Layers of the Earth
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Learning Objectives
- 1Identify the four main layers of the Earth: crust, mantle, outer core, and inner core
- 2Describe a key feature of each Earth layer
- 3Order the four layers from the outermost to the innermost
Mini Lesson
If you could slice the Earth in half like an apple, you would see four distinct layers inside. Each layer has a different thickness, temperature, and composition. Scientists have discovered these layers by studying earthquake waves that pass through the Earth.
The Four Layers
- Crust — the thin, rocky outer shell we live on. It is divided into large pieces called tectonic plates. The oceanic crust (under oceans) is thinner than the continental crust (under land).
- Mantle — the thick layer beneath the crust, made of hot semi-solid rock. It is the largest layer. Slow-moving currents in the mantle drive the movement of tectonic plates.
- Outer Core — a layer of liquid iron and nickel. Its movement generates the Earth's magnetic field, which protects us from harmful solar radiation.
- Inner Core — the solid center of the Earth, made mainly of iron and nickel. Despite being the hottest part, it stays solid due to the enormous pressure from all the layers above.
Key Facts
- The crust is about 5–70 km thick — the thinnest layer.
- The mantle is about 2,900 km thick — the thickest layer.
- The outer core is about 2,260 km thick and is liquid.
- The inner core has a radius of about 1,220 km and is solid.
Remember the order from outside to inside: Crust, Mantle, Outer Core, Inner Core. You can use the initials C-M-O-I to help you recall them.
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