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.