Recently weathered rock can be seen at the foot of chalk and limestone cliffs and is easily identified because it is angular.

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Weathering is the breakdown of rock in situ by the action of rainwater, extremes of temperature, and biological activity.

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Chemical weathering is the breakdown of rock through changing its chemical composition.

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Mechanical weathering is the breakdown of rock without changing its chemical structure (composition).

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When rainwater hits rock it decomposes it or eats it away. This is known as carbonation. This occurs when slightly acidic (carbonic) rain or seawater comes into contact with sedimentary rock, such as limestone or chalk, it causes it to dissolve. A chemical reaction occurs between the acidic water and the calcium carbonate and forms calcium bicarbonate. This is soluble and is carried away in solution. Carbonation weathering occurs in warm, wet conditions.

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