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The consequence of this was that Britain became an island. The counterbombardment and anti-aircraft gun fire was directed from a control room in the cliff complex. (Caesar's Commentaries, Book IV.). It is thought that the chalk was deposited very slowly, probably only half a millimetre a year, equivalent to about 180 coccoliths piled one on top of another. The White Cliffs date back over 136 million years, having formed during the Cretaceous period in the Mesozoic era as the shells and skeletons of billions of tiny sea creatures fell to the bottom of the sea. Looking up at the cliffs from Townwall Street, on the approach to the Eastern Docks, you can see signs of massive tunnelling works at various levels in the cliff below the Castle. ", Dover Museum Market Square Dover Kent CT16 1PH, Enquiries:Booking: [email protected]: [email protected], Monday to Saturday     9.30am-5pmClosed December 25th, 26th and 1st January, » Visitor Information» About the Museum» Friends of Dover Museum. The prosecutor had to double as executioner and throw the thief off the cliff. The White Cliffs of Dover The White cliffs hass an amazing Geology. Dit is een doorverwijspagina , bedoeld om de verschillen in betekenis of gebruik van White Cliffs of Dover inzichtelijk te maken. The bottom of the sea had been covered with white mud which formed from fragments of coccoliths, the skeletons of algae which floated in the surface waters and which sank to the bottom during the period of Cretaceous. Although the cliffs are famous for many reasons, it is perhaps their composition that makes them most interesting. The White Cliffs of Dover, 300 feet high above the English Channel in some places, draw thousands of visitors every year. The Cliffs have been immortalised in song, in literature and in art. Shakespeare's mention of samphire gatherers prompts a diversion from literature to an example of the plant life which abounds on the chalk grasslands and even on the cliff face. The first recorded description of Dover describes the scene that Julius Caesar saw in 55 BC when, with two legions of soldiers, he arrived near Dover looking for a suitable landing place for the Roman invasion. At that point steep cliffs came down close to the sea in such a way that it is possible to hurl weapons from them right down to the shore. The quartz silica filled cavities which has been left by dead marine creatures are generally found as flint fossils, especially moulds of Micrasterechinoids. The upper layer is a nodular chalk with flints. The sea bottom was made of a white mud formed from the fragments of coccoliths, which were the skeletons of tiny algae which floated in the surface waters of the sea. These sediments had been formed very slowly with only about a half of a milimeter adding up in an year which is equivalent to about 180 coccoliths piled on top of one another. As the fragments settled over hundreds of thousands of years, they formed layers of chalk, or soft white limestone, that became the cliffs. The latter part of the Ice Age also saw the invasion of chalk by the English Channel. With subsequent movements by the earth the Alps was formed and it raised the sea floor deposits above the sea level.

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