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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 .
On a clear day, it is possible to see the opposite coastline of England from France and vice versa with the naked eye, with the most famous and obvious sight being the White Cliffs of Dover from the French coastline and shoreline buildings on both coastlines, as well as lights on either coastline at night, as in Matthew Arnold's poem "Dover Beach".
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 ...
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 ...
The Port of Dover and the White Cliffs of Dover. The Dover Harbour Board [21] is the responsible authority for the running of the Port of Dover. The English Channel, here at its narrowest point in the Straits of Dover, is the busiest shipping lane in the world. Ferries crossing between here and the Continent have to negotiate their way through ...
Capel-le-Ferne / ˌ k eɪ p əl l ə ˈ f ɜːr n / is a village on the White Cliffs of Dover, near Folkestone in Kent, England. Its name derives from a medieval French term meaning "chapel in the ferns". In 2011 the village had a population of 1,884. [1] It is perched on top of the White Cliffs of Dover.
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The area consists of a layer of approximately 25 m (82 ft) depth of fine sand resting on an Upper Chalk platform belonging to the same geological feature that incorporates the White Cliffs of Dover. The banks lie between 0.5 m (1 ft 8 in) above the low water mark to around 3 m (10 ft) below low water, except for one channel that drops to around ...