The Thames Estuary is where the River Thames meets the waters of the North Sea, in the south-east of Great Britain.
An estuary can be defined according to different criteria (e.g. tidal, geographical, navigational or in terms of salinity). For this reason the limits of the Thames Estuary have been defined differently at different times and for different purposes.
This limit of the estuary has been defined in two main ways: [1]
The transition between the Thames Estuary and the North Sea has been located at various notional boundaries, including: [1]
The estuary just east of the Tideway has a tidal range of 4 metres. Winds excluded, it moves at 2.6 knots (4.8 km/h; 3.0 mph) in bi-monthly spring tides. [5]
The estuary is one of the largest of 170 such inlets on the coast of Great Britain. It constitutes a major shipping route, with thousands of movements each year, including: large oil tankers, container ships, bulk carriers (of loose materials/liquids), and roll-on/roll-off (ro-ro) ferries. It is the accessway for the Port of London (including London Gateway, associated Tilbury and Purfleet) and the Medway Ports of Sheerness, Chatham and Thamesport.
The traditional Thames sailing barge worked in this area, designed to be suitable for the shallow waters in the smaller ports.
A 2000s-decade-built wind farm is 8.5 km north of Herne Bay, Kent, on a shoal south-west of Kentish Knock. It is 30 wind turbines generating typically 82.4MW of electricity.
The much larger 630 MW London Array was inaugurated in 2013.
The term Greater Thames Estuary [6] applies to the coast and the low-lying lands bordering the estuary. These are characterised by the presence of mudflats, low-lying open beaches, and salt marshes, namely the North Kent Marshes and the Essex Marshes. Human-made embankments are backed by reclaimed wetland grazing areas, but rising sea levels may make it necessary briefly to flood some of that land at spring tides, to take the pressure off the defences and main watercourses.
There are many smaller estuaries in Essex, including the rivers Colne, Blackwater and Crouch. Small coastal villages depend on an economy of fishing, boat-building, and yachting. [7] The Isle of Sheppey, the Isle of Grain, Canvey Island, Two Tree Island, Havengore Island, New England Island, Rushley Island, Potton Island, Foulness Island and Mersea Island are part of the coastline. [8]
Where higher land reaches the coast, there are some larger settlements, such as Clacton-on-Sea to the north in Essex, Herne Bay, Kent, and the Southend-on-Sea area within the narrower part of the estuary.
The Thames Estuary is the focal part of the 21st-century toponym, the "Thames Gateway", designated as one of the principal development areas in Southern England.
The Thames Estuary 2050 Growth Commission report published in June 2018 identified the economic potential of the region. In 2020 the Thames Estuary Growth Board [9] was appointed, led by government-appointed Envoy Kate Willard OBE, to unlock the potential of the UK's number one green growth opportunity.
Entrepreneurs and investors have looked at the greater estuary as a possible place for a new airport, [10] and have expanded Southend Airport in the 2010s, which has a rail link to Liverpool Street station, London among others.
Designations | |
---|---|
Official name | Thames Estuary and Marshes |
Designated | 5 May 2000 |
Reference no. | 1025 [11] |
The Thames flowing through London is an archetypal, well-developed economy urban, upper river estuary with its sedimentary deposition restricted through manmade embankments and occasional dredging of parts. It is mainly a freshwater river about as far east as Battersea, insofar as the average salinity is very low and the fish fauna consists predominantly of freshwater species such as roach, dace, carp, perch, and pike. It becomes brackish between Battersea and Gravesend, and the diversity of freshwater fish is smaller, primarily roach and dace. Euryhaline species then dominate, such as flounder, European seabass, mullet, and smelt. Further east salinity increases and conditions become fully marine and the fish fauna resemble that of the adjacent North Sea, a spectrum of euryhaline and stenohaline types. An alike pattern of zones applies to the aquatic plants and invertebrates. [12] [13]
Joseph Conrad lived in Stanford-le-Hope close to the Essex marshes. His The Mirror of the Sea (1906) contains a memorable description of the area as seen from the Thames. He refers to this area in the first pages of his novel Heart of Darkness , describing it as both the launching place of England's great ships of exploration and colonization and, in ancient times, the site of colonization of the British Isles by the Roman Empire.
The form of speech of many of the people of the area, principally the accents of those from Kent and Essex, is often known as Estuary English. The term is a term for a milder variety of the "London Accent". The spread of Estuary English extends many hundreds of miles outside London, and all of the neighbouring home counties around London have residents who moved from London and brought their version of London accents with them, leading to interference with the established local accents. The term London Accent is generally avoided, as it can have many meanings. Forms of "Estuary English", as a hybrid between Received pronunciation and various London accents, can be heard in all of the New Towns, all of the coastal resorts, and in the larger cities and towns along the Thames Estuary.
For commercial shipping rounding the Nore sandbank and thus accessing Greater London, main deep-water routes were the Princes-Queens Channel and the South Channel to the south, to a lesser extent the Kings Channel and the Swin to the north. The Swin was used by barges and leisure craft from the Essex rivers, and coasters and colliers from the north east. These channels were made up of natural troughs; Yantlet Channel (Sea Reach), Oaze Deep, Knock John Channel, Black Deep/Black Deep Channel which have been much-marked. These are separated by slow-moving sandbanks with names such as the East and West Barrows, the Nob, the Knock, Kentish Knock, the John, the Sunk, the Girdler, and Long Sand/the Long Sands. [14]
Shallow-bottomed barges and coasters would navigate the swatchways at flood tide, and would cross the sand banks at spitways, points where the water was least shallow, and just deep enough at that point of the tide. If they missed the moment they would heave to (lay anchor) and wait for the next tide.
Recreational craft are expected use channels most suited to the size of their vessel. Their main guide says to use when navigating to or from:
To cross the south-east quarter of the estuary large vessels use Fisherman's Gat, and small vessels to were expected to use Foulger's Gat. [15]
Provision of buoys and beacons for the purpose of navigation came relatively late to England (compared to the Netherlands, for example). [16] Instead, coastal navigators and pilots relied on the use of transits (the alignment of prominent structures or natural features on land) for guidance. In 1566 Trinity House of Deptford (which oversaw pilotage on the Thames) was empowered to 'make, erect and set up [...] beacons, marks and signs for the sea' (albeit at its own expense). [17] Not long afterwards, the decay of the steeple of Margate Church (an important landmark for negotiating 'the Narrows', a complex route between sandbanks used by vessels sailing to or from London along the North Kent coast) led to Trinity House marking the Narrows with buoys in the late 16th century. [16]
In his coastal survey of 1682-93, Greenvile Collins records five buoys around the Narrows, just north of Reculver, on the southern approach to the Thames. The Swin (the northern approach) was marked with buoys at the easternmost points of the Gunfleet, Middle and Buxey sands, and by beacons on the Whitaker, Shoe and Blacktail spits. A buoy marked the easternmost point of the Nore sandbank at this time, and three more buoys marked sandbanks in the middle part of the estuary (Spaniard, Red Sand and the Oaze). [16]
The Nore Lightship, the world's first lightvessel, was established in the Estuary as a private venture in 1732 to mark the 'best position for entering the Thames and Medway, and to clear the Nore Sand'. [18] The coastwise approach from the north was aided by the establishment of the Sunk lightvessel in 1802 'to mark the north-east entrance to East Swin, and to guide vessels round Long Sand'. Later, the Swin channel was further marked by lightvessels at Swin Middle (1837) and Mouse (1838), and by screw-pile lighthouses on the Maplin Sands (1841) and at Gunfleet (1856). [19] Meanwhile, one of the outlying sandbanks of the Estuary was marked by a lightvessel at Kentish Knock (in 1840); and in due course the southern approach was marked by lightvessels at the Tongue (1847) and Girdler (1848) sands, with another being added (between these two) in the Princes Channel (1856). In 1851 two more screw-pile lighthouses were built further upriver, on the northern foreshore of Sea Reach: at Mucking and on the Chapman sands (just off Canvey Island).
Prior to 1684 beacons were set up on the mudflats north of the Swin channel, to help vessels approaching the Thames from the north to navigate the sands. Pan-sand Beacon was set up by Trinity House in 1774 to mark a dangerous sandbank on the southern approach. [20] Similar daymarks were set up on other nearby sandbanks in later years, including on Margate Hook (1843), Middle Ground (1844) and Shingles (1846). [20] Trinity House also maintained beacons further upriver, including at Broadness (established in 1821), Stoneness (1839), Erith (1830) and Tripcock (1832).
In 1864 responsibility for maintaining the navigation lights of the River Thames between London Bridge and Yantlet was transferred by Act of Parliament from the Thames Conservancy to the Corporation of Trinity House; responsibility for buoyage was transferred likewise in 1878. [21] In 1885 the beacons at Broadness and Stoneness were replaced with iron-frame experimental lighthouses, each lit by a novel system which would allow the light to function unattended (except for a twice-weekly visit by a boatman for cleaning and maintenance). Broadness was lit by Pintsch gas, and Stoneness by a Lindberg light (which burned petroleum naphtha). [22] At the same time Trinity House began experimenting with the application of lamps to buoys, using Pintsch's oil-gas system, beginning with three in the Thames Estuary (East Oaze, Ovens and Sheerness Middle); the experiment was deemed a success and subsequently further buoys and beacons were lit by Trinity House using the same system, in the Estuary and beyond. [22]
Today the Port of London Authority's Thames Navigation Service (established in 1959) is responsible for buoyage, beaconage and bridge lights on the Tideway. [23] Trinity House remains responsible for aids to navigation in the wider estuary (and beyond).
This table shows, from west to east, the principal navigation lights, buoys and other marks to the north (port) and south (starboard) of the main deep-water channels of the River Thames from Gallions Reach to the Sunk Light Float. [24] [25] [26] [27] [28] The Thames is in IALA region A so port buoys are red and starboard buoys are green.
Name of navigational mark | South of channel | Channel | North of channel | ||||
---|---|---|---|---|---|---|---|
Type | Light | Location coordinate | Type | Light | Location coordinate | ||
Margaretness Point (or Tripcock Ness) Light | Lighthouse | Group flashing (2) white 5s | 51°30.662′N0°05.766′E / 51.511033°N 0.096100°E | Gallions Reach / Barking Reach | ̶ | ̶ | ̶ |
Crossness Point Light | Lighthouse | Flashing white 5s | 51°30.920′N0°07.990′E / 51.515333°N 0.133167°E | Barking Reach / Halfway Reach | ̶ | ̶ | ̶ |
Crayfordness Point Light | Lighthouse | Flashing white 5s + fixed | 51°28.689′N0°13.000′E / 51.478150°N 0.216667°E | Erith Rands / Long Reach | ̶ | ̶ | ̶ |
Stone Ness Light | ̶ | ̶ | ̶ | Long Reach / St Clement's Reach | Lighthouse | Flashing green 2.5s | 51°27.9167′N0°16.8231′E / 51.4652783°N 0.2803850°E |
Broadness Point Light | Lighthouse | Occulting red 5s | 51°27.878′N0°18.900′E / 51.464633°N 0.315000°E | St Clement's or Fiddler's Reach / Northfleet Hope | ̶ | ̶ | ̶ |
Tilbury Warning Light | ̶ | ̶ | ̶ | Gravesend Reach | Warning light, vessels manoeuvring at Tilbury | Isophase 6s | 51°27.000′N0°21.340′E / 51.450000°N 0.355667°E |
Shornmead Light | Lighthouse | Group flashing (2) white, red 10s | 51°26.983′N0°26.533′E / 51.449717°N 0.442217°E | Gravesend Reach / The Lower Hope | ̶ | ̶ | |
Ovens | ̶ | ̶ | ̶ | The Lower Hope | Quick flashing green | 51°27.493′N0°26.355′E / 51.458217°N 0.439250°E | |
Haven Traffic Warning Lights | Warning light, vessels manoeuvring at Coryton | E | 51°27.90′N0°30.10′E / 51.46500°N 0.50167°E | The Lower Hope / Sea Reach | Warning light, vessels manoeuvring at Coryton | White | 51°30.50′N0°31.65′E / 51.50833°N 0.52750°E |
London Gateway | ̶ | ̶ | ̶ | Sea Reach | Buoy | 51°30.30′N0°28.20′E / 51.50500°N 0.47000°E | |
Sea Reach № 7 | Port buoy Racon T | Flashing Red 2.5s | 51°30.011′N0°36.908′E / 51.500183°N 0.615133°E | The Yantlet Channel | Yellow pillar buoy | Flashing yellow 2.5s | 51°30.206′N0°36.938′E / 51.503433°N 0.615633°E |
Sea Reach № 6 | Port buoy | Flashing red 5s | 51°29.932′N0°39.839′E / 51.498867°N 0.663983°E | Starboard buoy | Flashing green 5s | 51°30.126′N0°39.867′E / 51.502100°N 0.664450°E | |
Sea Reach № 5 | Port buoy | Very quick flashing red | 51°29.848′N0°41.426′E / 51.497467°N 0.690433°E | Starboard buoy | Very quick flashing Green | 51°30.041′N0°41.473′E / 51.500683°N 0.691217°E | |
Sea Reach № 4 | Port buoy | Group flashing (2) red 5s | 51°29.504′N0°44.121′E / 51.491733°N 0.735350°E | Starboard buoy | Group flashing (2) green 5s | 51°29.694′N0°44.193′E / 51.494900°N 0.736550°E | |
Sea Reach № 3 | Port buoy | Quick flashing red | 51°29.221′N0°46.707′E / 51.487017°N 0.778450°E | Starboard buoy | Quick flashing green | 51°29.410′N0°47.061′E / 51.490167°N 0.784350°E | |
Sea Reach № 2 | Port buoy | Flashing red 5s | 51°29.296′N0°49.754′E / 51.488267°N 0.829233°E | Starboard buoy | Flashing green 5s | 51°29.493′N0°49.726′E / 51.491550°N 0.828767°E | |
Sea Reach № 1 | Port buoy | Flashing red 2.5s | 51°29.368′N0°52.445′E / 51.489467°N 0.874083°E | Yellow pillar buoy Racon T | Flashing yellow 2.5s | 51°29.586′N0°52.710′E / 51.493100°N 0.878500°E | |
West Oaze | ̶ | ̶ | ̶ | The Oaze Deep | Red & white buoy | Isophase 5s | 51°28.975′N0°55.413′E / 51.482917°N 0.923550°E |
Oaze Bank | ̶ | ̶ | ̶ | Starboard buoy | Quick flashing green | ||
Oaze | Yellow pillar buoy | Group flashing (4) Yellow 10s | 51°28.977′N0°56.917′E / 51.482950°N 0.948617°E | ̶ | ̶ | ̶ | |
Argus | ̶ | ̶ | ̶ | Yellow pillar buoy yellow ‘X’ topmark | Flashing yellow 2.5s | 51°29.297′N0°58.715′E / 51.488283°N 0.978583°E | |
Oaze Deep | ̶ | ̶ | ̶ | Starboard buoy | Group flashing (2) green 5s | 51°30.000′N1°0.000′E / 51.500000°N 1.000000°E | |
Knob | Red & white buoy | Isophase 5s | ̶ | ̶ | ̶ | ||
SE Mouse | ̶ | ̶ | ̶ | Starboard buoy | Quick flashing green | ||
Knock John № 7 | ̶ | ̶ | ̶ | The Knock John Channel | Starboard buoy | Group flashing (4) green 15s | 51°31.956′N1°06.406′E / 51.532600°N 1.106767°E |
Knock John № 5 | ̶ | ̶ | ̶ | Starboard buoy | Group flashing (3) green 10s | 51°32.490′N1°07.750′E / 51.541500°N 1.129167°E | |
Knock John № 4 | Port buoy | Group flashing (3) red 10s | 51°32.323′N1°07.906′E / 51.538717°N 1.131767°E | ̶ | ̶ | ̶ | |
Knock John № 3 | ̶ | ̶ | ̶ | Starboard buoy | Flashing green 5s | 51°33.278′N1°09.692′E / 51.554633°N 1.161533°E | |
Knock John № 2 | Port buoy | Flashing red 5s | 51°33.112′N1°09.847′E / 51.551867°N 1.164117°E | ̶ | ̶ | ̶ | |
Knock John № 1 | ̶ | ̶ | ̶ | South cardinal buoy | Quick flashing white (6) + long flash 15s | 51°33.717′N1°10.833′E / 51.561950°N 1.180550°E | |
Knock John | Port buoy | Group flashing (2) red 5s | 51°33.661′N1°11.357′E / 51.561017°N 1.189283°E | ̶ | ̶ | ̶ | |
Black Deep № 12 | Port buoy | Group flashing (4) red 15s | 51°33.661′N1°13.511′E / 51.561017°N 1.225183°E | The Black Deep Channel | ̶ | ̶ | ̶ |
Black Deep № 11 | ̶ | ̶ | ̶ | Starboard buoy | Group flashing (3) green 10s | 51°34.250′N1°13.475′E / 51.570833°N 1.224583°E | |
Black Deep № 10 | Port buoy | Group flashing (3) red 10s | ̶ | ̶ | ̶ | ||
Black Deep № 9 | ̶ | ̶ | ̶ | South cardinal buoy | Quick flashing white (6) + long flash | ||
Inner Fisherman | Port buoy | Quick flashing red | ̶ | ̶ | ̶ | ||
Black Deep № 7 | ̶ | ̶ | ̶ | Starboard buoy | Quick flashing green | ||
Black Deep № 8 | ̶ | ̶ | ̶ | West cardinal buoy | Quick flashing white (9) 15s | ||
BDM2 | Yellow pillar buoy (mid-channel) | Flashing yellow 2.5s | 51°37.370′N1°20.040′E / 51.622833°N 1.334000°E | ̶ | ̶ | ̶ | |
Black Deep № 6 | Port buoy | Flashing red 2.5s | ̶ | ̶ | ̶ | ||
Black Deep № 5 | ̶ | ̶ | ̶ | East cardinal buoy | Very quick flashing white (3) 5s | ||
Black Deep № 4 | Port buoy | Group flashing (2) red 5s | ̶ | ̶ | ̶ | ||
BDM1 | Yellow pillar buoy (mid-channel) yellow ‘X’ topmark | Flashing yellow 2.5s | 51°41.960′N1°27.590′E / 51.699333°N 1.459833°E | ̶ | ̶ | ̶ | |
Black Deep № 3 | ̶ | ̶ | ̶ | Starboard buoy | Group flashing (3) green 15s | ||
Black Deep № 1 | ̶ | ̶ | ̶ | Starboard buoy | Flashing green 5s | ||
Black Deep № 2 | Port buoy | Group flashing (4) red 15s | ̶ | ̶ | ̶ | ||
SHM | Yellow pillar buoy (mid-channel) yellow ‘X’ topmark Racon T | Flashing yellow 2.5s | 51°46.050′N1°31.540′E / 51.767500°N 1.525667°E | ̶ | ̶ | ̶ | |
Sunk Head Tower | ̶ | ̶ | ̶ | North cardinal buoy | Quick flashing white | ||
Black Deep | Port buoy | Quick flashing red | 51°48.10′N1°36.60′E / 51.80167°N 1.61000°E | ̶ | ̶ | ̶ | |
Trinity | South cardinal buoy | Quick flashing (6) + long flash 15s | ̶ | ̶ | ̶ | ||
Dynamo | ̶ | ̶ | ̶ | Yellow pillar buoy yellow ‘X’ topmark | Flashing yellow 2.5s | 51°50.060′N1°33.880′E / 51.834333°N 1.564667°E | |
Sunk Inner | ̶ | ̶ | ̶ | Light float | Isophase 3s | 51°51.170′N1°34.400′E / 51.852833°N 1.573333°E |
The Corporation of Trinity House of Deptford Strond, also known as Trinity House, is the official authority for lighthouses in England, Wales, the Channel Islands and Gibraltar. Trinity House is also responsible for the provision and maintenance of other navigational aids, such as lightvessels, buoys, and maritime radio/satellite communication systems. It is also an official deep sea pilotage authority, providing expert navigators for ships trading in Northern European waters.
A lightvessel, or lightship, is a ship that acts as a lighthouse. They are used in waters that are too deep or otherwise unsuitable for lighthouse construction. Although some records exist of fire beacons being placed on ships in Roman times, the first modern lightship was located off the Nore sandbank at the mouth of the River Thames in London, England, by its inventor Robert Hamblin in 1734. Lightships have since been rendered obsolete by advancing lighthouse construction techniques, and by large automated navigation buoys.
The history of the many lightvessel stations of Great Britain goes back over 250 years to the placement of the world's first lightship at the Nore in the early 18th century.
The Port of London Authority (PLA) is a self-funding public trust established on 31 March 1909 in accordance with the Port of London Act 1908 to govern the Port of London. Its responsibility extends over the Tideway of the River Thames and its continuation. It maintains and supervises navigation, and protects the river's environment.
Isle of Grain is a village and the easternmost point of the Hoo Peninsula within the district of Medway in Kent, south-east England. No longer an island and now forming part of the peninsula, the area is almost all marshland and is a major habitat for diverse wetland birds. The village constitutes a civil parish, which at the 2011 census had a population of 1,648, a net decrease of 83 people in 10 years.
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.
The Nore is a long bank of sand and silt running along the south-centre of the final narrowing of the Thames Estuary, England. Its south-west is the very narrow Nore Sand. Just short of the Nore's easternmost point where it fades into the channels it has a notable point once marked by a lightship on the line where the estuary of the Thames nominally becomes the North Sea. A lit buoy today stands on this often map-marked divisor: between Havengore Creek in east Essex and Warden Point on the Isle of Sheppey in Kent.
The Maplin Sands are mudflats on the northern bank of the Thames estuary, off Foulness Island, near Southend-on-Sea in Essex, England, though they actually lie within the neighbouring borough of Rochford. They form a part of the Essex Estuaries Special Area of Conservation due to their value for nature conservation, with a large colony of dwarf eelgrass and associated animal communities.
The Tideway is the part of the River Thames in England which is subject to tides. This stretch of water is downstream from Teddington Lock. The Tideway comprises the upper Thames Estuary including the Pool of London.
The Gloucester Harbour Trustees are the competent harbour authority (CHA) for the tidal part of the River Severn from the Gloucester weirs down to seaward of the Second Severn Crossing, on the Welsh side of the Severn Estuary from the Second Severn Crossing as far as Goldcliff, and on the River Wye up to its tidal limit (Bigsweir).
The Varne Bank or Varne Shoal is a 5+3⁄4-mile (9.3 km) long sand bank in the Strait of Dover, lying 9 miles (14 km) southwest of Dover in Kent, England. With the Lobourg Channel running along it, the Varne bank lies immediately south-west of the deepest point 223 feet (68 m) in the strait of Dover. Its rectilinear shape is similar to other banks in the strait such as South Falls bank bordering the Lobourg Channel on the east, the Colbart bank and others. Rectilinear banks are only present on the English side of the strait.
The Wyre Light was a 40-foot (12 m) tall iron screw-pile lighthouse marking the navigation channel to the town of Fleetwood, Lancashire, England.
The Black Deep is in the outer Thames Estuary. It is the greatest of three mainly natural shipping channels linking the Tideway to central zones of the North Sea without shoals, the others being the Barrow Deep and Princes Channel. Between these, a few others, and the shores of Kent, Suffolk and Essex are many long shoals in the North Sea, broadly shallow enough to wreck vessels of substantial draft at low tide.
The Low Lighthouse is one of three historic lighthouses in Burnham-on-Sea, Somerset, England, and the only one of the three which is still active. It is a Grade II listed building and stands on the foreshore. First lit in 1832, the Low Lighthouse operated in conjunction with the (onshore) High Lighthouse for 137 years. Then, in 1969 the Low Lighthouse was deactivated; but later, in 1993, the Low Lighthouse was re-established and the High Lighthouse was instead decommissioned).
Gunfleet Lighthouse is a derelict screw-pile lighthouse lying in the North Sea, six miles off the coast at Frinton-on-Sea in Essex, constructed in 1850 by James Walker of Trinity House. George Henry Saunders was the contractor. Walker and Burges were the Engineers. It is 74 feet (23 m) in height and hexagonal in plan; mounted on seven piles forming a steel lattice and originally painted red. It was first lit on 1 May 1856, replacing a light vessel which had been on station there since 1850.
The Broomway, also formerly called the "Broom Road", is a public right of way over the foreshore at Maplin Sands off the coast of Essex, England. Most of the route is classed as a byway open to all traffic, with a shorter section of bridleway. When the tide is out, it provides access to Foulness Island, and was the only access to Foulness on foot, and the only access at low tide, until a road bridge was built over Havengore Creek in 1922.
The Kentish Knock is a long shoal in the North Sea east of Essex, England. It is the most easterly of those of the Thames Estuary and its core, which is shallower than 18 feet (5.5 m), extends 6 miles (9.7 km). Thus it is a major hazard to deep-draught navigation. It is exactly 28 miles (45 km) due east of Foulness Point, Essex and is centred about 15 miles (24 km) NNE of North Foreland, Kent – both are extreme points of those counties.
The Swin is a passage in the Thames estuary between Maplin Sands, Foulness Sand and Gunfleet Sand northwest and the Barrow and Sunk sand ridges (shoals), southeast. The Swin was used by barges and leisure craft from the Essex rivers, and coasters and colliers from Hull, Great Grimsby, North East England, Edinburgh and other similar sets of trading ports.
George Smeed is a Thames barge built in 1882 by Smeed Dean & Co. Ltd. in Murston.
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.
Notes
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