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The Strait of Dover or Dover Strait, [a] historically known as the Dover Narrows, is the strait at the narrowest part of the English Channel, marking the boundary between the Channel and the North Sea, and separating Great Britain from continental Europe.
The Strait of Dover viewed from France, looking towards England. The white cliffs of Dover on the English coast are visible from France on a clear day. The Strait of Dover (French: Pas de Calais), at the Channel's eastern end, is its narrowest point, while its widest point lies between Lyme Bay and the Gulf of Saint Malo, near its midpoint. [3]
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 .
The Channel Tunnel (French: Tunnel sous la Manche), sometimes referred to by the portmanteau Chunnel, [3] [4] is a 50.46 km (31.35-mile) undersea railway tunnel, opened in 1994, that connects Folkestone (Kent, England) with Coquelles (Pas-de-Calais, France) beneath the English Channel at the Strait of Dover.
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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 subsurface of the Strait of Dover and English Channel.
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Sele Strait (a.k.a. Galowa Strait, Revenges Strait) – between Salawati and New Guinea; Serpent's Mouth (Boca de la Serpiente) – between Trinidad and Venezuela; Shelikof Strait – between the Alaska mainland to the west and Kodiak and Afognak islands to the east, in the USA; Sibutu Passage – between Borneo and the Sulu Archipelago