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Coastal Processes

Emily Pine

  • Waves
    •  Constructive - build up the beach, strong swash and weak backwash 
    • Destructive -destroy the beach, weak swash and strong backwash
  • Freeze-thaw Weathering
    • Water enters rocks
    • It freezes
    • Ice melts and goes deeper into the rock
    • Happens many times and the cracks become bigger
  • Biological Weathering
    • Roots enter rocks
    • Roots grow and make them wider
    • Rock breaks away
  • Chemical Weathering
    • Acid in the rain and sea water dissolve the rocks
  • Hydraulic Action - waves smash against the cliff causing it to breakdown
  • Abrasion - pebels grind agaisnt each other and become smooth
  • Attrition - rocks knock against each other causing them to break up
  • Solution - sea water dissolves rocks
  • Solution - dissolved materials are carried in the water
  • Suspension - small rocks flow with the water
  • Saltation - small rocks bounce along the sea bed
  • Traction - larger rocks roll along the sea bed
  • Longshore Drift 
    • Waves approach the sea at an angle due to the prevailing winds
    • Swash carries material onto the beach
    • This repeats in a zig zag formation causing a material build up
  • Deposition - when waves drop materials onto the beach

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