Shoals and sandbanks are characteristic underwater seabed features of the southern North Sea and the eastern English Channel. The relatively shallow water depth allows tidal currents to transport, configure and alter seabed materials, such as sand, shells, clay, and gravel, into elongated banks or shoals of shallow water.
In the southern North Sea the Spring Tide range is in excess of 7 metres. [1] The large tidal amplitude produces tidal currents of 1.5 metres per second (m/s) on the flood tide, and 1.35 m/s during the ebb tide. Water flows parallel to the shore and this is reflected in the orientation of sandbanks. Typically, sandbanks of the English Channel and southern North Sea rise 10 to 25 m above the sea floor and are 10 to 30 km long and 1 to 3 km wide. [2] [1] [3] The volume of material in some of the banks has been estimated at between 70 and 1100 Million m3. [4]
Strong eddies and rip tides occur in the vicinity of many shoals, and the sea can break heavily over shoals especially when the wind is against the tidal current. [5] Sandbanks and shoals are often marked by buoys. There are usually north and south marks, and on large shoals, east and west marks. [6] [7] [8]
The table below is a list of the named sandbanks and shoals of the southern North Sea, the Dover Strait (Pas-de-Calais) and the eastern English Channel (La Manche). [9] [10] [11] The geographical extent is eastwards from a line (00°14'E) extending south from Beachy Head England to Étretat France in the English Channel, through the Straits of Dover, then north through the southern North Sea to a line extending east from Berwick-upon-Tweed England (55°50’N) to Ringkobing Fjord Denmark. [6] [7] [8] [12] [13] [14]
This area includes the shipping forecast areas of Wight (part); Dover; Thames; Tyne; Humber; Dogger and German Bight (part). [15] It includes the territorial waters and exclusive economic zones of Belgium, Denmark, France, Germany, the Netherlands and the United Kingdom.
The Thames Estuary is defined as from the Nore Sand eastwards to a line from North Foreland to Harwich. [6]
The Humber is defined as west of the Outer Sea Reach buoy 00° 06’E. [8]
SNS – Southern North Sea; S-N – South to North; E-W – East to West; SW-NE – South-West to North-East; SE-NW – South-East to North-West.
A tabulated list of shoals and sandbanks in the southern North Sea, Dover Strait and English Channel. [6] [7] [8] [9] [10] [11] [14] [15]
Name | Country | Location | Coordinates at centre of bank or shoal | Orientation | Length, km | Width, km | Remarks |
---|---|---|---|---|---|---|---|
Akkaertbank | Belgium | SNS | 51°23’N 02°49’E | SW-NE | 7.4 | 0.5 | |
Aldeburgh Napes | UK | SNS | 52°09’N 01°43’E | S-N | 10 | 1 | |
Aldeburgh Ridge | UK | SNS | 52°08’N 01°37’E | S-N | 7 | 1 | |
Anrum Bank | Germany | SNS | 54°38’N 08°00’E | S-N | 23.4 | ||
Banc Breedt | France | SNS | 51°07’N 02°22E | SW-NE | 24 | 2 | |
Banc de Snouw | France | SNS | 51°04’N 02°15’E | E-W | 7.5 | 1 | |
Barmade Bank | UK | SNS | 55°00’N 00°00’ | - | - | - | |
Barrow | UK | Thames Estuary | 51°37’N 01°10’E | SW-NE | 5.5 | 3.5 | The adjacent Barrow Deep used for dumping sewage sludge 1889-1998 |
Bassurelle Bank | UK & France | Dover Strait | 50°38’N 01°05’E | SW-NE | 15 | 2.5 | |
Bassurelle de la Somme | France | English Channel | 50°12’N 01°22’E | SW-NE | 5.2 | 0.6 | |
Bassure de Baas | France | English Channel | 50°27'N 01°20'E | 56 | |||
Battur | France | English Channel | 50°22'N 01°18'E | 14 | |||
Bawdsey Bank | UK | SNS | 51°59’N 01°33’E | S-N | 12.5 | 1.5 | |
Bergues Bank | France & Belgium | SNS | 51°15’N 02°18’E | SW-NE | 11 | 2 | |
Blakeney Overfalls | UK | SNS | 53°01’N 01°11’E | E-W | 4.0 | 1.0 | |
Bligh Bank | Belgium | SNS | 51°33’N 02°35’E | SW-NE | 5.5 | 0.5 | |
Boulder Banks | UK | English Channel | 50°52’N 00°47’E | - | 0.6 | 0.6 | |
Boulders Bank | UK | SNS | 54°25’N 01°35’E | - | - | - | Dogger Bank |
Broad Fourteens | Netherlands | SNS | 53°00’N 00°03’E | S-N | Named from depth of 14 fathoms | ||
Broadstairs Knoll | UK | SNS | 51°21’N 01°29’E | - | 5.5 | 5.5 | |
Broken Bank | UK | SNS | 53°19’N 02°12’E | SE-NW | 35 | 1 | Volume of bank: 360 Million m3 |
Brown Bank, Brown Ridge [16] | UK & Netherlands | SNS | 52°40’N 03°15’E | S-N | 30 | 2 | Bruine Bank |
Bruceys Garden | UK | SNS | 54°50’N 00°50’E | - | - | - | |
Bullock Bank | France | English Channel | 50°44'N 01°05''E | 11 | |||
Burcom Sand | UK | Humber | 53°35’N 00°04’W | SE-NW | 2.5 | 1 | |
Buiten Ratel | Belgium | SNS | 51°15’N 02°31’E | SW-NE | 14.8 | 2 | |
Bull Sand | UK | Humber | 53°33’N 00°05’E | SE-NW | 4.0 | 1.5 | |
Buxey Sand | UK | SNS | 51°41’N 01°27’E | SW-NE | 9 | 4 | |
Chequer Shoal | UK | Humber | 53°33’N 00°10’E | E-W | 3.5 | 2 | |
Cleaver Bank | Netherlands | SNS | 54°10'N 03°08'E | Klaverbank | |||
Coal Pit | UK | SNS | 53°29’N 01°46’E | ||||
Cork Sand | UK | SNS | 51°53’N 01°24’E | S-N | 8 | 4.5 | |
Corton Sands | UK | SNS | 52°35’N 01°47’E | S-N | Position and depth changes | ||
Cromer Knoll | UK | SNS | 53°18’N 01°18’E | S-N | 5 | 1 | |
Cutler Shoal | UK | SNS | 51°59’N 01°27’E | SW-NE | 2.5 | 0.5 | |
Docking Shoal | UK | SNS | 53°10’N 01°45’E | - | 13.5 | 13.5 | |
Dogger Bank | UK | SNS | 54°43’N 02°46’E | - | 260 | 100 | Windfarm |
Dogger Bight | UK | SNS | 54°19’N 01°50’E | - | - | - | Dogger Bank |
Dogger North Shoal | UK | SNS | 54°55’N 01°35’E | - | 17.1 | 21.6 | Dogger Bank |
Dogger Tail End | Germany & Netherlands | SNS | 55°29’N 04°00’E | - | - | - | |
Drillstone | UK | SNS | 51°26’N 01°41’E | ||||
Dudgeon Shoal | UK | SNS | 53°17’N 00°56’E | SE-NW | 9.75 | 7.5 | Windfarm |
Dunwich Bank | UK | SNS | 52°14’N 01°40’E | S-N | 3 | 1 | |
Dyck Central | France | SNS | 51°07’N 02°12’E | SW-NE | 8 | 1.5 | |
Dyck Occidental | France | SNS | 51°05’N 02°00 | SW-NE | 18.5 | 2 | |
Dyck Oriental | France | SNS | 51°13’N 02°23’E | SW-NE | 13 | 2 | |
East Barrow | UK | Thames Estuary | 51°35’N 01°10’E | SW-NE | 9 | 3.5 | |
East Spaniard | UK | Thames Estuary | 51°25’N 01°01’E | E-W | |||
Eastermost Shoal | UK | SNS | 54°40’N 02°30’E | - | 54 | 40.5 | Dogger Bank |
Engelsmanplaat | Netherlands | SNS | 53°27'N 06°03'E | ||||
Fairy Bank | France | SNS | 51°23’N 02°20’E | SW-NE | 5.5 | 0.5 | |
Fisher Bank | Denmark | SNS | |||||
Flemish Banks | Belgium | SNS | 51°17'N 02°38E | ||||
Foulness Sand | UK | SNS | 51°37’N 01°02’E | SW-NE | 11 | 4.5 | Extends from shore |
Four Fathoms Sand Ridge | UK | English Channel | 50°48’N 00°39’E | SW-NE | 5.4 | 0.6 | |
Galloper | UK | SNS | 51°46’N 01°57’E | S-N | 5.5 | 1 | Windfarm |
Girdler | UK | Thames Estuary | 51°30’N 01°08’E | E-W | 3 | 1 | |
Goodwin Sands | UK | SNS | 51°16’N 01°21’E | SW-NW | 22 | ||
Grandes Écamias | France | English Channel | 50°59’N 00°54’E | E-W | 5 | 0.6 | |
Großer Knechtsand | Germany | SNS | 53°50'N 08°21'E | ||||
Gunfleet Sand | UK | Thames Estuary | 51°45’N 01°15’E | SW-NE | 23 | 3 | Abandoned lighthouse; Windfarm |
Haddock Bank | UK | SNS | 53°19’N 01°31’E | SE-NW | |||
Haile Sand | UK | Humber | 53°32’N 00°13’E | - | |||
Haisborough Sand | UK | SNS | 52°54’N 01°42’E | SE-NW | 16 | 2 | Volume of bank: 530 Million m3 |
Hammond Knoll | UK | SNS | 52°52’N 01°55’E | SE-NW | 9.7 | Volume of bank: 99 Million m3 | |
Hastings Shoals | UK | English Channel | 50°49’N 00°34’E | SW-NE | |||
Hearty Knoll | UK | SNS | 52°46’N 02°10’E | SE-NW | Volume of bank: 120 Million m3 | ||
Helgoland | Germany | SNS | 54°12’N 07°55’E | - | 9 | 9 | |
Hessle Sand | UK | Humber | 53°43’N 01°25’W | E-W | 2 | 1 | |
Hewett Ridge | UK | SNS | 52°52’N 02°00’E | SE-NW | 28 | 4 | Gas field. Volume of bank: 190 Million m3 |
Holm Sand | UK | SNS | 52°29’N 01°47’E | S-N | 11 | 1.5 | |
Horse of Willingdon | UK | English Channel | 50°45’N 01°02’E | E-W | 3 | 1 | |
Hull Middle | UK | Humber | 53°42’N 00°22’W | E-W | 3.5 | 1 | |
Indefatigable Bank 1, 2 & 3 | UK | SNS | 53°30’N 02°23’E | SE-NW | 4 | Gas field. Volume of bank: 85 Million m3 (1), 69 Million m3 (2), 310 Million m3 (3) | |
Inner Bank | UK | SNS | 53°12’N 02°01’E | SE-NW | 18 | 1 | Volume of bank: 110 Million m3 |
Inner Bank | UK | SNS | 54°20’N 00°30’E | - | - | - | Dogger Bank |
Inner Dowsing | UK | SNS | 53°19’N 00°35’E | S-N | 7.5 | 3 | Windfarm |
Inner Gabbard | UK | SNS | 51°55’N 01°54’E | S-N | 16 | 1.5 | Windfarm |
Inner Silver Pit | UK | SNS | 53°32′N 00°47′E | ||||
In Ratel | France | SNS | 51°07’N 02°16’E | SW-NE | 6.5 | 1 | |
In Ruytingen | France | SNS | 51°13’N 02°17’E | SW-NE | 12 | 5.5 | |
Jim Howe Bank | UK | SNS | 52°57’N 02°25’E | SE-NW | |||
Kachelotplate | Germany | SNS | 53°39'N 06°49'E | ||||
Kentish Knock | UK | SNS | 51°37’N 01°38’E | S-N | 13.5 | 2.5 | |
Knock John | UK | Thames Estuary | 51°34’N 01°04’E | SW-NE | 3 | 1 | Maunsell fort |
Kobbergrund | Denmark | SNS | 57°12'N 11°15'E | ||||
Koresand | Denmark | SNS | 55°15'N 08°29'E | ||||
Kwintebank | Belgium | SNS | 51°15’N 02°38’E | SW-NE | 11 | 2 | |
Le Colbart | France | Dover Strait | 50°53’N 01°20’E | SW-NE | 16 | 1 | Also called The Ridge |
Leman Bank | UK | SNS | 53°08’N 01°55’E | SE-NW | 42 | 11 | Gas field. Volume of bank: 840 Million m3 |
Les Ridens | France | Dover Strait | 50°45'N 01°18'E | Several shoals | |||
Long Sand | UK | Thames Estuary | 51°37’N 01°30’E | SW-NE | 33 | 7.5 | |
Maplin Sand | UK | Thames Estuary | 51°33'N 00°47’E | SW-NE | 23 | 6.1 | Extends from coast |
Maplin Spit | UK | Thames Estuary | 51°36’N 01°06’E | SW-NE | 4.5 | 1 | |
Margate Sand | UK | Thames Estuary | 51°26’N 01°20’E | E-W | 9 | 2 | |
Middelbank | Netherlands | SNS | 51°40’N 03°22’E | SW-NE | 14.8 | 0.5 | |
Middelkerke Bank | Belgium | SNS | 51°15’N 02°43’E | SW-NE | 13 | 2.5 | |
Middle Cross Sand | UK | SNS | 52°39’N 01°52’E | S-N | 3 | 1 | |
Middle Sand | UK | Thames Estuary | 51°27’N 01°02’E | SW-NE | 6 | 1.5 | |
Middle Shoal | UK | Humber | 53°37’N 00°02’W | SE-NW | 4.0 | 1 | |
Mouse | UK | Thames Estuary | 51°32’N 01°04’E | SW-NE | 4.5 | 0.5 | |
Newarp Banks | UK | SNS | 52°42’N 02°00’E | S-N | 8.5 | 2 | |
Noordhinder Bank | Belgium | SNS | 51°39′N 02°41′E | S-N | 11 | 1 | |
Nieuwpoort Bank | Belgium | SNS | 51°13’N 02°41’E | SW-NE | 9.25 | 1 | |
Nore Sand | UK | Thames Estuary | 51°29’N 00°46’E | E-W | 6 | 1 | |
North Cross Sand | UK | SNS | 52°45’N 01°52’E | S-N | 7 | 1 | |
North Falls | UK | SNS | 51°40’N 01°57’E | S-N | 11 | 1 | |
Oaze | UK | Thames Estuary | 51°30’N 01°00’E | SW-NE | 5.5 | 1 | |
Oost Dyck | Belgium | SNS | 51°18’N 02°29’E | SW-NE | 14.8 | 1.5 | |
Oostende Bank | Belgium | SNS | 51°16’N 02°48’E | SW-NE | 15 | 2 | |
Oosthinder | Belgium | SNS | 51°32’N 02°38’E | SW-NE | 16.6 | 1.5 | |
Out Ruytingen | France | Dover Strait | 51°14’N 02°17°E | SW-NE | 33 | 2 | |
Outer Bank | UK | SNS | 54°30’N 01°05’E | - | - | - | Dogger Bank |
Outer Dowsing | UK | SNS | 53°25’N 01°08’E | SE-NW | 19.5 | 1 | Windfarm |
Outer Gabbard | UK | SNS | 51°58’N 02°03’E | S-N | 5 | 2 | Windfarm |
Outer Silver Pit | UK | SNS | 54°00′N 02°00′E | ||||
Ower Bank | UK | SNS | 53°14’N 01°52’E | SE-NW | 45 | 1 | Volume of bank: 730 Million m3 |
Paardenmarkt | Belgian | SNS | 51°21'N 03°17'E | ||||
Pan Sand | UK | Thames Estuary | 51°28’N 01°10’E | E-W | 3.5 | 1 | |
Raan | Netherlands | SNS | 51°27’N 03°20’E | - | 22 | 6 | |
Race Bank | UK | SNS | 53°12’N 00°51’E | SE-NW | 21.0 | 5.5 | Windfarm |
Red Sand | UK | Thames Estuary | 51°28’N 01°00’E | E-W | 2 | 0.5 | Maunsell fort |
Petits Écamias | France | English Channel | 50°01’N 00°53’E | E-W | 5.2 | 1.5 | |
Richel | Netherlands | SNS | 53°17N 05°08'E | ||||
Quemer | France | English Channel | 50°15’N 01°18’E | - | 10 | - | |
Ridins de Dieppe | France | English Channel | 50°06’N 01°08’E | - | 10.4 | 10.4 | |
Ridins de Tréport | France | English Channel | 50°05’N 01°16’E | - | 5 | 0.6 | |
Rosse Spit | UK | Humber | 53°30’N 00°15’E | SW-NE | 4.5 | 2 | |
Rough Shoals | UK | SNS | 51°54’N 01°30’E | S-N | 10 | 8 | HM Fort Roughs |
Royal Sovereign Shoals | UK | English Channel | 50°45’N 00°26’E | S-N | 4 | 1 | |
Sandettie Bank | France & UK | Dover Strait | 51°09′N 01°47′E | SW-NE | 27 | 5 | |
Schouwenbank | Netherlands | SNS | 51°48′N 03°25′E | SW-NE | 18.5 | 1 | |
Scroby Sands | UK | SNS | 52°38’N 01°47’E | S-N | 14 | 2 | Windfarm |
Sheringham Shoal | UK | SNS | 53°03’N 01°10’E | E-W | 10 | 1.0 | |
Shingles | UK | Thames Estuary | 51°31’N 01°13’E | E-W | 6.5 | 5.0 | |
Shipwash | UK | SNS | 51°58’N 01°37’E | S-N | 18 | 2 | |
Shivering Sand | UK | Thames Estuary | 51°30’N 01°24’E | SW-NE | 3.5 | 0.5 | Maunsell fort |
Simonszand | Netherlands | SNS | 53°31'N 06°24E | ||||
Sizewell Bank | UK | SNS | 52°10’N 01°40’E | S-N | 4 | 1 | |
Smal Bank | France & Belgium | SNS | 51°06’N 02°30’E | SW-NE | 26 | 2 | |
Smiths Knoll | UK | SNS | 52°52’N 02°13’E | S-N | 28 | 1 | Volume of bank: 390 Million m3 |
Sole Pit High | UK | SNS | 53°35’N 01°23’E | SW-NE | 7 | 1 | |
South Cross Sand | UK | SNS | 52°34’N 01°51’E | S-N | 9 | 1 | |
South Dogger Ground | UK | SNS | 54°18’N 02°25’E | - | - | - | Dogger Bank |
South Falls | UK | SNS | 51°21’N 01°47’E | S-N | 28 | ||
South Shoal | UK | Humber | 53°36’N 00°00’ | SE-NW | 3.5 | 1 | |
Spaniard | UK | Thames Estuary | 51°27’N 01°03’E | E-W | 1 | 0.5 | |
SouthWest Patch | UK | SNS | 54°35’N 02°05’E | - | 67.5 | 22.5 | Dogger Bank |
Spile | UK | Thames Estuary | 51°07’N 00°57’E | E-W | 2 | 0.5 | |
Steenbanken | Netherlands | SNS | 51°41’N 02°25’E | SW-NE | 11 | 0.5 | |
Stephensons Shoal | UK | English Channel | 50°53’N 00°54’E | E-W | 5 | - | |
Stroombanc | Belgium | SNS | 51°13’N 02°48’E | SW-NE | 13 | 2 | |
Sunk Sand | UK | Thames Estuary | 51°39’N 01°15’E | SW-NE | 24 | 3 | Maunsell fort (ruin) |
Swarte Bank | UK | SNS | 51°24’N 02°13’E | SE-NW | 41 | 1 | Volume of bank: 440 Million m3 |
Sylt Outer Reef | Germany | SNS | 55°06’N 07°35’E | - | - | - | |
Terschellinger Bank | Netherlands | SNS | 53°32’N 05°08’E | SE-NW | - | - | |
Tertius (sandbank) | Germany | SNS | 54°08'N 08°42E | ||||
The Hills | UK | SNS | 54°21’N 00°60’E | - | - | - | |
Thornton Ridge or Bank | Belgium | SNS | 51°34’N 03°00’E | SW-NE | 6 | 1 | Windfarm |
Tizard Bank | UK | Thames Estuary | 51°33’N 01°12’E | E-W | 2.5 | 0.5 | |
Tongue Sand | UK | Thames Estuary | 51°31’N 01°13’E | E-W | 7.5 | 1.5 | Maunsell fort (ruin) |
Triton Knoll | UK | SNS | 53°23’N 01°00’E | SE-NW | 25.5 | Windfarm | |
Varne Bank | UK | Dover Strait | 51°00’N 01°23’E | SW-NE | 9.3 | 1 | |
Vergoyer Banks | France | English Channel | 50°33'N 01°15'E | 24 | |||
Weiss Bank | Germany | SNS | 55°00’N 06°00’E | - | - | - | |
Well Bank | UK | SNS | 53°14’N 02°11’E | SE-NW | 57 | 2 | Volume of bank: 1100 Million m3 |
West Barrow | UK | Thames Estuary | 51°35’N 01°56’E | SW-NE | 13 | 1.8 | |
West Dyck | France | Dover Strait | 51°03’N 01°51’E | ||||
Westhinder | Belgium | SNS | 51°28’N 02°31’E | SW-NE | 22 | 2 | |
Whitaker Spit | UK | Thames Estuary | 51°40’N 01°07’E | SW-NE | 6 | 1 | |
Winterton Ridge | UK | SNS | 52°50’N 02°02’E | SE-NW | 8 | 0.5 | Volume of bank: 105 Million m3 |
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Goodwin Sands is a 10-mile-long (16 km) sandbank at the southern end of the North Sea lying 6 miles (10 km) off the Deal coast in Kent, England. The area consists of a layer of approximately 25 m (82 ft) depth of fine sand resting on an Upper Chalk platform belonging to the same geological feature that incorporates the White Cliffs of Dover. The banks lie between 0.5 m above the low water mark to around 3 m (10 ft) below low water, except for one channel that drops to around 20 m (66 ft) below. Tides and currents are constantly shifting the shoals.
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Cuspate forelands, also known as cuspate barriers or nesses in Britain, are geographical features found on coastlines and lakeshores that are created primarily by longshore drift. Formed by accretion and progradation of sand and shingle, they extend outwards from the shoreline in a triangular shape.
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George Smeed is a Thames barge built in 1882 by Smeed Dean & Co. Ltd. in Murston.
William Hewett was a Royal Navy officer noted for making the first comprehensive survey of the North Sea and for his work on tides.
The Edinburgh Channels, formerly a single channel known as the Bullock Channel and then the Duke of Edinburgh Channel are two roughly parallel transverse channels in the Thames Estuary. They used to be important for navigation, providing a deep approach to the River Thames from the south-east through the sandbanks of the estuary. The opening of an alternative channel in 2000 has greatly reduced their use, but having been surveyed and studied extensively over the past two centuries they provide an important example of the processes that shape shallow water landforms.