Earth's Crust Has Many Rock Layers — Reading Comprehension

The Earth's crust is the outermost layer of our planet. It is made up of many different layers of rock. These rock layers are stacked on top of each other, like layers in a cake. Each layer forms over a long period of time. Some layers are very old, while others are much younger.

Most rock layers in the crust are called sedimentary rocks. These rocks form from small pieces of other rocks, sand, and even plants and animals. Over time, these tiny pieces are pressed together and hardened into new rock. This process is called sedimentation.

Each layer of sedimentary rock can tell us something about Earth's history. For example, a thick layer with seashells means the area was once underwater. Sometimes, you can find fossils in these layers. Fossils are the remains or marks of plants and animals that lived long ago. They help scientists learn what life was like in the past.

The layers in Earth's crust can be seen in places like the Grand Canyon. This famous canyon was formed by the Colorado River cutting through the rock over millions of years. The rock walls show many different colored layers, each from a different time in Earth's history.

Sometimes, heat and pressure deep underground can change sedimentary rocks into metamorphic rocks. Also, melted rock called magma can cool and form igneous rocks. This whole process of changing rocks is called the rock cycle.

Learning about Earth's rock layers helps us understand how the planet has changed over time and what it was like millions of years ago.

Interesting Fact: The Grand Canyon has rock layers that are over 2 billion years old!

What is Earth's outermost layer called?

What do fossils help scientists learn?

What forms most rock layers in the crust?

What does sedimentation do?

Where can you see many rock layers?

How are metamorphic rocks formed?

The rock cycle changes rocks. True or false?

What is magma?