The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.
the Himalayas were formed by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.
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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.
The Himalayas were lifted by the subduction of the Indian tectonic plate under the Eurasian Plate,
collision of tectonic plates
The Indian Plate and the Eurasian Plate are the two major tectonic plates involved in the formation of the Himalayan mountain range. The collision between these plates has led to the uplift of the Himalayas over millions of years.
collision of tectonic plates
the Himalayas were formed by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.
The Himalayas are Fold Mountains
The Himalayan mountains were created by the collision of the Indian Plate with the Eurasian Plate. This collision resulted in the uplift of the Earth's crust and the formation of the towering mountain range that we see today.
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 Himalayas are on the boundary between the Eurasian Plate and the Indo-Australian Plate.