The Layers Of The Earth

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The layers of the Earth are the distinct shells of material that make up our planet, stacked from the surface down to the centre. There are four main layers: the crust (the thin, solid outer skin we live on), the mantle (the thick middle layer of hot rock that flows very slowly), the outer core (a layer of liquid molten metal), and the inner core (a solid ball of metal at the centre). Together they reach roughly 6,400 km from the surface to the middle of the Earth.

These layers form because of heat and pressure. The deeper you go, the hotter and more squeezed the material becomes β€” the inner core is hotter than the outer core, yet it stays solid because the enormous pressure stops the metal from melting. The mantle's slow-flowing rock is what drives moving continents, earthquakes and volcanoes at the surface.

Learners come away knowing the order of the four layers from outside to centre, why temperature rises with depth, and the surprising fact that the outer core is liquid while the even-hotter inner core is solid.

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Frequently asked questions

What are the four main layers of the Earth?
From the outside to the centre they are the crust, the mantle, the outer core and the inner core. The crust is the thinnest and the mantle is the thickest.
Why is the inner core solid if it is the hottest layer?
The inner core is under enormous pressure from all the layers pressing down on it. That pressure squeezes the metal so tightly that it stays solid even though it is hotter than the liquid outer core.
Which layer of the Earth do we live on?
We live on the crust, the thin outermost layer. All the soil, rock, seabed and buildings β€” including everything in Singapore β€” sit on top of the crust.
Why does it get hotter as you go deeper into the Earth?
Heat left over from when the Earth formed, plus heat from natural radioactive material inside, makes the temperature rise the closer you get to the centre. The inner core can reach thousands of degrees Celsius.
What is the mantle made of?
The mantle is made of hot, dense rock. It is so warm that the rock can slowly flow like very thick toffee, even though it is mostly solid, and this slow movement helps cause earthquakes and volcanoes.

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