Erosional processes

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  • Created by: Neha_mali
  • Created on: 13-01-20 12:22
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  • erosional processes
    • how they are influenced by:
      • wave type
        • constructive
          • strong swash, weak back wash
          • low wave height, long wavelength
          • low frequency
          • depositional
            • drops more sediment than it erodes
          • low energy coastline associated w/ weaker waved, deposition exceeds the rate of erosion
        • destructive
          • strong backwash, weak swash
          • high wave height, short wavelength
          • high frequency
          • erosional
            • erodes more than it deposits
          • high energy coastline associated w/ powerful waves, erosion rate increase
      • size
        • sediment
          • smaller sediment more evident where more erosion has occurred, visa versa
        • waves
          • high energy waves have a high wave height and short wavelength
          • low energy waves have a low wave height but long wavelength
      • lithology
        • permeable
          • allows water to easily flow through meaning it erodes in the gaps as well as outside
        • weaknesses
          • weaknesses
            • water can get into cracks and erode out, increases erosion
          • not many weaknesses
            • few cracks so harder for water to enter and erode, decreases erosion
        • reactivity
          • highly reactive
            • more suceptible to chemical weathering e.g. limestone
        • clastic or crystalline?
          • clastic
            • made up of smaller rocks broken rocks that erode more easily
          • crystaline
            • have interlocking crystals that are harder to erode
    • erosional features created
      • wave cut notch and platforms
        • marine erosion attacks base of a cliff
        • notch of eroded material between high and low tide height is created
        • as notch deepens the cliff face becomesunstable
          • falls under its own weight through mass movement
        • platform of unaffected cliff base under notch is left behind
      • cliffs
        • through process of repeat wave-cut notches and platforms, new cliff faces are created whilst last retreats
      • cave-arch-stack stump sequence
        • occurs on pinnacle headlands
        • marine erosion widens faults in base of headland, widening over time to form cave
        • cave widens due to marine erosion & sub-oriel processes
          • erodes to the other side of the headland, creates an arch
        • arch keeps widening till is can't support itself
          • falls under its own weight, leaving a stack
          • one side of arch gets detached from mainland
        • marine erosion at the back of the stack, it will eventually collapse into a stump
    • processs
      • hydraulic action
        • this is the power of the waves when they hit a cliff
        • air is forced into the cracks the rock causing them to break apart
      • attrition
        • rock fragments in the sea knock against each other getting smaller
      • abrasion
        • pebbles grind over a rocky platform getting smoother
      • corrasion
        • fragments of rock are picked up and thrown at cliffs eroding the rock

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