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The surface is broken into plates and they are moving now

The Earth has a thin crust, a thick mantle that flows very slowly, and a core. The crust is broken into plates that move a few centimetres a year. Earthquakes and volcanoes occur mostly where plates meet, which is why they are not spread evenly.

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In beta. This lesson was written for Hone and has not yet been checked by a state certification officer. Practice material, not professional advice. What that means.

What it is for

The evidence is the lesson: the coastlines fit, the same fossils appear on both sides of an ocean, and earthquakes cluster in lines. A class asked to explain that pattern can reason their way to plates, and that is a far better hour than being told.

How to think about it

Start from the map, not the mechanism. Ask why earthquakes are in lines rather than everywhere, and why identical fossils are found on separated continents. Then name what would explain it, and only then describe the layers underneath.

Worked example

Crust is thin and solid; the mantle beneath flows extremely slowly; the core is the centre
Three layers, and the middle one is what carries the plates.
Plates move a few centimetres a year, about as fast as a fingernail grows
Slow, and never stopped.
Plates pulling apart make new crust; pushing together builds mountains or subducts one plate
Two boundaries, two very different landscapes.
Earthquakes and volcanoes cluster along boundaries, which is why the map has lines on it
The pattern is the evidence, and it came before the explanation historically too.

Your turn

Name the layer beneath the crust that the plates move on.

The plates move on the 

The trap

Describing the mantle as liquid. It is solid rock that deforms and flows over very long timescales. Calling it liquid makes the crust sound like a raft on a sea, which misleads about almost everything that follows.

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