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CCEA A-level Geography ยท A2 1 Option C ยท Dynamic Coastal Environments
Mini-Lesson

A2 Option: Dynamic Coastal Environments

This mini-lesson covers A2 1 Option C - Dynamic Coastal Environments: coastal processes and features, regional coastlines of submergence and emergence and the threat of rising sea levels, and coastal management and sustainability (hard and soft engineering, EIA, CBA, sediment cells and Shoreline Management Plans).

This is one of four A2 1 options; you study two. Answer each question to unlock the next screen. Press Start.

Coastal processes and features

Waves, erosion and transport

Waves shape the coast through wave action, refraction, erosion and transport. Swash-aligned coasts face the waves head-on; drift-aligned coasts move sediment along by longshore drift.

  • High-energy coasts (erosion) create headlands, cliffs, arches, stacks and stumps.
  • Low-energy coasts (deposition) create beaches, dunes, spits, tombolos and bars.

Wave refraction concentrates energy on headlands and disperses it in bays, driving differential erosion.

Quick check

Refraction and headlands

?Why does wave refraction cause headlands to erode faster than adjacent bays?
Calculate

Calculate โ€” cliff recession rate

1A cliff has retreated 60 m over 40 years. Calculate the mean annual recession rate.
m/yr
Hint: recession rate = 60 รท 40.
Calculate

Calculate โ€” spit sediment supply

2Longshore drift moves 18 000 m³ of sediment past a point in 3 years. Calculate the mean annual sediment transport.
mยณ/yr
Hint: 18 000 รท 3.
Regional coastlines

Submergence, emergence and sea-level rise

Sea level changes over time. Eustatic change is a global change in sea level; isostatic change is local land rising or sinking (for example after ice melts).

  • Coasts of submergence (sea rises relative to land): fjords and rias (drowned valleys).
  • Coasts of emergence (land rises relative to sea): raised beaches and relict landforms.

CCEA requires a regional or national study of a coastline threatened by sea-level rise in an LEDC (for example Kiribati), treated qualitatively.

Sort it

Sort the coastal strategy

Tap a term, then tap its category.

๐Ÿงฑ Hard engineering

๐Ÿ–๏ธ Soft engineering

๐ŸŒŠ Coastal process

Quick check

Eustatic vs isostatic

?Melting ice sheets add water to the oceans worldwide. This is an example of:
Coastal management

Engineering and management tools

Coastal management balances protection, cost and sustainability using Environmental Impact Assessment (EIA), Cost-Benefit Analysis (CBA), sediment cells and Shoreline Management Plans (SMPs).

  • Hard engineering - sea walls, revetments, rip-rap, gabions, groynes. Effective but costly and can worsen erosion downdrift.
  • Soft engineering - beach nourishment, dune regeneration, managed retreat. Cheaper and more sustainable, working with natural processes.

CCEA uses a regional case study employing both hard and soft strategies (for example South Devon and Dorset), evaluated qualitatively.

Match it

Match the coastal landform

Tap an item on the left, then its matching partner on the right.

Landform
Origin
Quick check

Groyne side-effect

?Building groynes to trap sediment on one beach often causes what problem further along the coast?
Quick check

Managed retreat

?Managed retreat is considered a sustainable option because it:
Recap

The big ideas to know

Processes: wave action, refraction, erosion, transport; swash- and drift-aligned coasts; longshore drift

Features: high-energy - headlands, cliffs, arches, stacks; low-energy - beaches, dunes, spits, tombolos, bars

Regional: eustatic vs isostatic; submergence (fjords, rias), emergence (raised beaches); sea-level rise threat

Management: EIA, CBA, sediment cells, SMPs; hard vs soft engineering and their sustainability

You have covered A2 1 Option C. Press Finish for your score.

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Mini-lesson complete!

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