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Understanding Coastal Landscapes and Processes

Jun 4, 2025

Coastal Landscapes for A-Level Geographers

Key Terminology

  • Backshore: Area between high watermark and lambwood limit.
  • Foreshore: Area between high watermark and low watermark.
  • Inshore: Area between low watermark and the point where waves don't influence.
  • Offshore: Point beyond where waves cease to impact the seabed.

Coastal Systems

  • Coasts viewed as systems with:
    • Flows: Links between stores.
    • Inputs: Addition of matter such as wind, waves, sea currents, and tides.
    • Stores: Where energy is kept.

Waves

  • Friction on seabed slows the wave; crest continues forward.
  • Swash: Wave rushes up the beach.
  • Backwash: Wave returns to the sea.
  • Constructive Waves:
    • Low wave height, low frequency.
    • Strong swash, weak backwash.
  • Destructive Waves:
    • High wave height, high frequency.
    • Strong backwash, leads to erosion.

Wave Refraction

  • Waves bend and refract towards shallower water influencing erosion and deposition.

Transportation Processes

  • Longshore Drift: Sediment movement due to angled waves.
  • Rip Currents: Strong currents moving away from the shore.

Tides

  • Definition: Periodic rise and fall of sea level.
  • Types:
    • Spring Tide: Just after new/full moon.
    • Neap Tide: Just after first/third quarters of the moon.
  • Tidal Range: Difference between high and low tide.

Coastal Energy

  • High Energy Coastlines: High wave energy, increased erosion.
  • Low Energy Coastlines: Lower wave energy, increased deposition.

Coastal Processes

  • Marine Processes: Erosion, transportation, deposition.
  • Sub-Aerial Processes: Weathering, mass movement.

Landforms

  • Caves, Arches, Stacks, Stumps: Result from erosion processes.
  • Wave-Cut Notches and Platforms: Features to explain formation.
  • Minor Landforms: Runnels and cusps on beaches.

Spit and Bar Formation

  • Simple Spit: Parallel to coast; Compound Spit: Hooked.
  • Bar: Ridge of sand/shingle joining headlands, creating lagoons.

Mud Flats and Salt Marshes

  • Form from fine sediment in sheltered areas.
  • Factors: River estuary, saltwater, and flows meeting.

Sea Level Change

  • Eustatic: Change due to water volume/ ocean basin shape.
  • Isostatic: Land movement relative to sea.

Submergent and Emergent Coastlines

  • Submergent: Coastlines inundated by sea rise (e.g., Rias, Fjords).
  • Emergent: Coast exposed due to falling sea level (e.g., Raised Beaches).

Coastal Management

  • Aims: Defense against flooding, coastal erosion protection.
  • Shoreline Management Plans: Sustainable management, considering different scales and local contexts.

Integrated Coastal Zone Management (ICZM)

  • Originated from UN Earth Summit 1992.
  • Considers local, regional, national authority input.
  • Example: Pevensey Bay strategy for longshore drift and coastal erosion.

Case Study: Sunderbans

  • Delta of the Ganges, threatened by climate change.
  • Risks: Cyclones, flooding, salinity, over-exploitation.
  • Management Strategies:
    • Resilience: Coping strategies.
    • Mitigation: Reducing hazard severity.
    • Adaptation: Adjusting living conditions.

Exam Preparation

  • Understand AO1 content and develop critical thinking for exams.

Note: Be familiar with diagrams and processes related to each concept and landform for better understanding and application in exams.