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The song included the line "Wandering I am lost, as I travel along the White Cliffs of Dover." The 1941 song "(There'll Be Bluebirds Over) The White Cliffs of Dover" is a popular World War II song composed by Walter Kent to lyrics by Nat Burton. It was made famous by Vera Lynn's 1942 version. The White Cliffs have long been a landmark for sailors.
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]
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 ...
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. The high sea levels left only small areas of land exposed, which accounts for the general lack of land-origin sand, mud or clay sediments found from around this time.
The lower stratigraphic units of the chalk cliffs of Dover consist of a sequence of glauconitic marls followed by rhythmically banded limestone and marl layers. [8] Such alternating cycles of chalk and marl are common in Cretaceous beds of northwestern Europe. [9] The Channel Tunnel follows these marl layers between France and the United ...
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 eastern part of the Wealden dome was eroded away by the sea. The White cliffs of Dover occur where the North Downs meets the coast. From there to Westerham is now the Kent Downs Area of Outstanding Natural Beauty. [6] The chalk displays all its characteristic features such as steep sided dry valleys, and sunken roads. [5] 'The White Cliffs ...
Samphire Hoe is a country park situated 2 miles (3 km) west of Dover in Kent in southeast England. The park was created by using 4.9 million cubic metres of chalk marl from the Channel Tunnel excavations and is found at the bottom of a section of the White Cliffs of Dover. [1]