Lesson 3 of 7

The rock cycle

Goal: Explain how rocks change from one type to another.

A river running through a canyon. The canyon walls are layers of red and cream rock, with loose rocks piled at the bottom

Over millions of years, rocks change from one type to another. This is the rock cycle.

IgneousrockSedimentSedimentaryrockMetamorphicrockMagma coolingweatheringand erosiondeposition,compaction andcementationheat andpressuremelting

Follow the arrows once round the cycle. There are short cuts too: any rock at the surface can be weathered, and any rock can be changed by heat and pressure, or melted.

  • Weathering wears rock down. Frost cracks it, plant roots split it and slightly acidic rain slowly dissolves it. The pieces stay where they are.
  • Erosion moves the pieces away. Rivers, ice and wind carry them.
  • Deposition, compaction and cementation make new rock. The pieces settle in layers. The weight on top squashes them, and minerals from the water glue the grains together.

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Key words in this lesson

Magma Molten rock below the surface of the Earth

Igneous rock Formed when magma cools and turns solid

Sedimentary rock Formed from layers of sediment squashed and stuck together

Metamorphic rock Formed when heat and pressure change an existing rock without melting it

Sediment Small pieces of rock that settle in layers

Weathering The wearing down of rock by physical, chemical or biological processes

Erosion The movement of pieces of rock by water, ice or wind

Rock cycle The processes that change rocks from one type to another

For teachers: AQA 3.7.1