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Mountains are formed by the movement of tectonic plates, which are large sections of the Earth’s crust. When two plates collide, a process called convergent boundary — the intense pressure forces the Earth’s crust to buckle and fold, pushing it upwards to form mountains. This is how major mountain ranges like the Himalayas were created, where the Indian plate collides with the Eurasian plate. In some cases, one plate may also be forced under another in a process called subduction, which can also
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