Mountains are some of the most fascinating features of our planet. They can be very old or relatively young, and they are formed in different ways over millions of years. Some mountains are still growing, with folded layers of rock pushed up by natural forces. These young mountains have high peaks, deep valleys, and play an important role in nature, climate, rivers, and the lives of people living nearby.
The Himalayas are called a Young Fold Mountain. They were formed when the Indian Plate collided with the Eurasian Plate, pushing rocks upward and creating tall, sharp peaks. These mountains are still rising a little every year, which makes them young compared to older ranges like the Aravallis. Their pointed peaks, deep valleys, glaciers, and strong rivers show that they are still growing and geologically active.
The Himalayas are called young because their peaks are still pointed and not worn down by weather and erosion. In contrast, older mountains, like the Aravalli hills, have rounded and smoother shapes. They are called fold mountains because the Earth’s crust bent and folded under pressure when two tectonic plates collided. Even today, the Himalayas are still rising a little every year, showing that they are geologically very young.
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