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).
It was a convergent boundary. The Indian plate (continental) and Eurasian plate (continental) collided to form the mountains.
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In the case of the Indian Plate colliding with the Asian Plate, the Indian Plate pushed under the harder Asian Plate, and the Himalayan mountain range was thrust upwards.
A set of mountains that are still forming as a result of the compaction of two tectonic plates are the Himalayas. 40 or 50 million years ago, the subcontinent of India collided with Eurasia and caused so much pressure that the only way to relieve it was to push up and that was the start of the Himalayan range.
It formed the Himalayan Mountain Range, better known as just the Himalayas..
The Himalayan mountain chain is formed by the convergence of the Indian and Eurasian plates. This mountain formation due to convergent plates is more correctly known as an orogeny or orogenic event. Please see related links.
The mountain range that is being created by the collision between the Indian tectonic plate and Asian tectonic plate is the Himalaya.
A continental plate is colliding with another continental plate, causing upward motion. A lithospheric plate is colliding with another lithospheric plate of similar bouyancy, causing upward motion.
In the case of the Indian Plate colliding with the Asian Plate, the Indian Plate pushed under the harder Asian Plate, and the Himalayan mountain range was thrust upwards.
It is caused by the Techtonic plate on which India sits colliding with the techtonic plate to its north. This process is still going on and the Himalayas are still increasing in height as a result of it.
The Himalayan Mountain Range was thrust upwards when the Indian Plate crashed into the European Plate.
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.
A set of mountains that are still forming as a result of the compaction of two tectonic plates are the Himalayas. 40 or 50 million years ago, the subcontinent of India collided with Eurasia and caused so much pressure that the only way to relieve it was to push up and that was the start of the Himalayan range.
It is thought that the summit of Mount Everest started at the bottom of the ancient Tethys Sea, the motion of the Indian sub continental plate and the urasian continental plate colliding, about 30 - 50 million years ago, caused the mountain to rise up and become the highest mountain on the Earth.
An example is when the Indian Plate collided with the Eurasian Plate. The softer Indian Plate was forced downwards into the magma. This resulted in the formation of the Himalayan Mountain Range.
It is thought that the summit of Mount Everest started at the bottom of the ancient Tethys Sea, the motion of the Indian subcontinental plate and the urasian continental plate colliding, about 30 - 50 million years ago, caused the mountain to rise up and become the highest mountain on the Earth.
It formed the Himalayan Mountain Range, better known as just the Himalayas..
San Andreas Fault--transform plate boundary. Himalayan Mountain Range--convergent plate boundary. Mid-ocean ridge--divergent plate boundary.
Apart from having Mount Everest, the highest mountain in the world, the Himalayas was formed by the Indian Plate crashing into the Asian plate and being forced beneath the Asian plate. This collision resulted in the formation of the Himalayan Range, which is still slowly rising today.