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Understanding Coastal Dynamics and Formations
May 13, 2025
Introduction to Coasts - GCSE Course by Job Rafik
Key Terms
Constructive Wave
Destructive Waves
Fetch
Swash
Backwash
Longshore Drift
Concordant Coastline
Discordant Coastlines
Bay
Cove
Beaches
Deposition
Clips and Erosion
Waves and Their Influence
Waves significantly shape the UK's coastline.
Causes of Waves:
Generated by wind blowing over sea surface.
Influenced by:
Duration of wind blowing.
Wind strength.
Distance wave travels (Fetch).
Wave Movements:
Swash:
Movement of waves up the beach.
Backwash:
Movement of waves back down the beach.
Types of Waves
Destructive Waves
Formed under stormy conditions.
Larger and more powerful.
High energy with long fetch.
Stronger backwash than swash, leading to erosion.
Characterized by:
High and steep shape.
Short length.
Constructive Waves
Formed in calmer weather.
Less energy compared to destructive waves.
Deposit materials on shore.
Stronger swash than backwash.
Characterized by:
Long length and short height.
Smooth and almost flat appearance.
Longshore Drift
Movement of sediment along the coast by wave action.
Occurs when swash comes in at an angle and backwash goes straight out.
Direction follows prevailing wind.
Important to draw and annotate correctly in diagrams.
Coastal Formations
Concordant Coastlines
Layers of different rock types parallel to the coast.
Harder rock acts as a barrier to softer rock.
Cove Formation:
Formed when a hard rock layer is breached.
Joints enlarge due to erosion.
Softer rock is eroded faster.
Example: Lulworth Cove, Dorset.
Discordant Coastlines
Bands of rock types perpendicular to the coast.
Formation of Headlands and Bays:
Headlands: Harder rock erodes slower.
Bays: Softer rock erodes quicker through hydraulic action, solution, and abrasion.
Cliffs
Found along the coastline.
Formation:
Soft rock erosion forms gentle slopes.
Hard rock creates steep cliffs.
Beaches
Formed through deposition.
Types: Sand, pebble, shingle, mud.
Constructive waves build beaches.
Beach Profile:
Sand beaches gently slope.
Shingle/pebble beaches have steeper profiles.
Sediment transportation involves longshore drift.
Larger sediment at the top due to constructive waves' inability to pull it back.
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