The Earth is really, really old, like older than your grandpa’s favorite tree.
Imagine you have a huge jar full of jellybeans. Every time you take one out, it means something happened on Earth, like a big earthquake or a new mountain growing. If the jar has billions of jellybeans, that means a lot of things happened, and the Earth is still going strong! Scientists use special tools to count these “jellybean moments” and figure out how long ago the Earth started.
Like a Really Old Cookie
Think of the Earth like a big, tasty cookie. When it was first made, it was hot and gooey. Over time, it cooled down, just like your cookie cools on the counter. Scientists look at layers in rocks, kind of like layers in a cake. Each layer is like a new bite of the cookie, telling them when it was baked.
Using Clocks in Rocks
Some rocks have tiny “clocks” inside them, scientists call them radioactive clocks. These clocks tick very slowly, and by counting how many ticks there are, they can tell how old the rock is. It’s like having a super slow clock that you can use to figure out how long ago your cookie was made! The Earth is really, really old, like older than your grandpa’s favorite tree.
Imagine you have a huge jar full of jellybeans. Every time you take one out, it means something happened on Earth, like a big earthquake or a new mountain growing. If the jar has billions of jellybeans, that means a lot of things happened, and the Earth is still going strong! Scientists use special tools to count these “jellybean moments” and figure out how long ago the Earth started.
Like a Really Old Cookie
Think of the Earth like a big, tasty cookie. When it was first made, it was hot and gooey. Over time, it cooled down, just like your cookie cools on the counter. Scientists look at layers in rocks, kind of like layers in a cake. Each layer is like a new bite of the cookie, telling them when it was baked.
Using Clocks in Rocks
Some rocks have tiny “clocks” inside them, scientists call them radioactive clocks. These clocks tick very slowly, and by counting how many ticks there are, they can tell how old the rock is. It’s like having a super slow clock that you can use to figure out how long ago your cookie was made!
Examples
- Fossils in layers of rocks help us know when ancient animals lived.
- Scientists compare the age of a rock to an atomic clock.
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See also
- Geology in a Minute - What is Geology?
- Ask Series | What are Mountains?
- How Do Volcanoes Shape Earth's Surface?
- How Do We Know How Old the Earth Is?
- How Do Volcanoes Shape Landscapes?