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Biological weathering is caused by the burrowing of animals as well as the growth of roots. Reputable information on biological weathering can be found on the BBC website under "Science" and many University Biology websites.

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Q: Where can one find more information on biological weathering?
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What is the difference between siliciclastic and chemical or biochemical sedimentary rocks?

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Where do you find chemical weathering more rapid?

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Which is not a factor that affects the rates of weathering in rocks?

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Biological Weathering of Rocks?

Biological weathering is caused by activities of living organisms - for example, the growth of roots or the burrowing of animals. Tree roots are probably the most occuring, but can often be by animals! Its where animals or roots prise the rock apart.This is more than roots digging in and wedging rocks. Biological weathering is the actual molecular breakdown of minerals. There are things called lichens (combinations of fungi and algae) which live on rocks. Lichens slowly eat away at the surface of rocks. The amount of biological activity that breaks down minerals depends on how much life is in that area. You might find more activities like lichens near oceans where the air is humid and cooler! Or for a short cut ask your daddy!


How does acid rain cause chemical weathering of rock?

1. Acids fom living things 2. Acid precipitation 3. Acids in groundwater Living things- When living things touch rock, some of the acids are transferred to the surface of the rock. Acid presipitation-Sometimes rain, sleet, or snow contains more acid than usual. Acids in groundwater-When ground water touches rock a reaction happens and it dissolves the rock which can cause caves.


What is biological of rocks?

Biological weathering is caused by activities of living organisms - for example, the growth of roots or the burrowing of animals. Tree roots are probably the most occuring, but can often be by animals! Its where animals or roots prise the rock apart.This is more than roots digging in and wedging rocks. Biological weathering is the actual molecular breakdown of minerals. There are things called lichens (combinations of fungi and algae) which live on rocks. Lichens slowly eat away at the surface of rocks. The amount of biological activity that breaks down minerals depends on how much life is in that area. You might find more activities like lichens near oceans where the air is humid and cooler! Or for a short cut ask your daddy!


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How does climate affect mechanical and chemical weathering?

Chemical weathering occurs more rapidly in warm, wet climates, and mechanical weathering occurs more in cold climates.