How Mountains Are Made

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Mountains are made by the slow movement of the giant rocky plates that form the Earth's outer shell, called tectonic plates. The Earth is like a cracked egg: a hot interior wrapped in a broken, rigid crust. As these plates push together, pull apart, or slide past one another, the land at their edges is squeezed, lifted, or split — and over millions of years, mountains rise.

There are three main ways this happens. Fold mountains form when two plates push into each other and the land between them crumples and folds upward, like a pushed-up rug — the Himalayas formed this way. Volcanic mountains build up when magma (hot melted rock) escapes through a crack and piles into layers as it cools. Block mountains appear when the crust cracks under stress and whole blocks are pushed up while others drop down.

Key ideas a learner takes away: the crust is made of moving plates, mountains grow incredibly slowly (about 1 cm a year, slower than a snail), and this building is still happening today.

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Frequently asked questions

How are mountains formed?
Mountains form when the Earth's tectonic plates move and press on the crust. The land can fold upward, be pushed up along cracks, or build up from cooled lava, creating fold, block, and volcanic mountains over millions of years.
What are the three main types of mountains?
Fold mountains form when two plates squeeze land into wrinkles; volcanic mountains build up as magma erupts and cools in layers; and block mountains form when the crust cracks and some blocks are pushed up while others drop down.
How fast do mountains grow?
Most mountains rise only about 1 cm a year — slower than a snail moves. A tall mountain range can take millions of years to form, and many are still slowly growing today.
Are mountains still being made now?
Yes. The Earth's plates are always moving, so mountains are still forming. The Himalayas, for example, are still rising a little each year as the Indian plate pushes into Asia.
What is the Earth's crust made of?
The Earth's outer shell is the crust, which is cracked into large pieces called tectonic plates. These plates float on the hot rock below and move very slowly, shaping mountains, valleys, and oceans.

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