Mountains, trees and weather
Can Earth's shell build mountains?
How mountains are built. A true how-it-works story for kids 5–9.
The Plate tectonics story, read aloud
Look out the window at the hills and houses. Everything sits on the ground under our car. Shh, here's a secret: that ground is moving right now! Earth has a hard outside, like the shell on an egg. But the shell is cracked into giant pieces.
Seven or eight big ones, and lots of little ones! When two pieces push into each other, the rock has nowhere to go. So it crumples and squishes upward. It's like pushing a blanket together on your bed. It bunches up into a bump!
Big bumps of rock become mountains! But the pieces move slower than a sleepy snail. Each year, only as far as your fingernails grow! Can you wiggle your fingernails? Mountains take a very, very long time to build.
Quiz the back seat
What happens when two pieces of Earth's shell push together?
Show the answer
They build mountains. They build mountains! Squish, squish, up! And it takes a very, very long time, longer than all the grown-ups you know put together.
Plate tectonics facts for kids
- Earth's rigid outer shell is broken into seven or eight major plates and many smaller ones.
- Plates usually move between zero and about 10 centimeters each year.
- Where plates meet, mountain-building, earthquakes and volcanoes can happen.
The Plate tectonics story, read aloud
On this road, the ground under our car feels still and solid. But it is moving, very slowly! Earth's hard outer shell is cracked into giant pieces, like a broken eggshell, and those pieces slide around. So can moving pieces of ground build a mountain? Let's follow one giant piece. It carries land and ocean on its back. Long, long ago, it drifted along, slower than slow.
It moved about as fast as your fingernails grow. A snail would win that race every single day! Then it bumped into another giant piece. Neither one would move out of the way. So they kept pushing, year after year after year. The ground where they met had nowhere to go but up. It crumpled and folded, like a rug when you push it against the wall.
Higher and higher it rose, until it became mountains. That's how the tallest mountains in the world grew! Count the hills you can see from the car right now. The giant pieces under us are still slowly pushing today. So mountains are still growing, a tiny bit at a time.
Quiz the back seat
How fast do the giant pieces of Earth's shell move?
Show the answer
About as fast as your fingernails grow. As fast as your fingernails grow! And when they push into each other, they can also shake the ground, which we call an earthquake.
Plate tectonics facts for kids
- Earth's hard outer shell is broken into seven or eight big plates and many small ones.
- Plates move from zero to about 10 centimeters a year.
- Where plates meet, there can be earthquakes, volcanoes and mountain-building.
Questions kids ask about Plate tectonics
Is the ground under us moving?
Yes, Earth's hard outer shell is cracked into giant pieces that move very slowly, about as fast as fingernails grow.
How do mountains form?
When two giant pieces of Earth's shell push together, the ground between them crumples and folds upward into mountains.
Why are there seashells on top of tall mountains?
Some mountains are made of old ocean floor that got pushed up into the sky when pieces of Earth's shell pushed together.
Are mountains still growing?
Yes, the pieces of Earth's shell are still pushing today, so some mountains are still growing a tiny bit at a time.
For grown-ups
Written with AI from public sources, then checked claim by claim against the sources below before it was published; stories that don't pass stay off the app and this site. Narration is pre-recorded, and nothing you do on this page is tied to your kids.
Sources
- education.nationalgeographic.org/resource/plate-tectonics
- nps.gov/subjects/geology/plate-tectonics-evidence-of-plate-motions.htm
- en.wikipedia.org/wiki/Plate_tectonics
- usgs.gov/faqs/how-fast-do-tectonic-plates-move
- geolsoc.org.uk/Plate-Tectonics/Chap3-Plate-Margins/Convergent/Continental-Collision.html?srsltid=AYCX9vLpTiAxT7dszhQm1hTbBXq8G2kh4c_4syW4q0yWFBqALBbvFoFt
- pubs.usgs.gov/gip/dynamic/himalaya.html
- ugc.berkeley.edu/background-content/mountain-building
- futura-sciences.com/en/mount-everest-is-still-growing-the-surprising-reason-scientists-just-revealed_32825
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