Weathering Processes - Geography

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  • Created by: bbaiton
  • Created on: 18-01-18 19:14

Freeze-thaw

  • Water collects in cracks or holes (pores) in the rock.
  • At night this water freezes and expands and makes cracks in the rock bigger.
  • When the temperature rises and the ice thaws, water will seep deeper into the rock.
  • After repeated freezing and thawing, fragments of rock may break off and fall to the foot of the cliff (scree)
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Salt Weathering

  • Seawater contains salt. When the water evaporates it leaves behind salt crystals.
  • In cracks and holes these salt crystals grow and expand
  • This puts pressure on the rocks and flakes may eventually break off.
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Carbonation

  • Rainwater absorbs CO2 from the air and becomes slightly acidic.
  • Contact with alkaline rocks such as chalk and limestone produces a chemical reaction causing the rocks to slowly dissolve.
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