River Welland in the context of "Fosdyke"

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⭐ Core Definition: River Welland

The River Welland is a lowland river in the east of England, some 65 miles (105 km) long. It drains part of the Midlands eastwards to The Wash. The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke. It is a major waterway across the part of the Fens called South Holland, and is one of the Fenland rivers that were laid out with washlands. There are two channels between widely spaced embankments with the intention that flood waters would have space in which to spread while the tide in the estuary prevented free egress. However, after the floods of 1947, new works such as the Coronation Channel were constructed to control flooding in Spalding, and the washlands are no longer used solely as pasture, but may be used for arable farming.

Significant improvements were made to the river in the 1660s, when a new cut with 10 locks was constructed between Stamford and Market Deeping, and two locks were built on the river section below Market Deeping. The canal section was known as the Stamford Canal, and was the longest canal with locks in Britain when it was built. The river provided the final outlet to the sea for land drainage schemes implemented in the seventeenth century, although they were not completely successful until a steam-powered pumping station was built at Pode Hole in 1827. Navigation on the upper river, including the Stamford Canal, had ceased by 1863, but Spalding remained an active port until the end of the Second World War.

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River Welland in the context of The Wash

The Wash is a shallow natural rectangular bay and multiple estuary on the east coast of England in the United Kingdom. It is an inlet of the North Sea and is the largest multiple estuary system in the UK, as well as being the largest natural bay in England and is the outflow for the rivers Witham, Welland, Nene and the Great Ouse. It is also one of the most important places of conservation in Europe, with several nature reserves located within this area.

The coastline is partly in Lincolnshire and partly in Norfolk. The Lincolnshire side forms part of the only coastline of the East Midlands region whilst the Norfolk side forms the north-west corner of the East Anglian region. The coastline stretches from Gibraltar Point just south of the seaside town of Skegness to Gore Point near the village of Holme-next-the-Sea, just east of the seaside town of Hunstanton in Norfolk. These two points are over 75 miles (121 km) from each other by road, but only eleven and a half miles (18.5 km) by sea.

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River Welland in the context of Ely, Cambridgeshire

Ely (/ˈli/ EE-lee) is a cathedral city and civil parish in the district of East Cambridgeshire in Cambridgeshire, England, 14 miles (23 km) northeast of Cambridge, 24 miles (39 km) southeast of Peterborough and 80 miles (130 km) from London. At the 2021 census, the built-up area had a population of 19,200. The parish which includes the villages of Chettisham, Prickwillow, Queen Adelaide and Stuntney and the hamlet of Mile End had a population of 20,574 in 2021.

Ely is built on a 23-square-mile (60 km) Kimmeridge Clay island which, at 85 feet (26 m), is the highest land in the Fens. It was due to this topography that Ely was not waterlogged like the surrounding Fenland, and an island separated from the mainland. Major rivers including the Witham, Welland, Nene and Great Ouse feed into the Fens and, until draining commenced in the eighteenth century, formed freshwater marshes and meres within which peat was laid down. Once the Fens were drained, this peat created a rich and fertile soil ideal for farming.

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