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Geology · Year 10

Active learning ideas

Weathering, Erosion, and Sedimentary Environments

This topic explores the processes of weathering and erosion that sculpt the Earth's surface. Students distinguish between the physical and chemical breakdown of rocks and how gravity, water, wind, and ice transport the resulting sediment. This is a core component of the Eduqas GCSE Geology Key Idea 5 and AQA Geography, linking geological processes to the formation of distinct UK landscapes.

National Curriculum Attainment TargetsEduqas GCSE Geology, Key Idea 5: Rock forming processes (Sedimentary processes)AQA GCSE Geography, Section C: Physical landscapes in the UK
20–45 minPairs → Whole Class3 activities

Activity 01

Simulation Game45 min · Small Groups

Simulation Game: The Sediment Race

Students use a 'stream table' (a tray of sand and water) to observe how different flow speeds transport different grain sizes. They record where 'boulders', 'sand', and 'silt' are deposited as the water slows down, mimicking a real river system.

What is the difference between weathering and erosion?
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Activity 02

Gallery Walk35 min · Pairs

Gallery Walk: Sedimentary Environments

Stations show photos of modern environments (e.g., the Sahara, the Mississippi Delta) alongside photos of sedimentary rocks. Students must match the rock (e.g., red sandstone with cross-bedding) to the environment that created it.

How do rivers, wind, and ice transport sediment?
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Activity 03

Think-Pair-Share20 min · Pairs

Think-Pair-Share: Chemical vs. Physical Weathering

Provide students with examples like 'freeze-thaw' and 'acid rain'. In pairs, they must explain the mechanism for each and predict which would be more dominant in the Scottish Highlands versus a tropical rainforest.

What can sedimentary structures tell us about past depositional environments?
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A few notes on teaching this unit


Watch Out for These Misconceptions

  • Weathering and erosion are the same thing.

    Weathering is the breakdown of rock *in situ*, while erosion involves the *movement* of that material. Using the analogy of 'breaking a biscuit' (weathering) versus 'blowing the crumbs away' (erosion) helps clarify this.

  • Rivers only erode during floods.

    Rivers erode constantly, though the rate increases significantly during floods. Hands-on stream table experiments help students see that even slow-moving water carries a 'suspended load' of fine sediment.


Methods used in this brief