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Weathering

Weathering is the breakdown of rocks in situ. It can be broken down into mechanical weathering, biological weathering and chemical weathering.

Mechanical (freeze-thaw)

Mechanical (freeze-thaw)

  • Mechanical (freeze-thaw) weathering is caused by drops in temperatures, especially during the evenings in the winter.
  • Rocks break down because the water expands and contracts as the water freezes and melts, putting pressure on the rock.
Biological

Biological

  • Biological weathering is when the roots of plants grow inside the rock, causing it to crack and break apart.
  • It can also be when animals burrow inside the rock.
Chemical

Chemical

  • Chemical weathering happens because rainwater can be slightly acidic.
  • The weakly acidic rainwater causes the breakdown of particular rocks over time.
Jump to other topics
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Physical Geography

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