Science // Earth's Systems
How fossils form
Describe in simple terms how fossils are formed when things that have lived are trapped within rock over millions of years
Quick check
Can the learner explain how a shell or bone from an ancient creature ended up preserved inside a rock?
Ask this to see whether the topic is secure.
Topic // Mastery
What mastery looks like
- Describe the basic process: organism dies, gets buried in mud/sand, layers build up, material turns to rock over millions of years
- Explain that the organism's shape is preserved as a fossil within the rock
- Give examples of common fossils (shells, bones, leaf imprints, footprints)
Topic // Map
Where this fits
- RequiredMust come first
- HelpfulHelps, but not essential
Before this
2 topics- Properties of materialsRequired
Earth's Systems // Ages 7 to 8
Must examine rocks before understanding how fossils form within rock
- Living, Dead & Never AliveHelpful
Ecosystems & Habitats // Ages 6 to 7
Understanding living vs dead supports understanding what gets fossilised
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How fossils form
Ages 7 to 8 // Concept
Leads to
3 topics- Fossils as EvidenceRequired
Dinosaurs & Paleontology // Ages 8 to 11
Must understand fossil formation in rocks before interpreting fossil data for evidence of past life
- How fossils formRequired
Space Systems & Earth's History // Ages 9 to 10
Must understand fossil formation before interpreting fossil patterns in rock layers
- How Fossils FormHelpful
Dinosaurs & Paleontology // Ages 7 to 9
Curriculum fossil formation topic (GB Y3) directly underpins detailed dinosaur fossil formation understanding
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 7–8, teach how fossils form as an ordered process story: an organism dies, is quickly buried in sediment, more layers pile on and press down, over millions of years sediment turns to rock while the organism's shape is preserved (often as minerals replace the material), and much later the rock is exposed and the fossil found. Two big ideas carry the most weight: burial must be QUICK (before the body rots or scatters) and fossilisation takes an ENORMOUS amount of time. Distinguish body fossils (shells, bones — shape preserved in stone) from trace fossils (footprints, imprints — evidence of activity). Link to prior learning that fossils occur mainly in sedimentary rock and that only once-living things fossilise. A driveable simulation of the process is proposed as the central activity, with sequencing/sorting practice, a retelling task, a tap-to-reveal cross-section, an optional excavation and expert Q&A, and a hands-on plaster-cast as complements. These are research-informed proposals, not validated interventions.
Common misconceptions
- 'Fossils are the actual bones/animal, unchanged' — not knowing minerals replace/preserve the shape in rock.
- 'Fossils form quickly' — missing the millions-of-years timescale.
- 'Any dead thing becomes a fossil' — not realising it needs quick burial and the right conditions (most don't fossilise).
- 'Fossils are found in any rock' — rather than mainly sedimentary rock.
- 'A footprint isn't a fossil' — not recognising trace fossils.
- 'Dinosaurs and fossils are the same thing' — conflating one example with the whole concept.
Useful representations
- A step-by-step fossil-formation sequence strip (die→bury→compress→rock→expose).
- Cross-section showing an organism buried under accumulating sediment layers.
- Body-fossil vs trace-fossil example cards (shell/bone vs footprint/imprint).
- A cast/mould demonstration (press a shell into clay, fill with plaster).
Teaching practices
- Teach fossilisation as an ORDERED sequence (die → bury → layers build → turn to rock → exposed/found) and have children retell it in order.
- Foreground the two big ideas: quick burial (before decay) and immense time (millions of years).
- Distinguish body fossils (shape preserved: shells, bones) from trace fossils (footprints, imprints) with examples.
- Link to prior learning — fossils form in sedimentary rock, and only once-living things fossilise.
- Use vivid before/after imagery and, ideally, a hands-on 'cast' model (plaster over a shell) to make preservation-of-shape concrete.
Activities to try
- 1
Fossil-formation time machine (drive the process)
Why it works: Fossilisation is a time-ordered process with a hidden mechanism; quick burial is essential (waiting too long usually means the remains are rotted, broken up or scattered before they can be preserved) and the process takes an unimaginably long time. The shape is preserved in rock rather than the unchanged original surviving.
- Place a dead organism (for example a shell or a small animal) on an ancient seabed.
- Face a choice: bury it now or wait — if you wait too long, scavengers, decay and moving water can break up and scatter it so nothing is left to become a fossil; choose to bury it quickly.
- Drag layer after layer of sediment on top of the buried organism.
- Move a time slider to sweep across a very long time (millions of years) and watch soft mud compress and harden into rock while the organism's shape is preserved in stone.
- Dig down and lift out the finished fossil.
- 2
Sequence and sort the fossil facts
Why it works: Consolidate the ordered sequence, the body-vs-trace distinction, and the vast timescale.
- Put the five fossilisation stages in order: organism dies → buried quickly in mud/sand → layers build up and press down → sediment turns to rock over millions of years (shape preserved) → rock exposed and fossil found.
- Sort example cards into body fossils (shell, bone) versus trace fossils (footprint, imprint).
- Answer how long fossils take to form: days, years, or millions of years (millions of years).
- 3
Retell the fossil story and explain the conditions
Why it works: A full explanation names burial in sediment, layers building up, sediment turning to rock over millions of years with the shape preserved, and why fossilisation is rare.
- In your own words, retell the fossil-formation sequence in order, from the organism dying to the fossil being found.
- Explain why most dead things — like leaves that fall in a park every autumn — do NOT become fossils.
- State what has to happen to the dead animal or plant first, before it can become a fossil.
- Describe whether a shell fossil found in rock is the unchanged original shell or something else, and how a shell ended up inside rock.
Topic // Standards
Curriculum standards
- The national curriculum in England: Key stages 1 and 2 framework document
- Y3.Sci.R.2
Science // Earth's Systems
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