Eduqas GCSE Geography · Coastal Hazards and their Management
Mini-Lesson
Coastal Hazards & their Management
This mini-lesson covers Eduqas Theme 4 — Coastal Hazards and their Management: why some coastlines are vulnerable, the waves and processes that shape them, the landforms of erosion and deposition, the threat of coastal flooding, and how coasts are managed — including "hold the line" vs "managed retreat".
Work through each screen, answer the questions as you go (multiple-choice, short-answer and games) and collect ⭐ stars. Press Start when you're ready.
Vulnerable coastlines
Why some coastlines are vulnerable
Eduqas asks you to explain why some coastlines are at greater risk of erosion and flooding than others. The main influences are:
Geology — soft rock (e.g. boulder clay) erodes far faster than resistant hard rock (e.g. granite).
Fetch and waves — a long fetch gives powerful destructive waves that erode more.
Relief — low-lying coasts (e.g. much of eastern England) are exposed to flooding from storm surges.
Rising sea level — climate change raises sea level, so waves reach further inland.
Key term — fetch: the uninterrupted distance of open sea over which the wind blows. A longer fetch (plus stronger, longer-lasting wind) makes bigger, more powerful waves.
Wave type
Constructive vs destructive waves
A wave has a swash (water rushing up the beach) and a backwash (water draining back down). Two kinds of wave shape the coast in opposite ways:
Constructive waves: low, long, strong swash — deposit sediment and build a beach. Destructive waves: tall, steep, strong backwash — drag sediment out and erode the beach.
Misconception: the constructive wave is the one that builds beaches (its swash is stronger than its backwash). Don't assume big, dramatic waves build up the coast — the tall destructive ones tear it down.
Quick check
Which wave builds a beach?
?A gently sloping beach has grown taller over the summer. Which type of wave is mainly responsible?
Coastal erosion
Four ways the sea erodes
Weathering (breakdown of rock in place, e.g. freeze–thaw) weakens the cliff. Then moving waves erode it by four marine processes:
Hydraulic action — the sheer force of water (and trapped, compressed air) pounding into cracks blasts the rock apart.
Abrasion (corrasion) — waves fling pebbles and sand against the cliff, sandpapering it away.
Attrition — rock fragments carried by the sea knock against each other, becoming smaller and rounder over time.
Solution (corrosion) — slightly acidic seawater dissolves soluble rock such as limestone.
Watch out:attrition wears down the sediment itself (making rounder pebbles); abrasion uses that sediment to wear down the cliff. Don't mix them up.
Match it
Match the process to its meaning
Tap a process on the left, then tap its correct description on the right.
Quick check
Which process?
?Over many years, angular pebbles on a beach become small and rounded. Which erosion process best explains this?
Transportation
Longshore drift moves the sediment
The sea moves eroded material along the coast. The key process is longshore drift:
Waves hit the beach at an angle, so swash carries sediment up diagonally; gravity pulls the backwash straight back down. Repeated, this zig-zag moves material along the coast.
Misconception: longshore drift moves sediment along the shoreline, not straight out to sea. It's the sideways, zig-zag transport of material — not the loss of a beach offshore.
Explain it
Your turn — longshore drift
✎Explain how longshore drift transports sediment along a coastline. Use the words swash, backwash and angle.
Model answer
Waves approach the beach at an angle (set by the prevailing wind), so the swash carries sediment up the beach diagonally.
The backwash then drains straight back down the beach under gravity (at 90° to the shoreline).
Repeating this zig-zag movement gradually transports the sediment along the coast in the direction the waves are pushing.
Erosion landforms
Cave → arch → stack → stump
Where hard and soft rock meet the coast, soft rock erodes into bays and resistant hard rock is left jutting out as headlands. On a headland, erosion attacks lines of weakness in a famous sequence:
1 A crack is widened into a cave. 2 The cave is cut right through the headland to make an arch. 3 The arch roof collapses, leaving an isolated pillar — a stack. 4 The stack is undercut and collapses to a low stump.
Where the sea attacks a cliff, it erodes a wave-cut notch at the base; the rock above collapses and the cliff retreats, leaving a wave-cut platform.
Quick check
Getting the order right
?What is the correct order in which these erosion landforms develop on a headland?
Deposition landforms
Deposition: beaches and spits
When waves lose energy — in sheltered bays or where the coast changes direction — they deposit sediment, building beaches, spits and bars.
Longshore drift carries sediment along the coast. Where the coastline bends, sediment is deposited in deeper water, building a spit. A change in wind direction can curve the end (a recurved spit); a bar forms if a spit grows right across a bay.Sort it
Erosion or deposition landform?
Tap a landform, then tap the box it belongs in.
🪨 Erosion
🏖️ Deposition
Coastal flooding
The threat of coastal flooding
Low-lying coasts face flooding as well as erosion. A storm surge is a temporary rise in sea level caused by low air pressure and strong onshore winds during a storm.
Rising sea level (climate change) means surges reach further inland and defences are overtopped more often.
Small Island States (e.g. the Maldives, Tuvalu) are extremely vulnerable — whole islands may be lost, creating environmental refugees.
Forecasting by the Met Office and the Environment Agency gives flood warnings so people can prepare or evacuate.
Exam link: Eduqas expects you to link coastal flooding to sea-level rise and to know its impact on vulnerable communities, including Small Island States.
Coastal management
Hard vs soft engineering
Coasts are managed to reduce erosion and flooding. Two broad approaches:
Hard engineering — sea walls reflect waves; groynes trap sediment moved by longshore drift and widen the beach; rock armour (rip-rap) and gabions absorb wave energy.
Soft engineering — beach nourishment adds sand to build up the beach; dune/marsh planting stabilises sediment naturally.
Sort it
Hard or soft engineering?
Tap the correct type of engineering for each defence.
Quick check
Choosing a defence
?A seaside town is losing its beach because longshore drift keeps carrying the sand away along the coast. Which hard-engineering defence is designed to trap that moving sediment and rebuild the beach?
Management strategy
"Hold the line" vs "managed retreat"
Shoreline Management Plans choose a policy for each stretch of coast, balancing the cost of defences against the value of the land:
Hold the line — keep defending the existing coastline with hard/soft engineering (used to protect towns and valuable land).
Managed retreat (managed realignment) — deliberately allow low-value land to flood or erode, often creating new salt marsh that absorbs wave energy.
Do nothing / no active intervention — allow natural processes where defending is not worthwhile.
Misconception:managed retreat is a deliberate decision to stop defending a stretch of coast and let it flood/erode naturally — it is a chosen strategy, not a failure or an accident. It is often used on low-lying coasts (e.g. parts of Essex and North Norfolk).
Explain it
Your turn — evaluating defences
✎Suggest one reason a coastal council might choose managed retreat instead of building a sea wall. Refer to cost and the value of the land.
Model answer
Hard engineering such as a sea wall is very expensive to build and maintain.
If the land being protected is low-value (e.g. farmland rather than a town), the cost of defending it is greater than its worth.
Managed retreat is cheaper and can create new salt marsh, which absorbs wave energy and provides a wildlife habitat.
Located case study
Case study: the Holderness Coast, UK
The Holderness Coast in East Yorkshire is one of the fastest-eroding coastlines in Europe, retreating on average about 1.5–2 metres every year.
Why so vulnerable? The cliffs are made of soft boulder clay (glacial till), which slumps easily when saturated. Powerful destructive waves have a long North Sea fetch.
Impacts: around 29 villages have been lost to the sea since Roman times; farmland, homes and roads continue to be lost.
Management: the town of Mappleton is protected by two rock groynes and rock armour (built 1991), which trap sediment and shield the cliff — "holding the line".
Conflict: the groynes trap sediment, so the coast down-drift (e.g. Great Cowden) is starved of beach material and erodes even faster — a source of conflict between residents.
Exam tip: a good case-study answer names the place, gives facts/figures (e.g. ~2 m/yr, 29 lost villages, Mappleton groynes 1991) and explains a conflict between different users of the coast.
Quick check
Understanding the case study
?At Mappleton, groynes trap sediment and protect the town. What is the main knock-on problem this creates for the coast further along (down-drift)?
Recap
The key ideas to know
Vulnerability: set by geology, fetch/waves, relief and rising sea level.