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The Himalayas were formed over millions of years due to the collision between the Indian and Eurasian tectonic plates. As the Indian plate pushed northward, it collided with the Eurasian plate, causing the Earth's crust to buckle and rise, forming the towering peaks of the Himalayas. This process, known as orogeny, continues today, slowly pushing the mountains higher each year. The Himalayas stand as a testament to the immense forces shaping our planet.


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