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Which rock forms the greater part of the White Cliffs of Dover?

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The White Cliffs of Dover are primarily made up of a type of limestone called chalk. Chalk is a soft, white, porous sedimentary rock that is composed of the skeletal remains of microscopic marine organisms such as coccoliths and foraminifera. The White Cliffs of Dover are one of the most famous landmarks in England and are located on the coast of southeastern England, facing the English Channel. The cliffs are formed from layers of chalk that were deposited over millions of years during the Cretaceous period, and have been shaped by erosion and weathering over time.
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The greater part of the White Cliffs of Dover is made up of chalk. Chalk is a soft, white sedimentary rock composed of the shells of microscopic marine organisms. It is formed from the accumulation of these shells over millions of years, and is highly resistant to erosion.
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The greater part of the White Cliffs of Dover is formed by a type of limestone called chalk. This chalk was formed from tiny marine organisms that lived in the sea over 65 million years ago. The layered chalk formations create the characteristic white cliffs visible from the English Channel.
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