The East Riding of Yorkshire, or simply East Riding or East Yorkshire, is a county in Northern England. At the 2011 United Kingdom census, its population was 334,179.
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.
Holderness is an area of the East Riding of Yorkshire, on the east coast of England. An area of rich agricultural land, Holderness was marshland until it was drained in the Middle Ages. Topographically, Holderness has more in common with the Netherlands than with other parts of Yorkshire. To the north and west are the Yorkshire Wolds. The Prime Meridian passes through Holderness just to the east of Patrington and through Tunstall to the north.
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.
Adlingfleet is a drained, fertile, former marshland village in the East Riding of Yorkshire, England, that forms part of the civil parish of Twin Rivers. It is 6.5 miles (10.5 km) east-southeast of Goole town centre. Its sea wall along the far north-east is set back from the Ouse estuary leaving the largest single reedbed in England.
Aike measuring approximately 0.6 miles (1 km) by 1,600 feet (500 m), is a hamlet, locally known as a village, 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.
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.
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.
Wilfholme is a hamlet in the East Riding of Yorkshire, England. It forms part of the civil parish of Beswick, and is situated just east from the A164 road, approximately 5 miles (8 km) north from Beverley and 6 miles (10 km) south from Driffield. Wilfholme Landing is 0.9 miles (1.4 km) to the south-east and provides access to the Driffield Navigation.
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.
Dunswell is a village in the East Riding of Yorkshire, England, and in the civil parish of Woodmansey.
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 River Foulness is a river in the East Riding of Yorkshire, England. Its name is derived from Old English fūle[n] ēa, meaning “dirty water”. Maintenance responsibilities for the river transferred from the Environment Agency to the Market Weighton Drainage Board on 1 October 2011. Market Weighton Drainage Board subsequently amalgamated with the Lower Ouse Internal Drainage Board on 1 April 2012 to create the Ouse and Humber Drainage Board. The river discharges into the Humber Estuary via Market Weighton Canal. Water levels within the river, its tributaries and the canal are managed and controlled by the Environment Agency. The river lies in an area known as the Humberhead Levels.
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.
