The Rock Cycle Loop
Age 14 · Science
Rocks are never finished: they slowly turn into new kinds of rock through melting, cooling, erosion, burial, heat and pressure. Igneous rock forms from cooled magma or lava, sedimentary rock from squeezed layers of sediment, and metamorphic rock from rock changed by heat and pressure deep underground.
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In the picture
- Basalt crust: lava cools and hardens into igneous rock
- River pebbles: wind, water and ice wear rock down and carry it away
- Sea floor layers: buried sediment is compacted and cemented into sedimentary rock
- Folded glowing layers: heat and pressure change rock into metamorphic rock without melting it
- Magma pool: rock melts deep underground and can rise again
Examples
- Pumice in a bathroom, used to scrub skin, is an igneous rock that formed from frothy lava cooling very fast.
- Marble kitchen worktops are metamorphic rock that was once limestone, a sedimentary rock made from shells.
Key takeaways
- Igneous, sedimentary and metamorphic rocks can each change into any of the other types.
- The rock cycle takes millions of years and is driven by Earth’s internal heat and by weathering at the surface.
Quiz: The Rock Cycle Loop (Age 14)
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How does metamorphic rock form?
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A sedimentary rock is part of the rock cycle. What can it eventually become?
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What drives the rock cycle, and how long does it take?
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