# Strait of Dover

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Narrowest part of the English Channel

"Pas de Calais" redirects here. For the French department, see [Pas-de-Calais](/source/Pas-de-Calais).

Dover Strait View from France across the Strait of Dover towards the English coast Location North Sea–English Channel (Atlantic Ocean) Coordinates 51°00′N 1°30′E / 51.000°N 1.500°E / 51.000; 1.500 Type Strait Basin countries France United Kingdom Min. width 20.5 miles (33.0 km) Average depth 150 feet (46 m) Max. depth 223 feet (68 m) Interactive map of Dover Strait

The **Strait of Dover** or **Dover Strait**,[a] historically known as the **Dover Narrows**, is the [strait](/source/Strait) at the narrowest part of the [English Channel](/source/English_Channel), marking the boundary between the Channel and the [North Sea](/source/North_Sea), and separating [Great Britain](/source/Great_Britain) from [continental Europe](/source/Continental_Europe). The shortest distance across the strait, at 20.6 miles (33.2 km), is from the [South Foreland](/source/South_Foreland), northeast of [Dover](/source/Dover) in the English county of [Kent](/source/Kent), to [Cap Gris-Nez](/source/Cap_Gris-Nez), a cape near to [Calais](/source/Calais) in the French [département](/source/D%C3%A9partement) of [Pas-de-Calais](/source/Pas-de-Calais). Between these points lies the most popular route for [cross-channel swimmers](/source/English_Channel#By_swimming).[1] The entire strait is within the [territorial waters](/source/Territorial_waters) of France and the United Kingdom, but a right of [transit passage](/source/Transit_passage) under the [United Nations Convention on the Law of the Sea](/source/United_Nations_Convention_on_the_Law_of_the_Sea) allows vessels of other nations to move freely through the strait.[2][3][4]

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](/source/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](/source/Matthew_Arnold)'s poem "[Dover Beach](/source/Dover_Beach)".

## Shipping traffic

[Automatic Identification System](/source/Automatic_Identification_System) display showing traffic in the strait in 2006

Most maritime traffic between the Atlantic Ocean and the North Sea and [Baltic Sea](/source/Baltic_Sea) passes through the Strait of Dover, rather than taking the longer and more dangerous route around the north of Scotland. The strait is one of the busiest [international seaways](/source/International_waterway) in the world, used by over 400 commercial vessels daily.[3] This has made traffic safety a critical issue, with [HM Coastguard](/source/Her_Majesty's_Coastguard) and the [Maritime Gendarmerie](/source/Maritime_Gendarmerie) maintaining a 24-hour watch over the strait and enforcing a strict regime of [shipping lanes](/source/Shipping_lane).[5]

In addition to the intensive north-east to south-west traffic, the strait is crossed from north-west to south-east by [ferries](/source/Ferry) linking [Dover](/source/Dover) to [Calais](/source/Calais) and [Dunkirk](/source/Dunkirk).[3] Until 1994 these provided the only route across it except for air transport. The [Channel Tunnel](/source/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](/source/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 [erosion](/source/Erosion). It had for many millennia (since the last warm [interglacial](/source/Interglacial)) been a land bridge that linked the [Weald](/source/Weald) in Great Britain to the [Boulonnais](/source/Boulonnais_(land_area)) in the [Pas de Calais](/source/Pas_de_Calais). Though pitted by troughs and rivers, the English Channel was almost mainly land at the height of the last ice age.[6] The predominant geology of both and of the seafloor is [chalk](/source/Chalk). Although somewhat resistant to erosion, erosion of both coasts has created the famous [white cliffs of Dover](/source/White_cliffs_of_Dover) in the UK and the [Cap Blanc Nez](/source/Cap_Blanc_Nez) in France. The [Channel Tunnel](/source/Channel_Tunnel) was bored through solid chalk – compacted remains of sea creatures and marine-[deposited](/source/Deposition_(geology)), ground up calciferous rock/soil debris.

The [Rhine](/source/Rhine) (as the [Urstrom](/source/Urstrom)) flows northeast into the North Sea as the sea (covering most of the Netherlands) fell during the start of the first of the [Pleistocene](/source/Pleistocene) [Ice Ages](/source/Last_Glacial_Period). The new ice unusually created a dam from [Scandinavia](/source/Scandinavia) to Scotland, and the Rhine, combined with the [Thames](/source/Thames) and drainage from much of [north Europe](/source/North_Europe), created a vast lake behind the dam, which eventually spilled over the Weald into the English Channel. This overflow followed by further scouring became recognisably the **Short Straits** (an alternative name for this strait) about 425,000 years ago. A narrow deep channel along the middle of the strait is the remnants of the main (summer) outflow of the northern Ustrom glacial lake (a collect for other then-seasonal rivers, in winter iced up, such as the Thames and Weser) in the [last Ice Age](/source/Last_glacial_period). A deposit in [East Anglia](/source/East_Anglia) marks the old [preglacial](/source/Rhine#Geologic_history) northward course of the Urstrom-Thames when it also drained [Doggerland](/source/Doggerland). The deep sea floor east of [Lincolnshire](/source/Lincolnshire) and [East Yorkshire](/source/East_Yorkshire), connecting to the [Atlantic](/source/Atlantic_Ocean) via the [Pentland Firth](/source/Pentland_Firth) in the last glaciation (of over 300,000 years) is a condition for the relatively late cutting through of the Strait to the south.

NASA Satellite image
December 2002

A 2007 study by British geoscientists [Sanjeev Gupta](/source/Sanjeev_Gupta_(geologist)) and [Jenny Collier](/source/Jenny_Collier) concluded that the Strait was formed by erosion caused by two major floods.[7][8] The first was about 425,000 years ago, when an ice-dammed lake in the southern North Sea overflowed and broke the Weald-[Artois](/source/Artois) (Boulonnais) chalk range in a catastrophic erosion and flood event. Consequently the ice-age-muted flows from the Thames and [Scheldt](/source/Scheldt) flowed through the gap into the English Channel/Inlet, but the [Meuse](/source/Meuse) and Rhine still flowed without any significant link to the inlet (such as today's [IJssel](/source/IJssel) distributary supports). In a second flood about 225,000 years ago supported by glaciers extending from areas then land such as the [Zuiderzee](/source/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](/source/Moraine#End_or_terminal_moraines) left by the ice sheet). Both floods cut massive flood channels in the dry bed of the English Channel, somewhat like the [Channeled Scablands](/source/Channeled_Scablands) or the [Wabash River](/source/Wabash_River) in the USA. A further update in 2017 attributed underwater holes in the Channel floor, "100 m deep" and in places "several kilometres in diameter", to lake water plunging over a rock ridge causing isolated depressions or [plunge pools](/source/Plunge_pool).[9] The melting ice and rising sea levels submerged [Doggerland](/source/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](/source/Varne_Bank) (shoals) where it plunges to 68 m (223 ft) and further south, the Ridge bank (shoals) (French name "*Colbart*") with a maximum depth of 62 m (203 ft).[10][11]

## Marine wildlife

[NASA](/source/NASA) [Terra](/source/Terra_(satellite)) 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](/source/Dune#Sub-aqueous_dunes).

The strong tidal currents of the strait at depth slow around its rocky masses as these stimulate [countercurrents](https://en.wiktionary.org/wiki/Special:Search/countercurrent) and deep, calm pockets where many species can find shelter.[12] In these calmer lee zones, the water is clearer than in the rest of the strait; thus [algae](/source/Alga) can grow despite the 46 m (151 ft) average depth.[13] They help increase diversity in the local species – some of which are [endemic](/source/Endemic) to the strait.[13] Moreover, this is a transition zone for the species of the Atlantic Ocean and those of the southern part of the North Sea.[13]

This mix of various environments promotes a wide variety of wildlife.[13]

The *[Ridens](https://fr.wikipedia.org/wiki/Ridens) de Boulogne*, a 10–20 m (33–66 ft) deep[14] rocky shoal, partially sand-capped,15 nmi (28 km; 17 mi) west of [Boulogne](/source/Boulogne-sur-Mer), boasts the highest profusion of [maerl](/source/Maerl) in the strait.[14]

Thus some 682 km2 (263 sq mi) of the strait is classified as a [Natura 2000](/source/Natura_2000) protection zone named *[Ridens](https://fr.wikipedia.org/wiki/Ridens) et dunes hydrauliques du Pas de Calais* (Ridens and [sub-aqueous dunes](/source/Dune#Sub-aqueous_dunes) of the Dover Strait). This includes the [sub-aqueous dunes](/source/Dune#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).[15]

## Unusual crossings

Further information: [English Channel § History of Channel crossings](/source/English_Channel#History_of_Channel_crossings)

Many crossings other than in conventional vessels have been attempted, including by [pedalo](/source/Pedalo), [jetpack](/source/Jetpack), [bathtub](/source/Bathtub), [amphibious vehicle](/source/Amphibious_vehicle) and more commonly by [swimming](/source/Human_swimming). Since [French law](/source/French_law) bans many of them, unlike [English law](/source/English_law), most such crossings originate in England.[*[citation needed](https://en.wikipedia.org/wiki/Wikipedia:Citation_needed)*]

## Ice

In the late 17th century during the "[Little Ice Age](/source/Little_Ice_Age)", there were reports of severe winter ice in the English Channel[16][17] and Strait of Dover, including a case in 1684 of only a [league](/source/League_(unit)) of open water remaining between Dover and Calais.[18]

## See also

- [Battle of Dover Strait (1916)](/source/Battle_of_Dover_Strait_(1916))

- [Battle of Dover Strait (1917)](/source/Battle_of_Dover_Strait_(1917))

- [Calais Lighthouse](/source/Calais_Lighthouse)

- [South Foreland Lighthouses](/source/South_Foreland_Lighthouses)

- [Cap Gris-Nez](/source/Cap_Gris-Nez)

- [France–United Kingdom border](/source/France%E2%80%93United_Kingdom_border)

- [Port of Boulogne-sur-Mer](/source/Port_of_Boulogne-sur-Mer)

## Notes

1. **[^](#cite_ref-1)** [French](/source/French_language): *Pas de Calais* [\[pɑ d(ə) kalɛ\]](https://en.wikipedia.org/wiki/Help:IPA/French) [ⓘ](https://en.wikipedia.org/wiki/File:Fr-Paris--Pas-de-Calais.ogg), "Strait of [Calais](/source/Calais)"; [Picard](/source/Picard_language): *Pas d'Calés*; [Dutch](/source/Dutch_language): *Nauw van Calais* [\[ˈnʌu vɑŋ kaːˈlɛː\]](https://en.wikipedia.org/wiki/Help:IPA/Dutch) or, less used, *Straat van Dover*.

## References

1. **[^](#cite_ref-2)** Crystal, David, ed. (1999). "English Channel". *Cambridge Paperback Encyclopedia* (3rd ed.). Cambridge University Press. p. 1080. [ISBN](/source/ISBN_(identifier)) [978-0521668002](https://en.wikipedia.org/wiki/Special:BookSources/978-0521668002).

1. **[^](#cite_ref-AnaLM_3-0)** López Martín, Ana G. (2010). *International Straits: Concept, Classification and Rules of Passage* (Illustrated ed.). Springer Science & Business Media. p. 95 & 102. [ISBN](/source/ISBN_(identifier)) [9783642129063](https://en.wikipedia.org/wiki/Special:BookSources/9783642129063).

1. ^ [***a***](#cite_ref-MarinePB_4-0) [***b***](#cite_ref-MarinePB_4-1) [***c***](#cite_ref-MarinePB_4-2) Glegg, G; Jefferson, R; Fletcher, S (30 June 2015). Sheppard, Charles; Galgani, Francois; Hutchings, Pat; Quintino, Victor (eds.). ["Marine Governance in the English Channel (La Manche): Linking Science and Management"](https://doi.org/10.1016%2Fj.marpolbul.2015.02.020). *Marine Pollution Bulletin*. **95** (2): 707–718. [Bibcode](/source/Bibcode_(identifier)):[2015MarPB..95..707G](https://ui.adsabs.harvard.edu/abs/2015MarPB..95..707G). [doi](/source/Doi_(identifier)):[10.1016/j.marpolbul.2015.02.020](https://doi.org/10.1016%2Fj.marpolbul.2015.02.020). [hdl](/source/Hdl_(identifier)):[10026.1/3662](https://hdl.handle.net/10026.1%2F3662). [PMID](/source/PMID_(identifier)) [25819447](https://pubmed.ncbi.nlm.nih.gov/25819447).

1. **[^](#cite_ref-Dyke_5-0)** Van Dyke, Jon M. (2009). "Transit Passage Through International Strait". In Chircop, Aldo; McDorman, Ted; Rolstons, Susan (eds.). *The Future of Ocean Regime-Building*. Brill (1618). pp. 175–232. [ISBN](/source/ISBN_(identifier)) [978-9004172678](https://en.wikipedia.org/wiki/Special:BookSources/978-9004172678).

1. **[^](#cite_ref-6)** ["The Channel Navigation Information Service (CNIS)"](https://web.archive.org/web/20071017200620/http://www.mcga.gov.uk/c4mca/mcga-hm_coastguard/channel_navigation_information_service_(cnis).htm). Archived from [the original](http://www.mcga.gov.uk/c4mca/mcga-hm_coastguard/channel_navigation_information_service_(cnis).htm) on 17 October 2007.

1. **[^](#cite_ref-7)** ["English Channel | channel, Europe"](https://www.britannica.com/place/English-Channel). *Encyclopædia Britannica*. [Archived](https://web.archive.org/web/20170403222035/https://www.britannica.com/place/English-Channel) from the original on 3 April 2017. Retrieved 16 May 2017.

1. **[^](#cite_ref-8)** Gupta, Sanjeev; Collier, Jenny S.; Palmer-Felgate, Andy; Potter, Graeme (2007). "Catastrophic Flooding Origin of Shelf Valley Systems in the English Channel". *[Nature](/source/Nature_(journal))*. **448** (7151): 342–5. [Bibcode](/source/Bibcode_(identifier)):[2007Natur.448..342G](https://ui.adsabs.harvard.edu/abs/2007Natur.448..342G). [doi](/source/Doi_(identifier)):[10.1038/nature06018](https://doi.org/10.1038%2Fnature06018). [PMID](/source/PMID_(identifier)) [17637667](https://pubmed.ncbi.nlm.nih.gov/17637667). [S2CID](/source/S2CID_(identifier)) [4408290](https://api.semanticscholar.org/CorpusID:4408290).

1. **[^](#cite_ref-9)** Gibbard, Philip (19 July 2007). ["Europe Cut Adrift"](https://doi.org/10.1038%2F448259a). *Nature*. **448** (7151): 259–60. [Bibcode](/source/Bibcode_(identifier)):[2007Natur.448..259G](https://ui.adsabs.harvard.edu/abs/2007Natur.448..259G). [doi](/source/Doi_(identifier)):[10.1038/448259a](https://doi.org/10.1038%2F448259a). [PMID](/source/PMID_(identifier)) [17637645](https://pubmed.ncbi.nlm.nih.gov/17637645).

1. **[^](#cite_ref-10)** [Morelle, Rebecca](/source/Rebecca_Morelle) (4 April 2017). ["Evidence of Ancient 'Geological Brexit' Revealed"](https://www.bbc.co.uk/news/science-environment-39494740). *BBC [News:Science](News:Science) & Environment*. Retrieved 6 April 2017.

1. **[^](#cite_ref-seaSeek_11-0)** ["Pas de Calais – Dover Strait"](http://www.sea-seek.com/?geo=1354). *sea-seek.com*.

1. **[^](#cite_ref-12)** ["CoastView – What happens offshore?"](http://www.sussex.ac.uk/geography/researchprojects/coastview/Offshore/offshore.htm). *GEOSYNTH-Project*. University of Sussex.

1. **[^](#cite_ref-13)** ["Underwater video of the ridens"](https://www.youtube.com/watch?v=vfTrDGK3j3w). *YouTube*. 15 June 2008.

1. ^ [***a***](#cite_ref-davoult_14-0) [***b***](#cite_ref-davoult_14-1) [***c***](#cite_ref-davoult_14-2) [***d***](#cite_ref-davoult_14-3) Davoult, D.; Richard, A. (1988). ["Les Ridens, haut-fond rocheux isolé du Pas de Calais: un peuplement remarquable"](http://cat.inist.fr/?aModele=afficheN&cpsidt=7856448) [The Ridens, Rocky Shallows in the Center of the Channel: A Distinguished Settlement]. *Cahiers de Biologie Marine* (in French). **29** (1): 93–107.

1. ^ [***a***](#cite_ref-RichessesAAMP_15-0) [***b***](#cite_ref-RichessesAAMP_15-1) ["Richesses de la mer"](https://www.eptb-bresle.com/userfiles/files/PNM_%203estuaires_Vol1_richesses%20de%20la%20mer.pdf) [Richness of the sea] (PDF) (in French). Picardy Estuaries and Opal Sea Marine Natural Park.

1. **[^](#cite_ref-natura2000Ridens_16-0)** ["Ridens et dunes hydrauliques du Pas de Calais"](http://inpn.mnhn.fr/site/natura2000/FR3102004) (in French). Natura 2000.

1. **[^](#cite_ref-17)** ["The Great Frost of 1683-4"](http://www.pastpresented.info/frost1683.htm). *www.pastpresented.info*. Retrieved 20 March 2020.

1. **[^](#cite_ref-18)** ["Notes and Queries"](https://archive.org/details/sim_notes-and-queries_1861-03-16_11_272/page/218/mode/2up). *Notes and Queries*. Second Series. **11**: 219. 16 March 1861 – via archive.org.

1. **[^](#cite_ref-19)** [*The World of Wonders: A Record of Things Wonderful in Nature, Science, and Art*](https://archive.org/details/worldofwondersre00londrich/page/22/mode/2up). London: Cassel Petter & Galpin. 1869.

## External links

- [Channel Navigation Information Service](http://www.mcga.gov.uk/c4mca/mcga07-home/emergencyresponse/mcga-searchandrescue/mcga-hmcgsar-sarsystem/channel_navigation_information_service__cnis_.htm)

- [Channel Swimming & Piloting Federation](http://www.channelswimming.net)

- [Channel Swimming Association](https://www.channelswimmingassociation.com)

- [Depth Chart showing straits and former course of Rhine](https://archive.today/20121208145804/http://mapserver.maptech.com/homepage/index.cfm?lat=50.9963257376773&lon=1.4719665462225308&scale=1500000&zoom=50&type=0&icon=0&width=498&height=498&searchscope=dom&CFID=1719760&CFTOKEN=33728793&scriptfile=http://mapserver.maptech.com/homepage/index.cfm&latlontype=DMS)

Authority control databases International VIAF GND FAST National United States France BnF data Israel Geographic Pleiades Other IdRef Yale LUX

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