Science  ›  5th Grade  ›  Earth's Layer Structure
5th Grade · Science

Earth's Layer Structure

Free sample questions, a clear explanation, and 5 practice skills with an AI tutor that guides without giving the answer away.

Concept Review

Earth's Layer Structure: Journey to the Center of Our Planet

What if you could dig a hole straight through the Earth? You'd travel 12,742 kilometers through four amazing layers before reaching the other side. Each layer has its own personality — different thickness, temperature, and even different materials!

Scientists have discovered that our planet is like a giant onion, with layers wrapped around each other. But unlike an onion, as you go deeper into Earth, things get incredibly hot and the pressure becomes crushing.

The Four-Layer Journey

🌱
Crust
5-70 km thick · Rocky · Cool temperatures
🔥
Mantle
2,900 km thick · Hot rock · Up to 4,000°C
🌊
Outer Core
2,300 km thick · Liquid iron · 4,000-6,000°C
Inner Core
1,200 km thick · Solid iron · 6,000°C

Here's what's fascinating: the deeper you go, the hotter it gets. The inner core is actually hotter than the surface of the Sun! All this internal heat doesn't just sit there — it moves upward, creating the volcanoes, hot springs, and geysers we see at Earth's surface.

🔑 Mind-Blowing Scale

If Earth were shrunk to the size of an apple, the crust would be thinner than the apple's skin. We live on the tiniest outer shell of our planet!

Yet despite being so thin, the crust varies dramatically — it's only 5 km thick under the oceans but up to 70 km thick under mountain ranges like the Himalayas.

The mantle makes up about 84% of Earth's volume and contains rock so hot it flows like thick honey over millions of years. This slow-moving rock creates the forces that push continents around and build mountains. The two cores are made mostly of iron and nickel — the outer core is liquid because of the intense heat, while the inner core is squeezed so hard by pressure that it stays solid despite being even hotter.

🔑 Key Takeaway

That 12,742-kilometer journey to the center would take you through four distinct worlds — from the rocky surface we know, through an ocean of liquid metal, to a solid iron ball hotter than the Sun. This hidden structure powers everything from the volcanoes in Hawaii to the geysers in Yellowstone, reminding us that our "solid" Earth is actually a dynamic, layered planet full of energy.

Sample questions

1. Maya is creating a model of Earth using clay. She wants to show all four main layers from the outside to the center. In what order should she build the layers?
Core, mantle, crust, atmosphere
Mantle, crust, core, outer space
Crust, mantle, outer core, inner core
Inner core, outer core, crust, mantle
Answer: Crust, mantle, outer core, inner core — Start from what you can see on Earth's surface and work your way down. The crust is the thin outer shell we live on, followed by the thick mantle, then the two parts of the core at the center.
2. True or False: The mantle is the thickest layer of Earth and is located between the crust and the outer core.
False - the outer core is the thickest layer
False - the mantle is located above the crust
False - the inner core is between the crust and outer core
True - the mantle is the thickest layer between the crust and outer core
Answer: True - the mantle is the thickest layer between the crust and outer core — The mantle makes up about 84% of Earth's volume, making it by far the thickest layer. It sits directly beneath the thin crust and surrounds the outer core.
3. A student draws a diagram showing Earth's layers but forgets to label them. The outermost layer in the diagram should be labeled as which layer?
Crust
Mantle
Outer core
Inner core
Answer: Crust — The crust is Earth's outermost solid layer - it's the thin 'skin' that forms the surface where we live, including the continents and ocean floor.

Skills in this topic

Practice 50+ questions on this topic

Unlimited interactive practice, progress tracking, and Nova — your AI tutor. Free to start.

Start learning free →