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Weathering

Weathering and erosion constantly attack rocks. Weaker rocks are weathered faster than harder, stronger, more resistant rocks.

Biological weathering

Biological weathering

  • Biological weathering happens when plants or animals break down rocks.
  • For example, trees roots can grow into cracks in rocks and split the rocks apart as the roots grow.
  • Animals can wear rocks down as they burrow into cavities.
Chemical weathering

Chemical weathering

  • In chemical weathering, the chemical composition of rock changes.
  • When the climate is warm and wet, carbonic dioxide can dissolve in rain to create a 'carbonic acid'.
  • The carbonic acid in rainfall hits rocks and dissolves the parts of the rock made of calcium carbonate.
Freeze-thaw weathering

Freeze-thaw weathering

  • Water expands when it freezes.
  • When water fills cracks in rocks, if it then freezes, it expands, putting pressure on the rock.
  • The water will then melt, but it has put pressure on the rock.
  • Eventually, this process of freezing and thawing will wear down the rock until it cracks.
Onion-skin weathering

Onion-skin weathering

  • Onion-skin weathering is when the outer layer separates from the rock.
  • One form of this weathering is exfoliation, where the outer layer of the rock is peeled off by the weather.
Onion-skin weathering cont.

Onion-skin weathering cont.

  • Rocks expand during the day in very hot temperatures and then contract again in the cooler night-time temperatures.
  • This constant movement over thousands of years finally causes the outer layer to peel away.
  • The process then repeats with the next layer.
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