The Aire and Calder Navigation is the canalised section of the Rivers Aire and Calder in West Yorkshire, England. The first improvements to the rivers above Knottingley were completed in 1704 when the Aire was made navigable to Leeds and the Calder to Wakefield, by the construction of 16 locks. Lock sizes were increased several times, as was the depth of water, to enable larger boats to use the system. The Aire below Haddlesey was bypassed by the opening of the Selby Canal in 1778. A canal from Knottingley to the new docks and new town at Goole provided a much shorter route to the River Ouse from 1826. The New Junction Canal was constructed in 1905, to link the system to the River Don Navigation, by then part of the Sheffield and South Yorkshire Navigation.
The River Hull is a navigable river in the East Riding of Yorkshire in Northern England. It rises from a series of springs to the west of Driffield, and enters the Humber Estuary at Kingston upon Hull. Following a period when the Archbishops of York charged tolls for its use, it became a free navigation. The upper reaches became part of the Driffield Navigation from 1770, after which they were again subject to tolls, and the section within the city of Hull came under the jurisdiction of the Port of Hull, with the same result.
The Leven Canal runs for 3.18 miles (5.1 km) from the River Hull to the village of Leven, East Riding of Yorkshire, England. It was built for Mrs Charlotta Bethell in 1805, and remained in use until 1935. It is now a Site of Special Scientific Interest.
The Driffield Navigation is an 11-mile (18-kilometre) waterway, through the heart of the Holderness Plain to the market town of Driffield, East Riding of Yorkshire, England. The northern section of it is a canal, and the southern section is part of the River Hull. Construction was authorised in 1767, and it was fully open in 1770. Early use of the navigation was hampered by a small bridge at Hull Bridge, which was maintained by Beverley Corporation. After protracted negotiation, it was finally replaced in 1804, and a new lock was built to improve water levels at the same time. One curious feature of the new works were that they were managed quite separately for many years, with the original navigation called the Old Navigation, and the new works called the New Navigation. They were not fully amalgamated until 1888.
The Sheffield & Tinsley Canal is a canal in the City of Sheffield, England. It runs 3.9 miles (6.3 km) from Tinsley, where it leaves the River Don, to the Sheffield Canal Basin in the city centre, passing through 11 locks. The maximum craft length that can navigate this lock system is 61 feet 6 inches (18.75 m) with a beam of 15 feet 6 inches (4.72 m).
The Yorkshire Ring is a canal ring in South and West Yorkshire, England. It was completed in 1905 with the construction of the New Junction Canal. It lasted for under thirty years before the closure of part of the Dearne and Dove Canal and subsequently the complete Barnsley Canal. Both these canals are currently under restoration.
The Market Weighton Canal ran 9.5 miles (15.3 km) from the Humber Estuary to its terminus near Market Weighton. It gained its Act of Parliament in 1772 and opened in 1782. The 3.5 miles (5.6 km) closest to Market Weighton was abandoned in 1900 and the right of navigation through Weighton lock was lost in 1971. However, as of 2002 the lock was passable and the canal usable up to the junction with the River Foulness where silt has made it impassable. Also there is no right of navigation under the M62 motorway bridge to the north of Newport.
Aike Beck or the Lockington Navigation was a stream in the East Riding of Yorkshire, England, which was constructed as a navigation in the late 18th century, and ceased to function as such in the 1850s. The water supply came from Bryan Mills Beck and Scorborough Beck, but in 1988, these were diverted to feed into Arram Beck, and most of the channel was filled in with material from the flood banks.
Wilfholme Landing is located on the Driffield Navigation in the East Riding of Yorkshire, England. The navigation is still tidal at this point, and is often considered to still be the River Hull, although technically the Navigation starts at the point where the Aike Beck used to join the river, a little further downstream. It is 0.9 miles (1.4 km) from the hamlet of Wilfholme, and its main features are boat moorings, a farm and a pumping station. It is a popular spot for fishing, with anglers targeting resident roach, bream and perch.
West Beck is the common name given to the upper section of the old River Hull, as it rises in the foothills of the Yorkshire Wolds. After reaching Frodingham Beck at Emmotland, it becomes called the River Hull. It is noteworthy for being the most northerly chalk stream in England. It provides fly fishing for wild brown trout and grayling.
The Pocklington Canal is a broad canal which runs for 9.5 miles (15.3 km) through nine locks from the Canal Head near Pocklington in the East Riding of Yorkshire, England, to the River Derwent which it joins near East Cottingwith. Most of it lies within a designated Site of Special Scientific Interest.
Hull Bridge is a village in the East Riding of Yorkshire, England. It is situated approximately 1.5 miles (2.4 km) north-east of Beverley town centre. It lies south of the A1035 road and straddles the Beverley and Barmston Drain and the River Hull from which it takes its name.
Foston on the Wolds is a village and civil parish in the East Riding of Yorkshire, England. It is situated approximately 8 miles (13 km) south-west of Bridlington town centre and 2 miles (3 km) north of the village of North Frodingham.
Beverley Beck is a short canal in the East Riding of Yorkshire, England. The beck runs from Grovehill Lock on the River Hull at Beverley west for about 0.8 miles (1.3 km) into the town of Beverley. Until 1802, the beck was tidal, but the Beverley and Barmston Drain needed to pass under it, and the lock was constructed to maintain water levels over its tunnel. In 1898, a steam engine was installed, which could be used to top up the water levels in the beck by pumping water from the River Hull. A multimillion-pound refurbishment of the area concluded in 2007, with the refurbishment of the lock gates and pumping engine.
The Ripon Canal is located in North Yorkshire, England. It was built by the canal engineer William Jessop to link the city of Ripon with the navigable section of the River Ure at Oxclose Lock, from where boats could reach York and Hull. It opened in 1773 and was a moderate success. It was sold to the Leeds and Thirsk Railway in 1847 and was effectively closed by 1906 owing to neglect. It was not nationalised with most canals and railways in 1948 and was abandoned in 1956.
The Rother Link is a planned English canal that would connect the Chesterfield Canal at Killamarsh, via the River Rother through to the Sheffield and South Yorkshire Navigation, thus creating a new cruising ring and encouraging boats to visit the Chesterfield Canal.
William Chapman (1749–1832) was an English engineer. Born in Whitby, he worked on the construction of the Old and Humber Docks in Hull, as well as many drainage and canal projects. He is credited with the invention of the bogie and articulation for rail vehicles.
Holderness Drain is the main feature of a Land Drainage scheme for the area of Holderness to the east of the River Hull in the East Riding of Yorkshire, England. Construction began in 1764, and several notable civil engineers were involved with the scheme over the years. Despite the high costs of the initial scheme, it was not particularly successful, because of the refusal of the ship owners of Hull to allow an outlet at Marfleet. They insisted that the water be discharged into the River Hull to keep the channel free of silt. Following a period of agricultural depression and the building of new docks in the early 1800s, an outlet at Marfleet was finally authorised in 1832. A high level system still fed upland water to the Hull, but the low level system discharged into the Humber, where levels were considerably lower. Following the success of steam pumping on the Beverley and Barmston Drain, the trustees looked at such a possibility for the Holderness Drain, but the development of the Alexandra Dock in the 1880s and then the King George V Dock in 1913 provided a solution, as the docks were topped up with water pumped from the drain, to lessen the ingress of silt-laden water.
The Beverley and Barmston Drain is the main feature of a land drainage scheme authorised in 1798 to the west of the River Hull in the East Riding of Yorkshire, England. The area consisted of salt marshes to the south and carrs to the north, fed with water from the higher wolds which lay to the north, and from inundation by tidal water passing up the river from the Humber. Some attempts to reduce the flooding by building embankments had been made by the fourteenth century, and windpumps appeared in the seventeenth century. The Holderness Drainage scheme, which protected the area to the east of the river, was completed in 1772, and attention was then given to resolving flooding of the carrs.
Hedon Haven is a waterway that connected the Humber Estuary with the port of Hedon, in Holderness, East Riding of Yorkshire, England. The waterway allowed ships to unload at the port in Hedon, which was also known as Hedon Haven and had, at its peak, three canalised arms that stretched into the town. The port at Hedon was the main port for south Holderness between the 12th and 13th centuries, and was the busiest port in Holderness before the docks at Hull were built.
