Waterway | Regent's Canal |
---|---|
County | Tower Hamlets Greater London |
Maintained by | Canal & River Trust |
Operation | Assisted |
First built | 1820 |
Latest built | 1989 |
Length | 100 feet (30.5 m) |
Width | 30 feet (9.1 m) |
Fall | tidal |
Distance to Paddington Basin | 9 miles (14.5 km) |
Coordinates | 51°30′36″N0°02′12″W / 51.510098°N 0.036693°W Coordinates: 51°30′36″N0°02′12″W / 51.510098°N 0.036693°W |
Limehouse Basin Lock is a lock forming the exit from Limehouse Basin to the Thames, in the London Borough of Tower Hamlets, England. [1] It is the final lock on the Regent's Canal. The Narrow Street swing bridge sits between the lock and the river.
The current lock was built in 1989 for yachts and pleasure craft, to conserve water in the Basin. It measures 100 feet (30.5 m) by 30 feet (9.1 m) and was built completely within the chamber of the former Ship Lock entrance to the basin. This measured 350 feet (106.7 m) by 60 feet (18.3 m). The original gate-recesses and one of the gates remain in situ, to demonstrate the size of the former lock.
The nearest Docklands Light Railway station is Limehouse.
Limehouse is a district in the London Borough of Tower Hamlets in East London. It is 3.9 miles (6.3 km) east of Charing Cross, on the northern bank of the River Thames. Its proximity to the river has given it a strong maritime character, which it retains through its riverside public houses and steps, such as The Grapes and Limehouse Stairs. It is part of the traditional county of Middlesex. It became part of the ceremonial County of London following the passing of the Local Government Act 1888, and then part of Greater London in 1965. It is located between Stepney to the west and north, Mile End and Bow to the northwest, Poplar to the east, and Canary Wharf and Millwall to the south, and stretches from the end of Cable Street and Butcher Row in the west to Stainsby Road near Bartlett Park in the east, and from West India Dock and the River Thames in the south to Salmon Lane and Rhodeswell Road in the north.
The Forth and Clyde Canal is a canal opened in 1790, crossing central Scotland; it provided a route for the seagoing vessels of the day between the Firth of Forth and the Firth of Clyde at the narrowest part of the Scottish Lowlands. This allowed navigation from Edinburgh on the east coast to the port of Glasgow on the west coast. The canal is 35 miles (56 km) long and it runs from the River Carron at Grangemouth to the River Clyde at Bowling, and had an important basin at Port Dundas in Glasgow.
The Limehouse Cut is a largely straight, broad canal in the East End of London which links the lower reaches of the Lee Navigation to the River Thames. Opening on 17 September 1770, and widened for two-way traffic by 1777, it is the oldest canal in the London area. Although short, it has a diverse social and industrial history. Formerly discharging directly into the Thames, since 1968 it has done so indirectly by a connection through Limehouse Basin.
Limehouse Basin, a navigable link between the River Thames and two of London's canals, is a body of water 2 miles east of London Bridge. First dug in 1820 as the eastern terminus of the new Regent's Canal, its wet area was less than 5 acres originally, but it was gradually enlarged in the Victorian era, reaching a maximum of double that size, when it was given its characteristic oblique entrance lock, big enough to admit 2,000-ton ships. Throughout its working life the basin was better known as the Regent's Canal Dock, and was used to transship goods between the old Port of London and the English canal system. Cargoes handled were chiefly coal and timber, but also ice, circus animals, and even Russian oil and WW1 submarines. Sailing ships delivered cargoes there until WW2, and can be seen in surviving films and paintings.
Regent's Canal is a canal across an area just north of central London, England. It provides a link from the Paddington Arm of the Grand Union Canal, 550 yards (500 m) north-west of Paddington Basin in the west, to the Limehouse Basin and the River Thames in east London. The canal is 8.6 miles (13.8 km) long.
The Hertford Union Canal or Duckett's Cut, just over 1 mile (1.6 km) long, connects the Regent's Canal to the Lee Navigation in the London Borough of Tower Hamlets in East London. It was opened in 1830 but quickly proved to be a commercial failure. It was acquired by the Regents Canal Company in 1857, and became part of the Grand Union Canal in 1927.
The Lee Navigation is a canalised river incorporating the River Lea. It flows from Hertford Castle Weir to the River Thames at Bow Creek; its first lock is Hertford Lock and its last Bow Locks.
The Huddersfield Narrow Canal is an inland waterway in northern England. It runs just under 20 miles (32 km) from Lock 1E at the rear of the University of Huddersfield campus, near Aspley Basin in Huddersfield, to the junction with the Ashton Canal at Whitelands Basin in Ashton-under-Lyne. It crosses the Pennines by means of 74 locks and the Standedge Tunnel.
Bow Creek is a 2.25-mile (3.6 km) long tidal estuary of the English River Lea and is part of the Bow Back Rivers. Below Bow Locks the creek forms the boundary between the London Boroughs of Newham and Tower Hamlets, in East London.
City Mill River is part of the Bow Back Rivers in London, England. It formerly fed City Mill, used for the production of chemicals in the late nineteenth and early twentieth centuries. In the 1930s, the mill was removed and the river was isolated from the tides by the construction of locks at both ends. City Mill Lock, at the southern end, has been refurbished and reopened in 2010.
The Grand Surrey Canal was a canal constructed in south London, England during the early 19th century. It opened to the Old Kent Road in 1807, to Camberwell in 1810, and to Peckham in 1826. Its main purpose was to transport cargo, primarily timber from the Surrey Commercial Docks.
Grosvenor Canal was a canal in the Pimlico area of London, opened in 1824. It was progressively shortened, as first the railways to Victoria Station and then the Ebury Bridge housing estate were built over it. It remained in use until 1995, enabling barges to be loaded with refuse for removal from the city, making it the last canal in London to operate commercially. A small part of it remains among the Grosvenor Waterside development.
Gas Street Basin is a canal basin in the centre of Birmingham, England, where the Worcester and Birmingham Canal meets the BCN Main Line. It is located on Gas Street, off Broad Street, and between the Mailbox and Brindleyplace canal-side developments.
Bow Locks (No20) is a set of bi-directional locks in Bromley-by-Bow in the London Borough of Tower Hamlets and Newham. The locks link the tidal Bow Creek to the River Lee Navigation, which is a canalised river. These locks were first built in 1850 and then rebuilt in 1930, at the same time as the Prescott Channel was cut nearby. At high tide, the tide from Bow Creek formerly flowed through Bow Locks, to raise the level of the canals, such as the Limehouse Cut. In 2000, these locks were modified to keep the tide out, to reduce silting in the canal system.
Britannia Stop Lock was a lock on the Limehouse Cut in the London Borough of Tower Hamlets. It was built in 1853. The gates were either side of Commercial Road bridge and were oriented such that a boat travelling from south-west to north-east would ascend in height.
St Pancras Lock is a lock on the Regent's Canal, in the London Borough of Camden, England. The St Pancras Basin is nearby.
City Road Lock is a lock on the Regent's Canal, in the London Borough of Islington, England. It is located a short distance to the east of Islington Tunnel, and immediately to the west of City Road Basin.
Commercial Road Lock is a lock on the Regent's Canal in the London Borough of Tower Hamlets. It marks the point at which the canal enters Limehouse Basin, and is the penultimate lock before the canal reaches the Thames.
Maida Hill Tunnel is a canal tunnel on the Regent's Canal in London, England. The two other tunnels on the Regent's Canal are Islington Tunnel and Eyre's Tunnel.