Strait of Dover

Coordinates: 51°00′N 1°30′E / 51.000°N 1.500°E / 51.000; 1.500
Source: Wikipedia, the free encyclopedia.

Dover Strait
View from France across the Strait of Dover towards the English coast
LocationNorth Sea–English Channel (Atlantic Ocean)
Coordinates51°00′N 1°30′E / 51.000°N 1.500°E / 51.000; 1.500
TypeStrait
Basin countriesFrance
United Kingdom
Min. width20 miles (32 km)
Average depth150 feet (46 m)

The Strait of Dover or Dover Strait (

cross-channel swimmers.[2] The entire strait is within the territorial waters of France and the United Kingdom, but a right of transit passage under the United Nations Convention on the Law of the Sea allows vessels of other nations to move freely through the strait.[3][4][5]

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".

Shipping traffic

Automatic Identification System
display showing traffic in the strait in 2006

Most maritime traffic between the Atlantic Ocean and the North Sea and

shipping lanes.[6]

In addition to the intensive north-east to south-west traffic, the strait is crossed from north-west to south-east by ferries linking Dover to Calais and Dunkirk.[4] Until 1994 these provided the only route across it except for air transport. The Channel Tunnel now provides an alternative route, crossing beneath the strait at an average depth of 45 m (148 ft) below the seabed.

The town of Dover gives its name to one of the sea areas of the British Shipping Forecast.

Geological formation

Map showing the hypothetical extent of Doggerland (c. 10,000 BCE), which provided a land bridge between Great Britain and continental Europe

The formation of strait was through scouring by

Cap Blanc Nez in France. The Channel Tunnel was bored through solid chalk – compacted remains of sea creatures and marine-deposited
, ground up calciferous rock/soil debris.

The

East Yorkshire, connecting to the Atlantic via the Pentland Firth
in the last glaciation (of over 300,000 years) is a necessary pre-condition for the relatively late cutting through of the Strait to the south.

NASA Satellite image
December 2002

Likewise, a 2007 study[8][9] concluded that the Strait was formed by erosion caused by two major floods. The first was about 425,000 years ago, when an ice-dammed lake in the southern North Sea overflowed and broke the Weald-Artois (Boulonnais) chalk range in a catastrophic erosion and flood event. Consequently the ice-age-muted flows from the Thames and Scheldt flowed through the gap into the English Channel/Inlet, but the Meuse and Rhine still flowed without any significant link to the inlet (such as today's IJssel distributary supports). In a second flood about 225,000 years ago supported by glaciers extending from areas then land such as the Zuiderzee, the Meuse and Rhine were ice-dammed into a lake that broke catastrophically through a high weak barrier (perhaps chalk, or an end-moraine left by the ice sheet). Both floods cut massive flood channels in the dry bed of the English Channel, somewhat like the Channeled Scablands or the Wabash River in the USA. A further update in 2017 attributed a series of previously described underwater holes in the Channel floor, "100m deep" and in places "several kilometres in diameter", to lake water plunging over a rock ridge causing isolated depressions or plunge pools.[10] The melting ice and rising sea levels submerged Doggerland, the area linking Britain to France, around 6,500–6,200 BCE.

The Lobourg strait, the deepest part the strait, runs its 6 km (4 mi)wide slash on a NNE–SSW axis. Nearer to the French coast than to the English, it borders the Varne sandbank (shoals) where it plunges to 68 m (223 ft) and further south, the Ridge bank (shoals) (French name "Colbart"[11]) with a maximum depth of 62 m (203 ft).[12]

Marine wildlife

NASA Terra satellite image, March 2001

The depth of the strait varies between 68 m (223 ft) at the Lobourg strait and 20 m (66 ft) at the highest banks. The seabed forms successions of three habitats:

  • rocky zones relatively deserted by ships wanting to spare their nets
  • sandy flats
  • sub-aqueous dunes.

The strong tidal currents of the strait at depth slow around its rocky masses as these stimulate

endemic to the strait.[14] Moreover, this is a transition zone for the species of the Atlantic Ocean and those of the southern part of the North Sea.[14]

This mix of various environments promotes a wide variety of wildlife.[14]

The Ridens de Boulogne, a 10–20 m (33–66 ft) deep[15] rocky shoal, partially sand-capped,15 nmi (28 km; 17 mi) west of Boulogne, boasts the highest profusion of maerl in the strait.[15]

Thus some 682 km2 (263 sq mi) of the strait is classified as a Natura 2000 protection zone named Ridens et dunes hydrauliques du Pas de Calais (Ridens and sub-aqueous dunes of the Dover Strait). This includes the sub-aqueous dunes of Varne, Colbart, Vergoyer and Bassurelle, the Ridens de Boulogne, and the Lobourg channel which provides calmer and clearer waters due to its depth reaching 68 m (223 ft).[16]

Unusual crossings

Further information: English Channel § History of Channel crossings

Many crossings other than in conventional vessels have been attempted, including by

French law bans many of them, unlike English law, most such crossings originate in England.[citation needed
]

Ice

In the late 17th century during the "Little Ice Age", there were reports of severe winter ice in the English Channel[17][18] and Strait of Dover, including a case in 1684 of only a league of open water remaining between Dover and Calais.[19]

See also

Notes

  1. ^ Historically known as the Dover Narrows; Dutch: Nauw van Calais Dutch pronunciation: [ˈnʌu vɑŋ kaːˈlɛː] or the lesser used Straat van Dover
  2. ISBN 978-0521668002
    .
  3. ISBN 9783642129063
    .
  4. ^
    PMID 25819447
    .
  5. ISBN 978-9004172678
    .
  6. ^ "The Channel Navigation Information Service (CNIS)". Archived from the original on 17 October 2007.
  7. ^ "English Channel | channel, Europe". Encyclopædia Britannica. Archived from the original on 3 April 2017. Retrieved 16 May 2017.
  8. S2CID 4408290
    .
  9. PMID 17637645
    .
  10. ^ Morelle, Rebecca (4 April 2017). "Evidence of Ancient 'Geological Brexit' Revealed". BBC News:Science & Environment. Retrieved 6 April 2017.
  11. ^ "Pas de Calais – Dover Strait". sea-seek.com.
  12. ^ "CoastView – What happens offshore?". GEOSYNTH-Project. University of Sussex.
  13. ^ "Underwater video of the ridens". YouTube.
  14. ^ a b c d Davoult, D.; Richard, A. (1988). "Les Ridens, haut-fond rocheux isolé du Pas de Calais: un peuplement remarquable" [The Ridens, Rocky Shallows in the Center of the Channel: A Distinguished Settlement]. Cahiers de Biologie Marine (in French). 29 (1): 93–107.
  15. ^ a b "Richesses de la mer" [Richness of the sea] (PDF) (in French). Picardy Estuaries and Opal Sea Marine Natural Park.
  16. ^ "Ridens et dunes hydrauliques du Pas de Calais" (in French). Natura 2000.
  17. ^ "The Great Frost of 1683-4". www.pastpresented.info. Retrieved 20 March 2020.
  18. ^ "Notes and Queries". Notes and Queries. Second Series. 11: 219. 16 March 1861 – via archive.org.
  19. ^ The World of Wonders: A Record of Things Wonderful in Nature, Science, and Art. London: Cassel Petter & Galpin. 1869.

External links

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