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 cliffs, on both sides of the town of Dover in Kent, stretch for eight miles (13 km). The White Cliffs of 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 cliffs, on both sides of the town of Dover in Kent, stretch for eight miles (13 km). The White Cliffs of Dover form part of the North Downs. The cliffs are part of the Dover to Kingsdown Cliffs Site of Special Scientific Interest and Special Area of Conservation. The top of the cliffs hosts a chalk grassland ecosystem with an abundance of bird, flower, and butterfly species. The cliffs mark the point where Great Britain is closest to continental Europe; on a clear day the cliffs are visible from France, approximately 20 miles (32 km) away. A celebrated UK landmark, their striking appearance has met visitors since ancient times. Julius Caesar remarked upon their appearance when he invaded Britain in 55 BC. The cliffs served as a natural defensive barrier, reinforced by the building of Dover Castle in the 11th century. The cliffs gained symbolic importance during World War II, as a symbol of Britain's resolute defence and as a welcome sight for the evacuees from Dunkirk. The… South Foreland Lighthouse is a Victorian-era lighthouse on the South Foreland in St. Margaret's Bay, which was once used to warn ships approaching the nearby Goodwin Sands. Goodwin Sands is a 10-mile-long (16 km) sandbank at the southern end of the North Sea lying six miles (10 km) off the Deal coast. The area 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 cliffs, on both sides of the town of Dover in Kent, stretch for eight miles (13 km). The White Cliffs of Dover form part of the North Downs. The cliffs are part of the Dover to Kingsdown Cliffs Site of Special Scientific Interest and Special Area of Conservation. The top of the cliffs hosts a chalk grassland ecosystem with an abundance of bird, flower, and butterfly species. The cliffs mark the point where Great Britain is closest to continental Europe; on a clear day the cliffs are visible from France, approximately 20 miles (32 km) away. A celebrated UK landmark, their striking appearance has met visitors since ancient times. Julius Caesar remarked upon their appearance when he invaded Britain in 55 BC. The cliffs served as a natural defensive barrier, reinforced by the building of Dover Castle in the 11th century. The cliffs gained symbolic importance during World War II, as a symbol of Britain's resolute defence and as a welcome sight for the evacuees from Dunkirk. The cliffs are part of the coastline of Kent in England between approximately 51°06′N 1°14′E and 51°12′N 1°24′E, at the point where Great Britain is closest to continental Europe – the Strait of Dover is approximately 20 miles (32 km) across. On a clear day, South Foreland Lighthouse is a Victorian-era lighthouse on the South Foreland in St. Margaret's Bay, which was once used to warn ships approaching the nearby Goodwin Sands. Goodwin Sands is a 10-mile-long (16 km) sandbank at the southern end of the North Sea lying six miles (10 km) off the Deal coast. The area consists of a layer of fine sand approximately 82 ft (25 m) deep resting on a chalk platform belonging to the same geological feature that incorporates the White Cliffs of Dover. More than 2,000 ships are believed to have been wrecked on the Goodwin Sands because they lie close to the major shipping lanes through the Straits of Dover. It went out of service in 1988 and is now owned by the National Trust for Places of Historic Interest or Natural Beauty. The cliffs have great symbolic value in Britain because they face towards continental Europe across the narrowest part of the English Channel (approximately 20 miles (32 km) between coasts), where invasions have historically threatened and against which the cliffs form a symbolic guard. The National Trust calls the cliffs "an icon of Britain", with "the white chalk face a symbol of home and wartime defence." Because crossing at Dover was the primary route to the continent before the advent of air travel, the white line of cliffs also formed the first or last sight of Britain for travellers. During the Second World War, thousands of allied troops on the little ships in the Dunkirk evacuation saw the welcoming sight of the cliffs. In the summer of 1940, reporters gathered at Shakespeare Cliff to watch aerial dogfights between German and British aircraft during the Battle of Britain. Vera Lynn, known as "The Forces' Sweetheart" for her 1942 wartime classic "(There'll Be Bluebirds Over) The White Cliffs of Dover" celebrated her 100th birthday in 2017. That year she led a campaign for donations to buy 170 acres (0.7 km2) of land atop Dover's cliffs when it was feared that they might be sold to developers; the campaign met its target after only three weeks. The National Trust, which owns the surrounding areas, plans to return the land to a natural state of chalk grassland and preserve existing military structures from the Second World War. In June 2021, a wildflower meadow on White Cliffs of Dover was named in honour of Dame Vera Lynn. Aerial view of the cliffs and surrounding area on YouTube Dover Museum information on the cliffs White Cliffs of Dover website

On the shore of the English Channel, half hidden by its shady grove of trees, stands Walmer Castle, the sweet red roses trailing up the ramparts and clustering in lovely bouquets round its cannon, emblematic of the peaceful end of him—illustrious Wellington—whose last breath ceased within those grey stone walls.From this lonely beach, against whose front the “wild waves ceaseless play,” creating their own barrier in the great banks of shingle which ceaselessly they raise, we look out upon the fleet of vessels in the Downs, and far beyond the long white line of surf—the shroud of many a noble heart—that marks the Goodwin Sands, is seen the distant coast of France.From Walmer,the “white cliffs of Albion,” so conspicuous here for their numerous and regular bands of flints, gradually rise towards Dover, whose far-famed castle stands on a mountain mass of microscopic shells, overlooking the red-roofed tenements of that ancient port, winding along the deep valley which at this point cuts abruptly through the strata.The opposite hill is furrowed in its entire extent with the trenches of the citadel, and at the foot of its steep cliff is the long and narrow street which formerly, when the town was walled, led to the Snaregate.

AbstractWhere beaches and harbors have frequently been taken to signify openness and intermingling, a different coastal setting, the cliffs of Dover, overtly bespeaks opposition and closure. Demarcating the British coast at its closest point to continental Europe, the cliffs often stand for Britain’s supposedly elemental insularity. However, the chalk composing the cliffs makes them, in their own way, as malleable and permeable as a beach. I argue that poems by Matthew Arnold, W. H. Auden, and Daljit Nagra contest the cliffs’ association with an exclusive Britishness by focusing on their material composition. In these poems, the cliffs’ chalk—formed by fossilized marine microorganisms at a time when what would become Britain was at the bottom of a prehistoric sea—attests to Britain’s geohistorical contingency. Arnold, Auden, and Nagra use this chalk geology to develop a new model of British identity as contingent, permeable, and linked with the wider world. In these poems, that is, Dover’s cliffs collapse oppositions rather than enforcing them: they blur the lines between Britain and the world, past and present, organic and inorganic, human history and geological history. The literature of the Dover cliffs thus highlights the revisionary potential of this distinctive kind of littoral space.