The Layers of the Earth
Earth looks solid and still, but under your feet it is made of layers, like an onion. Scientists cannot dig to the center, so they learn about the layers by studying earthquakes. When an earthquake shakes the ground, waves travel through the planet. The way the waves bend, speed up, and slow down tells scientists what the inside is made of.
The outer layer is the crust, a thin shell of solid rock. In proportion, the crust is about as thin as the skin of an apple. It is thickest under the continents and thinnest under the oceans.
Below the crust is the mantle, the thickest layer. The mantle is made of hot rock. It is solid, but over a very long time it flows slowly, like thick putty. Slow movements in the mantle are one reason the plates in the crust move.
At the center is the core, which has two parts. The outer core is made mostly of iron and nickel, and it is so hot that the metal is liquid. The inner core is also iron and nickel, but it is solid, because the pressure at the center of the Earth is so great that the metal cannot melt.
The motion of the liquid outer core also produces Earth's magnetic field. That field is the reason a compass needle points north.