2.2.6

Discordant & Concordant Coastlines

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Main Landforms of Discordant and Concordant Coastlines

The formation of discordant and concordant coastlines results in different landforms based on rock type orientation and erosion processes.

Discordant coastlines

Discordant coastlines

  • Discordant coastlines occur where bands of hard and soft rock run perpendicular to the coast.
    • Softer rocks erode faster, forming bays.
    • Harder rocks resist erosion, creating headlands that project into the sea.
    • This contrast shapes jagged coastlines with clear landforms.
Landforms of discordant coastlines

Landforms of discordant coastlines

  • Bays form where soft rock erodes quickly, making wide, sheltered inlets.
  • Headlands are steep, rocky areas of hard rock standing out from the coast.
  • Cliffs and wave-cut platforms often develop at headlands.
  • Wave refraction causes erosion to concentrate on headlands.
Concordant coastlines

Concordant coastlines

  • Concordant coastlines have rock strata running parallel to the coast.
    • The sea erodes outer hard rock layers first.
    • Softer rock layers behind may form coves or inlets once exposed.
    • This process often creates smoother, more uniform coastlines.
Landforms of concordant coastlines

Landforms of concordant coastlines

  • Coves develop where the sea breaks through hard outer rock to erode softer rock inside.
    • Coves are typically circular or oval, with narrow entrances.
    • The cove formation creates sheltered, calm water areas.
    • Hard rock layers protect most of the coast, limiting wider erosion.
Comparing types of coastlines

Comparing types of coastlines

  • Discordant coastlines create alternating headlands and bays due to varying rock resistance.
  • Concordant coastlines feature fewer indentations with coves formed behind hard layers.
  • Wave energy dissipates differently on each.
    • This knowledge helps explain coastal shape and erosion patterns.
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