
How did himalayas mountain form?
Answer
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Hint: The Himalaya is the fold mountain range in Asia isolating the fields (plains) of the Indian subcontinent from the Tibetan Plateau.
Complete answer: Himalayas, which stretch 2,900 km along the outskirt among India and Tibet. This mountain range started to frame somewhere in the range of 40 and 50 million years ago when two huge landmasses, India and Eurasia, driven by plate tectonics collided. Since both these land masses had about a similar rock density, one plate couldn't be subducted under the other. The weight of the impinging plates must be eased by pushing upward, bending the impact zone and forming the Himalayas. Around 225 million years back, India was an enormous island actually arranged off the Australian coast, and a big sea (called Tethys Sea) isolated India from the Asian landmass. At the point when Pangaea split up around 200 million years back, India started to move toward the north. Around 80 million years ago, India was found 6,400 km south of the Asian landmass, moving toward the north at a pace of around 9 m a century. At the point when India smashed into Asia around 40 to 50 million years ago. The impact and related reduction in the pace of plate movement are deciphered to stamp the start of the fast inspire of the Himalayas.
Note: The Himalayas comprise of parallel mountain ranges namely, the Shivalik Hills on the south; the Lower Himalayan Range; the Great Himalayas, which is the most noteworthy and focal reach; and the Tibetan Himalayas on the north.
Complete answer: Himalayas, which stretch 2,900 km along the outskirt among India and Tibet. This mountain range started to frame somewhere in the range of 40 and 50 million years ago when two huge landmasses, India and Eurasia, driven by plate tectonics collided. Since both these land masses had about a similar rock density, one plate couldn't be subducted under the other. The weight of the impinging plates must be eased by pushing upward, bending the impact zone and forming the Himalayas. Around 225 million years back, India was an enormous island actually arranged off the Australian coast, and a big sea (called Tethys Sea) isolated India from the Asian landmass. At the point when Pangaea split up around 200 million years back, India started to move toward the north. Around 80 million years ago, India was found 6,400 km south of the Asian landmass, moving toward the north at a pace of around 9 m a century. At the point when India smashed into Asia around 40 to 50 million years ago. The impact and related reduction in the pace of plate movement are deciphered to stamp the start of the fast inspire of the Himalayas.
Note: The Himalayas comprise of parallel mountain ranges namely, the Shivalik Hills on the south; the Lower Himalayan Range; the Great Himalayas, which is the most noteworthy and focal reach; and the Tibetan Himalayas on the north.
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