Coastal Processes and Landforms

GeographyAQAGCSEUnit: Physical Landscapes in the UK
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The basics

The Coast That Is Disappearing

🌊 The Coast That Is Disappearing

In 1995, the residents of Holbeck Hall Hotel in Scarborough watched their garden begin to slide towards the sea. Over four days, a 60-metre section of cliff collapsed, taking the hotel's south wing with it. The building was eventually demolished — not by any storm, but by the relentless, invisible work of water soaking into soft rock until gravity did the rest.

On the Holderness Coast in East Yorkshire, whole villages have vanished. In the village of Skipsea, a farmhouse photographed standing on clifftop ground in the 1990s is now gone — swallowed by the North Sea. Thirty villages that existed at the time of the Domesday Book in 1086 are now underwater. The coastline here retreats by an average of 1.7 metres every year — and after storms, sections can collapse by up to 10 metres in a single night.

The coast is not a passive, stable boundary between land and sea. It is an active battlefield, where waves carrying the energy of thousands of miles of open ocean meet rock and cliffs that have been weakening for centuries. Understanding that battle — the processes, the landforms, and why some coasts retreat while others resist — is the heart of this topic.

What is attrition?: Rocks and pebbles carried by waves knock against each other, breaking into smaller, rounder, smoother fragments over time.
Key terms

Geography glossary

What is attrition?
Rocks and pebbles carried by waves knock against each other, breaking into smaller, rounder, smoother fragments over time.
What is longshore drift?
Waves approach the beach at an angle, moving sediment along the coast in a zigzag pattern. Swash moves material up at an angle; backwash pulls it back at 90 degrees.
Spotlight
Wave Energy: Where It Comes From and Why It Matters

Every wave that crashes against a British cliff started as a tiny ripple hundreds or even thousands of miles away. When wind blows across open water, friction between the air and the water surface transfers energy into the ocean. The water particles begin to move in circular orbits — they don't actually travel with the

Exam tip

Earn the mark scheme marks

🧠 Memory Frameworks for Coastal Processes

HASA — The Four Erosion Processes

H — Hydraulic action — air compression in cracks → pressure release → rock fractures
A — Abrasion — sediment as sandpaper → grinds down cliff face and wave-cut platform
S — Solution — acid seawater dissolves limestone/chalk → chemical attack
A — Attrition — sediment particles collide → get smaller and rounder → boulder to pebble to sand

Remember the difference: H, A and S attack cliffs. The second A (Attrition) acts on sediment in transit — it rounds pebbles, not cliffs.

CASE — Factors Affecting Erosion Rate

C — Cliffs (rock type): soft clay or chalk erodes fast; hard granite resists
A — Arrival of waves (fetch): long fetch = high-energy destructive waves
S — Sand and beach: wide beach absorbs energy; no beach = direct cliff attack
E — Engineering and climate change: sea walls and groynes change sediment budget; sea level rise accelerates everything

The Headland Sequence: C — A — S — S

Cave → Arch → Stack → Stump. Each stage in the destruction of a headland begins with hydraulic action exploiting a weakness and ends with the complete collapse and erosion of the remaining structure.

Now try it yourself

Quiz · Question 1 of 20

Which of the following best describes a destructive wave?

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