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White_Cliffs_of_Dover

The White Cliffs of Dover

The White Cliffs of Dover are one of the most iconic natural landmarks in the United Kingdom, located in the county of Kent, on the southeastern coast of England. These cliffs are part of the English Channel coastline and stretch approximately 8 miles from Dover to Kingsdown.

Geological Formation

The cliffs are composed primarily of chalk, which is a soft, white, porous limestone made from the accumulation of microscopic planktonic algae known as coccoliths over millions of years. This chalk was formed during the Cretaceous period, around 70 to 100 million years ago, when the area was submerged beneath a shallow sea. Over time, the sea receded, leaving behind layers of sediment that have since compacted into the chalk cliffs we see today.

Historical Significance

Environmental Concerns

Over the years, the White Cliffs of Dover have faced environmental challenges:

Tourism

The White Cliffs of Dover are a major tourist attraction:

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