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Erosional Landforms: Cliffs, Arches, StacksActivities & Teaching Strategies

Active learning works for this topic because erosion processes unfold over long timescales, making hands-on modeling and sequencing essential for students to grasp change over time. Concrete experiences with materials and images help students move beyond textbook descriptions to personal observations of differential erosion and landform development.

Year 12Geography4 activities30 min45 min

Learning Objectives

  1. 1Analyze the sequential processes of erosion and deposition that lead to the formation of cliffs, wave-cut notches, caves, arches, stacks, and stumps.
  2. 2Compare the erosional characteristics of different coastal landforms, differentiating between caves, arches, and stacks based on their structural development.
  3. 3Explain how wave-cut platforms serve as geomorphological evidence for past sea-level changes and coastal retreat.
  4. 4Classify coastal landforms based on their dominant erosional processes and stage of development.

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45 min·Small Groups

Modelling: Headland Erosion Trays

Fill trays with layered sand and clay to form headlands. Direct water hoses or droppers to simulate waves, noting cliff retreat, cave formation, arch collapse, and stack isolation. Groups photograph each stage and annotate changes on worksheets.

Prepare & details

Analyze the sequence of events leading to the formation of a stack from a headland.

Facilitation Tip: During Headland Erosion Trays, circulate to ensure students vary wave angles and materials to see how refraction focuses energy on headlands rather than bays.

Setup: Wall space or tables arranged around room perimeter

Materials: Large paper/poster boards, Markers, Sticky notes for feedback

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30 min·Pairs

Sequencing: Landform Evolution Cards

Distribute shuffled cards showing diagrammed stages from cliff to stump. Pairs arrange them chronologically, justify links with process explanations, then present to class for peer feedback.

Prepare & details

Differentiate between different types of caves and their erosional origins.

Facilitation Tip: For Landform Evolution Cards, ask groups to justify their sequence order by pointing to erosion processes in their model or textbook before finalizing.

Setup: Wall space or tables arranged around room perimeter

Materials: Large paper/poster boards, Markers, Sticky notes for feedback

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40 min·Individual

Profiling: Wave-Cut Platform Analysis

Provide cross-sectional photos of platforms from UK coasts. Individuals draw profiles, label erosion evidence, and infer past sea levels. Share in small groups to compare interpretations.

Prepare & details

Explain how wave-cut platforms provide evidence of past sea levels.

Facilitation Tip: When Profiling Wave-Cut Platforms, have students measure slope angles and platform widths to connect erosion rates with platform preservation over time.

Setup: Wall space or tables arranged around room perimeter

Materials: Large paper/poster boards, Markers, Sticky notes for feedback

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35 min·Small Groups

Concept Mapping: Virtual Jurassic Coast Tour

Use Google Earth to explore sites like Old Harry Rocks. Small groups identify and sketch cliffs, arches, stacks, adding labels for formation processes and sea level indicators.

Prepare & details

Analyze the sequence of events leading to the formation of a stack from a headland.

Facilitation Tip: On the Virtual Jurassic Coast Tour, pause at each location to ask students to predict the next landform stage based on current erosion evidence.

Setup: Tables with large paper, or wall space

Materials: Concept cards or sticky notes, Large paper, Markers, Example concept map

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Teaching This Topic

Teach this topic by layering physical models with visual timelines and real-world mapping. Avoid rushing through the stages; let students experience the slow, cumulative nature of erosion through repeated trials and observations. Research shows that combining tactile modeling with spatial mapping improves spatial reasoning and process understanding in geomorphology.

What to Expect

Successful learning looks like students explaining how wave refraction targets headlands, tracing cave-to-arch-to-stack evolution through multiple activities, and using platform profiles to infer past coastal changes. Students should connect processes like hydraulic action and abrasion to specific landform features they create or analyze.

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Watch Out for These Misconceptions

Common MisconceptionDuring Headland Erosion Trays, watch for students who assume waves erode all coastlines evenly.

What to Teach Instead

Redirect their attention to the refraction diagram and have them adjust wave angles in their tray to see energy concentration on headlands, then compare erosion between headland and bay materials.

Common MisconceptionDuring Landform Evolution Cards, watch for students who think arches and stacks form in a single storm.

What to Teach Instead

Ask groups to build a timeline using the cards, writing estimated durations (centuries) on the back of each card to challenge instant-formation ideas.

Common MisconceptionDuring Profiling Wave-Cut Platforms, watch for students who think wave-cut platforms only show current sea levels.

What to Teach Instead

Have students measure platform elevation above current sea level and compare it to historical sea level data provided in the activity, prompting discussion about uplift or past lower sea levels.

Assessment Ideas

Exit Ticket

After Headland Erosion Trays, provide an unlabeled coastal headland image. Ask students to label cliffs, arches, stacks, and wave-cut notches, then write one sentence explaining which process (hydraulic action, abrasion, or solution) most shaped the arch.

Quick Check

During Landform Evolution Cards, present a mixed set of diagrams showing arch formation and collapse out of order. Ask students to sequence them individually, then pair up to discuss and revise their orders before revealing the correct sequence as a class.

Discussion Prompt

After Profiling Wave-Cut Platforms, pose the question: 'How can the width of a wave-cut platform help us infer the rate of coastal erosion?' Facilitate a class discussion where students use their profile measurements and erosion process knowledge to explain their reasoning.

Extensions & Scaffolding

  • Challenge students to design a new coastal feature not listed, explaining the erosional processes and materials that would create it.
  • For students who struggle, provide pre-labeled diagrams of caves and arches with missing labels to fill in during the Sequencing activity.
  • Deeper exploration involves researching how human structures like seawalls alter erosional landform development and presenting findings in a short report.

Key Vocabulary

Hydraulic ActionThe force of moving water, particularly waves, compressing air in cracks in rocks, widening them and dislodging material.
AbrasionThe grinding and wearing away of rock surfaces by sediment particles carried by waves, similar to sandpapering.
Wave-Cut NotchA groove or indentation at the base of a cliff, formed by wave erosion at the high tide line.
Wave-Cut PlatformA gently sloping, flat area of bedrock exposed at low tide, extending from the base of a cliff seaward, formed by wave erosion and subsequent sea-level lowering or cliff retreat.
StackAn isolated pillar of rock standing in the sea, formed by the collapse of an arch.

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