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"The cliffs (of Dover on the Brittish Coast) themselves are still under attack from the sea as its continuous flow eats away at the soft chalk at the base of the cliffs. About 2-5cm on average are lost each year, but more than a metre can be lost in one large cliff fall, and as sea-levels rise the cliffs will probably retreat more quickly"...National Trust

http://www.nationaltrust.org.uk/main/w-index.htm

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13y ago
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13y ago

Chalk formations (e,g, The White Cliffs of Dover) erode easily for several reasons:

  • Chalk is a friable rock, it breaks apart easily under mechanical stress (heating and cooling, freezing and thawing, things rubbing against it)
  • Chalk is chemically reactive, acidic rains (even normal rain) dissolves it
  • Chalk absorbs water making it break up on freezing
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12y ago

because chalk is pourus(has lots of holes) and therefore, if lots of holes fill up with enough water and freeze repeatedly, more of the chalk will fall off as scree.

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Q: Why is chalk vulnerable to freeze thaw weathering?
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