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Spurn
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 island is over long, almost half the width of the estuary at that point, and as little as wide in places. The southernmost tip is known as Spurn Head or Spurn Point and is the home to an RNLI lifeboat station and two disused lighthouses. It forms part of the civil parish of Easington. Spurn Head covers above high water and of foreshore. It has been owned since 1960 by the Yorkshire Wildlife Trust and is a designated national nature reserve, heritage coast and is part of the Humber Flats, Marshes and Coast Special Protection Area. History Spurn Head was known to classical authors, such as Ptolemy as ''Oc ...
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Spurn Point Lighthouse
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 island is over long, almost half the width of the estuary at that point, and as little as wide in places. The southernmost tip is known as Spurn Head or Spurn Point and is the home to an RNLI lifeboat station and two disused lighthouses. It forms part of the civil parish of Easington. Spurn Head covers above high water and of foreshore. It has been owned since 1960 by the Yorkshire Wildlife Trust and is a designated national nature reserve, heritage coast and is part of the Humber Flats, Marshes and Coast Special Protection Area. History Spurn Head was known to classical authors, such as Ptolemy as ''Ocel ...
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Spurn 8
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 island is over long, almost half the width of the estuary at that point, and as little as wide in places. The southernmost tip is known as Spurn Head or Spurn Point and is the home to an RNLI lifeboat station and two disused lighthouses. It forms part of the civil parish of Easington. Spurn Head covers above high water and of foreshore. It has been owned since 1960 by the Yorkshire Wildlife Trust and is a designated national nature reserve, heritage coast and is part of the Humber Flats, Marshes and Coast Special Protection Area. History Spurn Head was known to classical authors, such as Ptolemy as ''Ocel ...
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Spurn Head Settlement
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 island is over long, almost half the width of the estuary at that point, and as little as wide in places. The southernmost tip is known as Spurn Head or Spurn Point and is the home to an RNLI lifeboat station and two disused lighthouses. It forms part of the civil parish of Easington. Spurn Head covers above high water and of foreshore. It has been owned since 1960 by the Yorkshire Wildlife Trust and is a designated national nature reserve, heritage coast and is part of the Humber Flats, Marshes and Coast Special Protection Area. History Spurn Head was known to classical authors, such as Ptolemy as ''Ocel ...
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Humber Lifeboat Station
The Humber Lifeboat Station is located on Spurn Point in the East Riding of Yorkshire, England. The station is one of nine Royal National Lifeboat Institution (RNLI) lifeboat stations situated along the Yorkshire Coast and the most southerly of them all. It is the only lifeboat station in the United Kingdom that is staffed full-time by a professional RNLI crew; this is due to the waters around this part of the coast being so dangerous and the station's remoteness from the mainland. A lifeboat station has been located on Spurn Point since 1810, the crews have been awarded 33 RNLI medals for gallantry. The current lifeboat is the ''Pride of the Humber'', a Lifeboat. History A lifeboat station was established in 1810 at Spurn Point with a crew supplied by Hull Trinity House. A decommissioned gun battery emplacement, last used in 1809, was requisitioned as the main lifeboat building and was also partly converted into the ''Life Boat House Hotel''. The crew of the lifeboat were bil ...
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Holderness
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. From 1974 to 1996 Holderness lay within the Borough of Holderness in Humberside. It gave its name to a wapentake until the 19th century, when its functions were replaced by other local government bodies, particularly after the 1888 Local Government Act. The city of Kingston upon Hull lies in the south-west corner of Holderness and Bridlington borders the north-east but both are usually considered separately. The main towns include Withernsea, Hornsea ...
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Humber Estuary
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. Although the Humber is an estuary from the point at which it is formed, many maps show it as the River Humber. Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the Port ...
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Ravenspurn
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 has also been flooded. The peninsula still survives and is known as Spurn Head. The North Sea lies to the east of the peninsula, the river Humber to the west. The nearest major city was Kingston upon Hull. The region of coastline is known as the Holderness Coast; geologically the land is formed of glacial tills (boulder clay), which are subject to coastal erosion. Now at sea, areas around the site are being drilled for natural gas. Ravenspurn appears in William Shakespeare's plays ''Richard II'', ''Henry IV, Part 1'', and ''Henry VI, Part 3'', under the spelling "Ravenspurgh". Two medieval English kings landed at Ravenspurn: Henry IV in 1399, on his way to dethrone Richard II, and Edward I ...
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East Riding Of Yorkshire
The East Riding of Yorkshire, or simply East Riding or East Yorkshire, is a ceremonial county and unitary authority area 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. The coastal towns of Bridlington, Hornsea and Withernsea are popular with tourists, the town of Howden contains Howden Minster, Market Weighton, Pocklington, Brough, Hedon and Driffield are market towns with markets held throughout the year and Hessle and Goole are important port towns for the county. The port city of Kingston upon Hull is an economic, transport and tourism centre which also receives much sea freight from around the world. The current East Riding of Yorkshire came into existence in 1996 after the abolition of the County of Humberside. The county's administration is in the ancient market town of Beverley. The landscape is mainly rural, consisting of rolling hills, valley ...
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Easington, East Riding Of Yorkshire
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 to the north-east. The civil parish is formed by the village of Easington and the hamlets of Kilnsea, Out Newton and Spurn Head. Bull Sand Fort is administered as part of the parish. According to the 2011 UK Census, Easington parish had a population of 691, a small decrease on the 2001 UK Census figure of 698. The parish church of All Saints' is a Grade I listed building. In 1823 the ecclesiastical parish incumbency was a perpetual curacy under the patronage of the Archbishop of York. The parish had a population of 488, with occupations that included a butcher, a corn miller, a weaver, two blacksmiths, two wheelwrights, two grocers, ...
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Ravenser Odd
Ravenser Odd, also spelled Ravensrodd, was a port in the East Riding of Yorkshire, England, during the medieval period, built on the sandbanks at the mouth of the Humber estuary. The name Ravenser comes from the Old Norse or 'Raven's tongue' referring to the lost sandbank promontory, the modern successor of which is now known as Spurn Point. The town was founded by the Count of Aumale in the mid-13th century, and had more than 100 houses and a flourishing market by 1299, when it was granted a borough charter. The town had wharves, warehouses, a court and a prison. It collected dues from more than 100 merchant ships a year. In the 13th century the town was a more important port than Kingston upon Hull further up the Humber, and sent two members to the Model Parliament of 1295. As the sandbanks shifted the town was swept away. Storms over the winter of 1356–57 completely flooded the town, leading to its abandonment, and it was largely destroyed by the storm or Saint Marcellu ...
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Yorkshire Wildlife Trust
The Yorkshire Wildlife Trust is a charitable non-governmental organisation, one of the UK's 46 county-based Wildlife Trusts. It's focus is nature conservation and it works to achieve a nature-rich Yorkshire with healthy and resilient ecosystems that support both Yorkshire's wildlife and its people. It works across the ceremonial county's of East, North, South, and West Yorkshire; with the exception of the Sheffield District and some of Rotherham District, where the separate Sheffield and Rotherham Wildlife Trust operates, and the Unitary Authorities of Middlesbrough, Redcar and Cleveland, and Stockton-on-Tees, where the separate Tees Valley Wildlife Trust operates. The second oldest Wildlife Trust, having been originally formed as the Yorkshire Naturalists Trust in 1946, it is now one of the largest Wildlife Trusts with an income of over £13 million, and over 150 staff. The Trust is a membership organisation and has grown to become one of the largest civil society organisa ...
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Spit (landform)
A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sediment in the direction the waves are breaking, forming an above-water spit. Without the co ...
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