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Chalk
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Chalk is relatively resistant to erosion and slumping compared to the clays with which it is usually associated, thus forming tall steep cliffs where chalk ridges meet the sea. Chalk hills, known as chalk downland, usually form where bands of chalk reach the surface at an angle, so forming a scarp slope. Because chalk is porous it can hold a large volume of ground water, providing a natural reservoir that releases water slowly through dry seasons. . Chalk has been quarried since prehistory, providing building material and marl for fields. In southeast England, deneholes are a notable example of ancient chalk pits. The Chalk Formation is a European stratigraphic unit deposited during the late Cretaceous Period. It forms the famous White Cliffs of Dover in Kent, England. The Champagne region of France is mostly underlain by chalk deposits, which contain famous caves beneath the hills. Chalk usesThe traditional uses of chalk have in many cases been replaced by other substances, although the word "chalk" is often still applied to the replacements.
See also
Categories: Limestone | Sedimentary rocks | Alchemical substances |
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| This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Chalk". A list of authors is available in Wikipedia. | ||||||||||||||||||||
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