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THE GEOLOGICAL PROCESS OF MOUNTAIN RANGE FORMATION Mountain ranges are formed through complex geological processes, mainly driven by the movement and collision of tectonic plates. When two continental plates collide, immense pressure forces the Earth's crust to buckle and fold, pushing rocks upward and forming towering mountain belts. This process can take millions of years and often involves earthquakes, metamorphism, and volcanic activity. Such formations are key indicators of Earth's dynamic
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The Himalayas, one of the world's most prominent mountain ranges, formed as a result of tectonic plate movements. Around 50 million years ago, the Indian Plate began to collide with the Eurasian Plate. As the Indian Plate, which was once a separate landmass, moved northward, it encountered the Eurasian Plate. The collision between these two massive plates caused the land to buckle and fold, leading to the uplift of the Himalayas. This process is known as continental collision or continental conv
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