Science // Volcanoes & Earthquakes
Types of Rock
Know the three main types of rock — igneous (formed when lava or magma cools), sedimentary (formed from layers pressed together), and metamorphic — and that fossils are found in sedimentary rock
Quick check
If the learner finds different rocks on a beach walk, can they sort them and explain that some formed from cooled lava, some from layers pressed together over time, and that fossils are found in the layered ones?
Ask this to see whether the topic is secure.
Topic // Mastery
What mastery looks like
- Name the three main rock types: igneous, sedimentary, metamorphic
- Explain that igneous rock forms when lava or magma cools and hardens
- State that fossils are preserved in sedimentary rock because it forms in layers
Topic // Map
Where this fits
- RequiredMust come first
- HelpfulHelps, but not essential
Before this
4 topics- What Is a VolcanoRequired
Volcanoes & Earthquakes // Ages 5 to 7
Igneous rock concept links to lava cooling from volcanoes
- Earth Is Made of RockRequired
Volcanoes & Earthquakes // Ages 5 to 7
Rock types build on knowing Earth is made of rock
- Properties of materialsHelpful
Earth's Systems // Ages 7 to 8
Volcanic rock types topic parallels curriculum rocks classification
- Earth's LayersHelpful
Volcanoes & Earthquakes // Ages 7 to 9
Rock types benefit from knowing Earth has hot interior (explains melting for igneous)
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Types of Rock
Ages 7 to 9 // Concept
Leads to
2 topics- The Rock CycleRequired
Volcanoes & Earthquakes // Ages 9 to 11
The rock cycle connects the three rock types already learned
Dinosaurs & Paleontology // Ages 9 to 11
Dinosaurs rock strata/relative dating benefits from knowing rock types (igneous, sedimentary, metamorphic)
Topic // Research-informed
Teaching notes
From the Marble Skill Taxonomy. These notes have not been validated in classrooms, so treat them as a starting point for your own judgement.
The approach
For ages 7–9: learn the three main rock types — igneous (melt cools and hardens), sedimentary (layers of material pressed together), metamorphic (existing rock changed by heat and pressure) — and that fossils are found mainly in sedimentary rock BECAUSE it forms gently in layers that can trap and preserve remains, whereas melting destroys remains and intense heat/pressure usually destroys or badly squashes them. Ground the naming in hands-on classification of real specimens first (grains vs crystals vs layers vs bands vs fossils), then attach each name as shorthand for its formation story. Note the standards context: classifying rocks and describing fossil formation is the statutory KS2 skill, while the three type-names and rock cycle are formally KS3 vocabulary taught here as enrichment atop that hands-on work.
Common misconceptions
- All rock is basically the same material (there are distinct types formed by distinct processes).
- All rocks contain fossils / fossils can be in any rock (fossils are found in sedimentary rock because it forms in gentle layers).
- Brick, concrete and tarmac are kinds of rock (they are human-made materials, not natural rock).
- Igneous, sedimentary and metamorphic are just names to memorise (each name IS its formation story).
- Rocks never change from one type to another (they can, very slowly — the rock cycle, taught next at 9–11).
Useful representations
- A 'rock factory' with three formation processes: cooling melt → igneous; pressing layers → sedimentary (with a trapped shell); heat+squeeze → metamorphic
- Real rock specimens examined with a hand lens (crystals vs grains vs layers vs fossils)
- Sedimentary layers building up with a shell caught between them → revealed as a fossil
- Natural-vs-manufactured sort (granite/sandstone vs brick/tarmac/concrete)
Teaching practices
- Ground naming in hands-on classification first (hand lens: grains vs crystals, visible layers, fossils) — the statutory KS2 skill — then attach the type name to what was observed.
- Teach each type by its FORMATION STORY, not just a label: igneous = melt cooled and hardened; sedimentary = layers of bits pressed together; metamorphic = existing rock changed by heat and pressure.
- Make the fossils–sedimentary link causal, not a coincidence: gentle layering can trap and preserve remains; melting (igneous) and intense heat/pressure (metamorphic) would destroy them.
- Use real specimens (granite, sandstone/chalk, marble/slate) and building stones/gravestones so classification is evidential and local (links to Geography).
- Address the 'rock = human-made too' misconception (Oak National Academy): brick, tarmac and concrete are manufactured, not natural rock — sort natural vs made.
Activities to try
- 1
Run the rock factory: make each type and test what survives
Why it works: A rock's type is its formation story, and fossils are found mainly in sedimentary rock because gentle layering can trap and preserve remains, while melting (igneous) destroys them and intense heat/pressure (metamorphic) usually destroys or distorts them.
- At a 'melt' step, cool a glowing lava/magma pool and watch crystals lock together, forming igneous rock.
- At a 'layers' step, drop layers of sand and mud with a small shell tucked between them, press them down to make sedimentary rock, then split it open to reveal the shell as a fossil. (In real rock, hardening the layers and turning a shell into a fossil takes a very long time.)
- At a 'heat and squeeze' step, take an existing rock and increase heat and pressure until it changes, for example its minerals lining up in bands, forming metamorphic rock (many, though not all, metamorphic rocks show bands).
- Try to preserve a shell in each process: drop it into the lava, put it through the heat-and-press, and set it among gentle layers — observe which process preserves it and which destroy it.
- State in your own words why fossils are found mainly in sedimentary rock: why melting in igneous rock destroys them, and why heat and pressure in metamorphic rock usually destroy or squash them.
- 2
Hand-lens classification of real specimens
Why it works: Rocks can be compared and grouped by their appearance and simple physical properties, and the observable texture (crystals, grains, layers, bands, fossils) is evidence of how the rock formed.
- Examine real rock specimens such as granite, sandstone or chalk, and marble or slate with a hand lens.
- Look for distinguishing clues: interlocking crystals, loose grains, visible layers, embedded fossils, or bands/stripes (foliation).
- Sort the specimens into igneous, sedimentary, and metamorphic based on what you observe, then say which clue led to each decision. (Note crystals can appear in both igneous rock such as granite and some metamorphic rock such as marble. Marble usually has no bands, so compare the crystals instead: granite has mixed colours, marble is mostly one pale colour. With an adult, you can also check whether it fizzes in vinegar.)
- Where possible, link to local examples such as building stones or gravestones.
- 3
Natural rock or made by people?
Why it works: Brick, concrete and tarmac are human-made materials, not natural rock, even though they can look rock-like.
- Look at a mixed set including natural rocks (granite, sandstone) and manufactured materials (brick, tarmac, concrete).
- Sort each item into 'natural rock' or 'made by people'.
- Give a reason for each sort, focusing on whether the material formed by a natural process or was manufactured.
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