eurasian Plate.