coastal revision notes
Coastal Environments Overview
Coastal environments consist of various ecosystems and physical processes.
Key topics include coastal processes, ecosystems, threats, and management strategies.
2.1 Coastal Processes & Landforms
2.1.1 Coastal Processes
Definition: Coastal processes shape the land along coastlines and are influenced by interactions between terrestrial and marine systems.
Types:
Marine processes (offshore)
Terrestrial processes (onshore)
Key Activities:
Wave action
Erosion
Transportation
Weathering
Mass movement
Wave Action
Role of Waves: Waves erode, transport, and deposit materials along the coast.
Formation Factors:
Fetch: Distance over which wind blows across water.
Wind strength and duration: Affect wave height.
Wave Types:
Destructive Waves: Short wavelength, steep, strong backwash, erode beaches.
Constructive Waves: Long wavelength, gentle, strong swash, build beaches.
Erosion Mechanisms
Destructive Wave Erosion Types:
Hydraulic Action: Water pressure in cracks of rocks.
Attrition: Rocks and stones collide and break apart.
Corrosion: Chemical action dissolving rocks.
Abrasion: Erosion through the movement of particles hitting the shore.
Tip: Differentiate between abrasion and attrition for exam success.
Transportation Processes
Materials arrive in coastal waters through several means:
Eroded cliffs
Longshore drift
River transport
Longshore Drift:
Waves approach at an angle; swash moves material up the beach while backwash returns it down.
Results in zig-zag movement along the coastline.
Weathering Processes
Definition: Breakdown of rocks without movement.
Types:
Mechanical: Freeze-thaw cycles causing rock fragmentation.
Chemical: Reactions with acidic rainwater.
Biological: Plant roots expanding in rock crevices.
2.1.2 Coastal Landforms
Headlands and Bays
Formation: Alternating layers of resistant and less resistant rock.
Bays: Formed by erosion of softer rock, creating sheltered areas.
Headlands: More resistant rock remains protruding into sea.
Coves and Cliffs
Coves: Circular bays formed by erosion of softer rocks behind harder rocks.
Cliffs: Formed by weathering and erosion processes leading to steep faces and wave-cut platforms.
Caves, Arches, Stacks, and Stumps
Caves evolve through hydraulic action and abrasion.
Arches result from continuous erosion, eventually collapsing into stacks (isolated columns of rock) and stumps (eroded stacks).
2.1.3 Coastal Environmental Change
Influences of Geology and Vegetation
Geology: Soft rocks erode faster creating low land; resistant rocks create rugged landscapes.
Vegetation: Stabilizes features like sand dunes increasing resilience to erosion.
Sea-level Changes
Rising Sea Levels: Cause submergent coastlines with features like rias and fjords.
Falling Sea Levels: Result in emergent coastlines with raised beaches and cliffs.
2.2 Ecosystems of the Coastline
2.2.1 Coastal Ecosystems of the World
Coral Reefs: Warm, shallow waters; biodiversity hotspot; crucial for marine life.
Mangroves: Tolerate salt; stabilize coastlines; provide habitats.
Characteristics of Ecosystems
Factors influencing distribution:
Temperature, light, water depth, salinity, and wave action.
Coral Reef Types:
Fringing, barrier, and atolls, each with unique growth patterns and conditions.
2.3 Management of Coasts
2.3.1 Conflict at the Coast
Various stakeholders have competing interests in coastal areas leading to conflict over resources.
2.3.2 Coastal Flooding
Causes: Storm surges, tsunamis, king tides, and human factors.
Impacts mostly felt in emerging countries with significant economic costs in developed nations.
2.3.3 Coastal Management Strategies
Hard Engineering Methods: Concrete structures, sea walls, and groynes.
Soft Engineering Methods: Utilizing natural processes, beach replenishment, and managed retreat.
Importance of Integrated Coastal Zone Management (ICZM) for sustainability and stakeholder needs.