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The White Cliffs of Dover are the region of English coastline facing the Strait of Dover and France. The cliff face, which reaches a height of 350 feet (110 m), owes its striking appearance to its composition of chalk accented by streaks of black flint , deposited during the Late Cretaceous .
It forms the famous White Cliffs of Dover in Kent, England, as well as their counterparts of the Cap Blanc Nez on the other side of the Dover Strait. The Champagne region of France is mostly underlain by chalk deposits, which contain artificial caves used for wine storage. [3] Some of the highest chalk cliffs in the world occur at Jasmund ...
The Seven Sisters cliffs are occasionally used in filmmaking and television production as a stand-in for the more famous White Cliffs of Dover, since they are relatively free of anachronistic modern development and are also allowed to erode naturally. As a result, the Seven Sisters and Beachy Head remain a bright white colour, whereas the White ...
Some of the best exposures of the Chalk are where these ranges intersect the coast to produce dramatic, often vertical cliffs as at Flamborough Head, the White Cliffs of Dover, Seven Sisters, Old Harry Rocks (Purbeck) and The Needles on the Isle of Wight.
The White Cliffs of Dover, Kent, made of chalk of Cretaceous age. The geology of England is mainly sedimentary.The youngest rocks are in the south east around London, progressing in age in a north westerly direction. [1]
It takes its name from the white hue of its high chalk cliffs, including those of Étretat, which stretch for over 120 km, dominating most of the coastline. It is part of the same geological system as the White Cliffs of Dover on the far side of the English Channel.
The white cliffs of Dover as seen from Cap Gris-Nez. The Straits of Dover were carved out of the anticline surface layer, presumably chalk, by glacial lake outburst floods. The Strait of Dover is geologically speaking a very young feature, which cuts through the much older Weald–Artois Anticline. The anticline continues uninterrupted in the ...
At the beginning of the Late Cretaceous, around 100 million years ago, deposition changed to that of chalk, with the deposition of the Chalk Group continuing until the end of the Cretaceous. Chalk was deposited over much of Great Britain, now notably exposed at the White Cliffs of Dover and the Seven Sisters, and also forming Salisbury Plain ...