Aike Beck | |
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Specifications | |
Locks | 2 |
Status | defunct |
History | |
Original owner | Hotham family |
Date completed | 1790s |
Date closed | 1850s |
Geography | |
Start point | Lockington Landing |
End point | Aike |
Connects to | River Hull |
Aike Beck | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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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.
Aike Beck joined the River Hull 0.4 miles (0.64 km) above its junction with the Leven Canal. Navigable for no more than 2 miles (3.2 km) from the river, its main function was to carry coal, and it had two canal locks taking craft of 40 feet by 8 feet 10 inches (12 m x 2.7 m). [1] One was an entrance lock where the Beck joined the River Hull, and the other was about halfway along the navigation. [2] Below the middle lock, Aike Beck was enlarged, while above it, the course of the navigation was made much straighter than the original course of the beck. Coal and agricultural fertiliser was transferred from keel boats to the smaller, shallow draughted boats used on the navigation, and hauled by horse or manpower to Lockington wharf. [3]
The navigation was constructed in the late 18th century by the Hotham family who owned large amounts of land in the area. [1] Aike Beck crossed over the Beverley and Barmston Drain with the drain culverted underneath; one of eleven similar structures required to allow the drain to cross existing waterways. [note 1] In 1809 engineer William Chapman reported to the drainage commissioners that the locks on the navigation had raised water levels and caused flooding. [1]
As part of an agreement with Lord Hotham to not oppose the construction of the Hull and Selby Railway (Bridlington branch) in the 1840s, the proprietors of the line agreed not to provide coal handling facilities in the vicinity of his canal. [6]
It is thought to have ceased to be used for navigation in the 1850s, as it appears to be derelict on the 1855 Ordnance Survey map, [1] where both the second lock and the coal basin at Lockington are marked "old". [2] By the time the 1891 map was published, the final section from the beck to the coal wharf had disappeared altogether, and the lock gates must have been removed, as the beck is marked as tidal to beyond the coal wharf junction. [7]
The Beck was supplied with water by Bryan Mills Beck and Scorborough Beck. The latter was also used for navigation in the early 19th century. [8]
In 1988, Aike and Arram Beck were altered, removing Aike Beck's connection to the River Hull completely. The waters of Scorborough Beck and Bryan Mills Beck were routed southwards along a catchwater drain, which runs beside the railway line to join Arram Beck. The original course of the navigation was largely filled in, using material from the embankments on either side of the channel. All that remains is a small section containing water near Beck Lane in Aike, [9] and a slight indentation in the bank of the Hull where Aike Beck used to enter.
The former junction of Aike Beck with the river marks the point at which the Driffield Navigation, upstream from the junction, becomes the River Hull, below it.
Point | Coordinates (Links to map resources) | OS Grid Ref | Notes |
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Lockington Landing | 53°54′28″N0°26′14″W / 53.9077°N 0.4373°W | TA027468 | Coal wharf |
Second lock | 53°54′08″N0°25′07″W / 53.9022°N 0.4186°W | TA040462 | |
Entrance lock | 53°53′45″N0°23′47″W / 53.8959°N 0.3964°W | TA054456 | Jn with River Hull |
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.
Arram Beck is a small stream in the East Riding of Yorkshire, England, running through high embankments and flowing eastwards from the village of Arram to join the River Hull. Depths are variable due to the tidal nature of the Hull. It provides habitat for a variety of fish species and chub have also been stocked here too.
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.
Aike is a hamlet and former civil parish, now in the parish of Lockington, in the East Riding of Yorkshire, England. The hamlet is centred around a single developed street, which lies to the east of the Yorkshire Wolds. Aike is approximately 4 miles (6 km) north of Beverley and approximately 0.4 miles (1 km) from the west bank of the River Hull. It is approached by a 2.5-mile (4 km) lane which is a no-through road that does not continue beyond the village, although a farm track continues as far as a bridge across the Beverley and Barmston Drain. In 1931 the parish had a population of 48.
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The Hull–Scarborough line, also known as the Yorkshire Coast Line, is a railway line in Yorkshire, England that is used primarily for passenger traffic. It runs northwards from Hull Paragon via Beverley and Driffield to Bridlington, joining the York–Scarborough line at a junction near Seamer before terminating at Scarborough railway station.
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.
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The Stainforth and Keadby Canal is a navigable canal in South Yorkshire and Lincolnshire, England. It connects the River Don Navigation at Bramwith to the River Trent at Keadby, by way of Stainforth, Thorne and Ealand, near Crowle. It opened in 1802, passed into the control of the River Don Navigation in 1849, and within a year was controlled by the first of several railway companies. It became part of the Sheffield and South Yorkshire Navigation, an attempt to remove several canals from railway control, in 1895. There were plans to upgrade it to take larger barges and to improve the port facilities at Keadby, but the completion of the New Junction Canal in 1905 made this unnecessary, as Goole could easily be reached and was already a thriving port.
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