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The Himalaya mountain range stretches about 2,400 km from Tibet into Pakistan. It began forming when the Indian plate collided with the Eurasian plate. The pressure of the colliding plates forced the crust upward, folding, bending, and twisting rock. The Indian plate still moves north at a rate of about 5 cm/year, which is faster than your fingernails grow. Some mountains in the Himalayas lift up at a rate of 10 mm/year 1. At which type of plate boundary did the Himalayas form?​

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Final answer:

The Himalayas were created at a continent-continent convergent boundary due to the collision of the Indian and Eurasian tectonic plates, which caused the crust to buckle and form mountains.

Step-by-step explanation:

The Himalayas formed at a type of plate boundary known as a continent-continent convergent boundary. This occurs when two continental tectonic plates collide, which in the case of the Himalayas, involved the Indian plate and the Eurasian plate. The pressure and friction from this collision cause the Earth’s crust to buckle and fold, leading to the formation of the mountain ranges. The Indian plate continues to move northward at a rate of about 5 cm/year, driving the uplift of the Himalayas, which increases their elevation by about 10 mm/year. Earthquakes are common in these seismically active areas, which also include majestic peaks such as Mount Everest and K2.

User IntA
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This immense mountain range began to form between 40 and 50 million years ago, when two large landmasses, India and Eurasia, driven by plate movement, collided. Because both these continental landmasses have about the same rock density, one plate could not be subducted under the other.Mar. 9, 2015
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