Erosional Landforms

Trace the sequence from crack to cave to arch to stack to stump.

  • Define and explain Erosional Landforms in your own words
  • Use key terms such as longshore drift accurately
  • Apply what you have learned to new examples and questions
  • Avoid the common mistakes learners make with this topic

This lesson focuses on Erosional Landforms: trace the sequence from crack to cave to arch to stack to stump.

Definition: Erosional Landforms

Trace the sequence from crack to cave to arch to stack to stump.

Key ideas

Waves come in two types

Destructive waves are tall, steep and frequent, with a powerful backwash that drags sediment down the beach — they erode. Constructive waves are lower, longer and less frequent, with a strong swash that pushes sediment up the beach — they build. Winter storms bring destructive waves; calm summer conditions bring constructive ones, so beaches often shrink in winter and recover in summer.

Coasts work as systems

A coastal system has inputs (weathered cliff material, river sediment), transfers (longshore drift), stores (beaches, dunes) and outputs (sediment lost offshore or to another cell). Building a groyne or sea wall interrupts the transfers, which is why protecting one stretch of coast can starve beaches further along the sediment cell.

Key term — longshore drift: The zigzag movement of sediment along a beach, driven by waves approaching the shore at an angle.

Worked example: Erosional Landforms

Put these in order: arch, stump, cave, stack.

Cave → arch → stack → stump.

Answer: Cave → arch → stack → stump.

Common mistakes
  • Saying longshore drift moves sediment straight along the beach The movement is a zigzag: swash up at an angle, backwash straight down. The net result is alongshore, but the path is not straight.
  • Confusing swash and backwash Swash is water rushing up the beach; backwash is water draining back down. In constructive waves the swash is stronger; in destructive waves the backwash dominates.

Practice

Describe two differences between destructive and constructive waves.
Compare their shape, frequency and which wash is stronger.

Destructive: tall, steep, frequent, strong backwash — erode. Constructive: low, long, less frequent, strong swash — deposit.

What is fetch, and why does it matter?
Think about how waves grow.

The distance wind blows over water; longer fetch allows bigger, more powerful waves to develop.

How does a wave-cut platform form?
Think about what happens at the base of a cliff over time.

Waves erode the cliff base by hydraulic action and abrasion, undercutting it until the overhang collapses; as the cliff retreats, a rocky platform is left behind at the high-tide level.

Give one advantage and one disadvantage of groynes.
Think about what happens updrift versus downdrift.

Advantage: they trap sediment and widen the beach updrift. Disadvantage: they starve beaches downdrift, increasing erosion there.

Quick check

Erosional Landforms — quick check

Which of these best defines "longshore drift"?

The zigzag movement of sediment along a beach, driven by waves approaching the shore at an angle.

Why might managed retreat be chosen over a sea wall for farmland?

Farmland is low value, so an expensive wall is hard to justify; managed retreat is cheaper, creates natural habitats like salt marsh, and works with coastal processes.
Key takeaways
  • Erosional Landforms: trace the sequence from crack to cave to arch to stack to stump.
  • Waves come in two types: Destructive waves are tall, steep and frequent, with a powerful backwash that drags sediment down the beach — they erode.
  • fetch: The distance wind travels over open water — a longer fetch builds larger, more powerful waves.
  • Watch out for: saying longshore drift moves sediment straight along the beach