Who is Tectonic Uplift?

Tectonic Uplift is when parts of Earth’s crust are pushed up to make mountains or hills.

Imagine you have a big block of Play-Doh, and it's sitting on your table. Now, imagine two giant hands push the sides of that Play-Doh block from below, like someone squeezing underneath it. What happens? The middle part gets pushed up, forming a hill or mountain!

That’s what tectonic uplift is like in real life. Earth’s crust is made of big slabs called plates. These plates move slowly, sometimes pushing against each other. When they do, parts of the land are squeezed up, just like your Play-Doh.

Sometimes, this upward push happens over millions of years. You can think of it like stacking blocks one by one, not all at once, but little by little. The Himalayas are a great example, they were made when two huge plates pushed against each other and kept pushing up the land for a really long time.

So next time you see mountains or hills, remember: Earth is doing something like squeezing Play-Doh, just on a giant scale!