Kingston upon Hull, usually shortened to Hull, is a port city and unitary authority area in the East Riding of Yorkshire, England. It lies upon the River Hull at its confluence with the Humber Estuary, 25 miles (40 km) inland from the North Sea and 37 miles (60 km) south-east of York, the historic county town. With a population of 268,852 (2022), it is the fourth-largest city in the Yorkshire and the Humber region after Leeds, Sheffield and Bradford. Hull has more than 800 years of seafaring history and is known as Yorkshire's maritime city.
Spurn is a narrow sand tidal island located off the tip of the coast of the East Riding of Yorkshire, England that reaches into the North Sea and forms the north bank of the mouth of the Humber Estuary. It was a spit with a semi-permanent connection to the mainland, but a storm in 2013 made the road down to the end of Spurn impassable to vehicles at high tide.
The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers Ouse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length.
The East Riding of Yorkshire, often abbreviated to the East Riding or East Yorkshire, is a ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and west, South Yorkshire to the south-west, and Lincolnshire to the south across the Humber Estuary. The city of Kingston upon Hull is the largest settlement.
The Humber Forts are two large fortifications in the mouth of the Humber Estuary in northern England: Bull Sand Fort and Haile Sand Fort.
Humberside was a non-metropolitan and ceremonial county in Northern England from 1 April 1974 until 1 April 1996. It was composed of land from either side of the Humber, created from portions of the East Riding of Yorkshire, West Riding of Yorkshire, and the northern part of Lindsey, Lincolnshire. The county council's headquarters was County Hall at Beverley, inherited from East Riding County Council. Its largest settlement and only city was Kingston upon Hull. Other notable towns included Goole, Beverley, Scunthorpe, Grimsby, Cleethorpes and Bridlington. The county stretched from Wold Newton at its northern tip to a different Wold Newton at its southernmost point.
Holderness is an area of the East Riding of Yorkshire, on the north-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. Holderness generally refers to the area between the River Hull and the North Sea. The Prime Meridian passes through Holderness just to the east of Patrington and through Tunstall to the north.
Hedon is a town and civil parish in Holderness in the East Riding of Yorkshire, England. It is situated approximately 5 miles (8 km) east of Hull city centre. It lies to the north of the A1033 road at the crossroads of the B1240 and B1362 roads. It is particularly noted for the parish church of St. Augustine, known as the 'King of Holderness', which is a Grade I listed building.
Easington is a small village and civil parish in the East Riding of Yorkshire, England, in the area known as Holderness. A coastal settlement, it is situated between the Humber estuary and the North Sea at the south-eastern corner of the county, and at the end of the B1445 road from Patrington. The coastal town of Withernsea is approximately 6 miles (10 km) to the north-east.
Paull is a village and civil parish in Holderness, in the East Riding of Yorkshire, England, lying on the north bank of the Humber Estuary, east of the watercourse known as Hedon Haven.
Ravensrodd, also spelt Ravenser Odd, was a constituency of the House of Commons of the Parliament of England, first represented in the Model Parliament of 1295. It was represented by two Members of Parliament intermittently, with the last known representation being in the Parliament of 1344.
Ravenspurn was a town in the East Riding of Yorkshire, England, which was lost due to coastal erosion, one of more than 30 along the Holderness Coast which have been lost to the North Sea since the 19th century. The town was located close to the end of a peninsula near Ravenser Odd, which had been flooded in the 14th century. The peninsula still survives and is known as Spurn Head. The North Sea lies to the east of the peninsula, the Humber estuary to the west.
The East Riding of Yorkshire is a local government district with unitary authority status, and is a ceremonial county of England. It is named after the historic East Riding of Yorkshire which was one of three ridings alongside the North Riding and West Riding, which were constituent parts a Yorkshire ceremonial and administrative county until 1974. From 1974 to 1996 the area of the modern East Riding of Yorkshire constituted the northern part of Humberside.
Lime Kiln Creek was an outlet onto the Humber Estuary in Kingston upon Hull, England, thought to be a previous outlet of the River Hull onto the estuary. It was blocked off during the construction of the Albert Dock in the 1860s.
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 Yorkshire Coast runs from the Tees estuary to the Humber estuary, on the east coast of England. The cliffs at Boulby are the highest on the east coast of England, rising to 660 feet (200 m) above the sea level.
Humber Lifeboat Station is an All-weather lifeboat station based at the mouth of the River Humber.
The Yorkshire coast fishery has long been part of the Yorkshire economy for centuries. The 114-mile (183 km) Yorkshire Coast, from the River Tees to the Humber estuary, has many ports both small and large where the fishing trade thrives. The historic ports at Hull and Whitby are important locations for the landing and processing of fish and shellfish. Scarborough and Bridlington are also sites of commercial fishing.
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.
Coastal erosion in Yorkshire has been a process that has been documented since Roman times. Rates of erosion on the Holderness coast are known to be the worst within Europe, with the East Riding coastlines having the greatest number of at risk properties in England. Almost 30 settlements on the Holderness coastline have been lost to the sea, with more being subjected to flooding and loss exacerbated by a projected rise in the sea level caused by climate change. Due to the limited protection from effects of rising seas in the Humber Estuary, the region has the greatest value of assets at risk from flooding than anywhere else in England.
