The Fens

The Fens, also known as the Fenlands, are a coastal plain in eastern England. This natural marshy region supported a rich ecology and numerous species, as well as absorbing storms. Most of the fens were drained several centuries ago, resulting in a flat, dry, low-lying agricultural region supported by a system of drainage channels and man-made rivers (dykes and drains) and automated pumping stations. There have been unintended consequences to this reclamation, as the land level has continued to sink and the dykes must be built higher to protect it from flooding.

A fen is the local term for an individual area of marshland or former marshland. It also designates the type of marsh typical of the area, which has neutral or alkaline water chemistry and relatively large quantities of dissolved minerals, but few other plant nutrients.

Fenland primarily lies around the coast of the Wash, occupying an area of nearly 1,500 sq mi (3,900 km2) in Lincolnshire, Cambridgeshire, and Norfolk.[2]

Most of the Fenland lies within a few metres of sea level. As with similar areas in the Netherlands, much of the Fenland originally consisted of fresh- or salt-water wetlands. These have been artificially drained and continue to be protected from floods by drainage banks and pumps. With the support of this drainage system, the Fenland has become a major arable agricultural region in Britain for grains and vegetables. The Fens are particularly fertile, containing around half of the grade 1 agricultural land in England.

The Fens have been referred to as the "Holy Land of the English" because of the former monasteries, now churches and cathedrals, of Crowland, Ely, Peterborough, Ramsey and Thorney. Other significant settlements in the Fens include Boston, Cambridge, Spalding, and Wisbech.[3][4]

The Fens
Wicken Fen
Map of eastern England, showing position of the Fens.[1]
Map of eastern England, showing position of the Fens.[1]
CountryUnited Kingdom
Constituent countryEngland
RegionEast of England and East Midlands
CountiesLincolnshire, Cambridgeshire, Norfolk; parts of Suffolk and Huntingdonshire
Area
 • Total1,500 sq mi (3,900 km2)
Time zoneUTC±0 (Greenwich Mean Time)
 • Summer (DST)UTC+1 (British Summer Time)
Websitevisitcambridgeshirefens.org

Background: historical flooding and drainage

The Fens are very low-lying compared with the chalk and limestone uplands that surround them – in most places no more than 10 m above sea level. As a result of drainage and the subsequent shrinkage of the peat fens, many parts of the Fens now lie below mean sea level. Although one writer in the 17th century described the Fenland as entirely above sea level (in contrast to the Netherlands),[5] the area now includes the lowest land in the United Kingdom. Holme Fen in Cambridgeshire, is around 2.75 metres below sea level.[6] Within the Fens are a few hills, which have historically been called "islands", as they remained dry when the low-lying fens around them were flooded. The largest of the fen-islands is the Isle of Ely, on which the cathedral city of Ely was built: its highest point is 39 m above mean sea level.[7]

Without artificial drainage and flood protection, the Fens would be liable to periodic flooding, particularly in winter due to the heavy load of water flowing down from the uplands and overflowing the rivers. Some areas of the Fens were once permanently flooded, creating small lakes or meres, while others were flooded only during periods of high water. In the pre-modern period, arable farming was limited to the higher areas of the surrounding uplands, the fen islands, and the so-called "Townlands", an arch of silt ground around the Wash, where the towns had their arable fields. Though these lands were lower than the peat fens before the peat shrinkage began, the more stable silt soils were reclaimed by medieval farmers and embanked against any floods coming down from the peat areas or from the sea. The rest of the Fenland was dedicated to pastoral farming, fishing, fowling, and the harvesting of reeds or sedge for thatch. In this way, the medieval and early modern Fens stood in contrast to the rest of southern England, which was primarily an arable agricultural region.

Since the advent of modern drainage in the 19th and 20th centuries, the Fens have been radically transformed. Today arable farming has almost entirely replaced pastoral. The economy of the Fens is heavily invested in the production of crops such as grains, vegetables, and some cash crops such as rapeseed and canola.

Drainage in the Fenland consists of both river drainage and internal drainage of the land between the rivers. The internal drainage was organised by levels or districts, each of which includes the fen parts of one or several parishes. The details of the organisation vary with the history of their development, but the areas include:

  • The Great Level of the Fens is the largest region of fen in eastern England: including the lower drainage basins of the River Nene and the Great Ouse, it covers about 500 sq mi (1,300 km2). It is also known as the Bedford Level, after Francis Russell, 4th Earl of Bedford, who headed the so-called adventurers (investors) in the 17th-century drainage in this area; his son became the first governor of the Bedford Level Corporation. In the 17th century, the Great Level was divided into the North, Middle and South Levels for the purposes of administration and maintenance. In the 20th century, these levels have been given new boundaries; they include some fens that were never part of the jurisdiction of the Bedford Level Corporation.
    • The South Level lies to the southeast of the Ouse Washes and surrounds Ely, as it did in the 17th century.
    • The Middle Level lies between the Ouse Washes and the Nene, but historically was defined as between the Ouse Washes and Morton's Leam, a 15th-century canal that runs north of the town of Whittlesey.
    • The North Level now includes all of the fens in Cambridgeshire and Lincolnshire between the Nene and the River Welland. It originally included only a small part of these lands, including the ancient parishes of Thorney and Crowland, but excluding most of Wisbech Hundred and Lincolnshire, which were under their own local jurisdictions.[8]
  • Deeping Fen, in the southern part of Lincolnshire, lies between the River Welland and the River Glen with its tributary the Bourne Eau.
  • The Black Sluice District, much of which was known as the Lindsey Level when it was first drained in 1639, extends from the Glen and Bourne Eau to Swineshead. Its water is carried through to the Haven at Boston.

The above were all redrained at one time or another after the Civil War (1642-1649).

These were drained in the 18th and 19th centuries.[9]

Formation and geography

At the end of the most recent glacial period, known in Britain as the Devensian, ten thousand years ago, Britain and continental Europe were joined by the ridge between Friesland and Norfolk. The topography of the bed of the North Sea indicates that the rivers of the southern part of eastern England flowed into the Rhine, hence through the English Channel. From the Fens northward along the modern coast, the drainage flowed into the northern North Sea basin. As the ice melted, the rising sea level drowned the lower lands, leading ultimately to the present coastline.[10]

These rising sea levels flooded the previously inland woodland of the Fenland basin; over the next few thousand years both saltwater and freshwater wetlands developed as a result. Silt and clay soils were deposited by marine floods in the saltwater areas and along the beds of tidal rivers, while organic soils, or peats, developed in the freshwater marshes. Fenland water levels peaked in the Iron Age; earlier Bronze and Neolithic settlements were covered by peat deposits, and have only recently been found after periods of extensive droughts revealed them.[10] During the Roman period, water levels fell once again. Settlements developed on the new silt soils deposited near the coast. Though water levels rose once again in the early medieval period, by this time artificial banks protected the coastal settlements and the interior from further deposits of marine silts. Peats continued to develop in the freshwater wetlands of the interior fens.[10]

The wetlands of the fens have historically included:

  • Washes: these are places such as tidal mud flats and braided rivers, which are sometimes exposed and at other times covered with water.
  • Salt marsh: this is the higher part of a tidal wash, on which salt-adapted plants grew.
  • Fen: this is a broad expanse of nutrient-rich shallow water in which dead plants do not fully decay, resulting in a flora of emergent plants growing in saturated peat.
  • Moor: this developed where the peat grew above the reach of the land water which carried the nutrients to the fen. Its development was enabled where the fen was watered directly by rainfall. The slightly acidic rain washed the hydroxide ions out of the peat, making it more suitable for acid-loving plants, notably Sphagnum species. This is the same as bog, but the word moor was applied to this acid peatland occurring on hills. These moors disappeared in the 19th century. Researchers did not think that the Fenland had this kind of peat, until the discovery of archaeological and documentary evidence showing that it did until the early 19th century.
  • Waters: these have included:
    • tidal creeks, which reached from the sea into the marsh, the Townlands and in some places, the fen. They were named only if big enough to be regarded as havens
    • meres, or shallow lakes, which were more or less static but aerated by wind action
    • many rivers, both natural and (from Roman times on) artificial

Major areas for settlement were:

  • Townlands, a broad bank of silt (the remains of the huge creek levees that developed naturally during the Bronze and Iron Ages), on which the settlers built homes and grew vegetables for households
  • fen islands: areas of higher land, which were never covered by the growing peat
  • fen edges: uplands surrounding the fens

In general, of the three principal soil types found in the Fenland today, the mineral-based silt resulted from the energetic marine environment of the creeks, the clay was deposited in tidal mud-flats and salt-marsh, while the peat grew in the fen and bog. The peat produces black soils, which are directly comparable to the American muck soils. A roddon, the dried raised bed of a watercourse, is more suitable for building than the less stable peat.

Since the 19th century, all of the acid peat in the Fens has disappeared. Drying and wastage of peats has greatly reduced the depth of the alkaline peat soils and reduced the overall elevation of large areas of the peat fens.

History

John Sell Cotman - Drainage Mills in the Fens, Croyland, Lincolnshire - Google Art Project
Drainage Mills in the Fens, Croyland, Lincolnshire. John Sell Cotman

Pre-Roman settlement

There is evidence of human settlement near the Fens from the Mesolithic on. The evidence suggests that Mesolithic settlement in Cambridgeshire was particularly along the fen edges and on the low islands within the fens, to take advantage of the hunting and fishing opportunities of the wetlands.[11]

Roman farming and engineering

The Romans constructed the Fen Causeway, a road across the Fens to link what later became East Anglia with what later became central England; it runs between Denver and Peterborough. They also linked Cambridge and Ely. Generally, their road system avoided the Fens, except for minor roads designed for exporting the products of the region, especially salt, beef and leather. Sheep were probably raised on the higher ground of the Townlands and fen islands, then as in the early 19th century. There may have been some drainage efforts during the Roman period, including the Car Dyke along the western edge of the Fenland between Peterborough and Lincolnshire, but most canals were constructed for transportation.[12]

How far seaward the Roman settlement extended is unclear owing to the deposits laid down above them during later floods.

Early post-Roman settlements

The early post-Roman settlements were made on the Townlands. It is clear that there was some prosperity there, particularly where rivers permitted access to the upland beyond the fen. Such places were Wisbech, Spalding, Swineshead and Boston. All the Townlands parishes were laid out as elongated strips, to provide access to the products of fen, marsh and sea. On the fen edge, parishes are similarly elongated to provide access to both upland and fen. The townships are therefore often nearer to each other than they are to the distant farms in their own parishes.

Early Middle Ages and Middle Ages

After the end of Roman Britain, there is a break in written records. It is thought that some Iceni may have moved west into the Fens to avoid the Angles, who were migrating across the North Sea from Angeln (modern Schleswig) and settling what would become East Anglia. Surrounded by water and marshes, the Fens provided a safe area that was easily defended and not particularly desirable to invading Anglo-Saxons.

The names of West Walton, Walsoken and Walpole are believed to suggest the native British population, as the Wal- coming from the Old English walh, meaning "foreigner".[13] However, the villages are in close proximity to the old Roman sea wall, so the wal- element is more probably from wal or weal, meaning "wall". Walton is generally believed to mean "wall-town",[14] Walsoken to mean "the district under particular jurisdiction by the wall",[14] and Walpole to mean simply "wall-pole" (Old English wal and pal)[15] or perhaps "well pool" (Old English welle and pol).[16]

When written records resume in Anglo-Saxon England, the names of a number of peoples of the Fens are recorded in the Tribal Hidage and Christian histories. They include North Gyrwe (Peterborough and Crowland), South Gyrwe (Ely), the Spalda (Spalding), and Bilmingas (part of south Lincolnshire).

In the early Christian period of Anglo-Saxon England, a number of Christians sought the isolation that could be found in the wilderness of the Fens. Later classified as saints, often with close royal links, they include Guthlac, Etheldreda, Pega, and Wendreda. Hermitages on the islands became centres of communities which later developed as monasteries with massive estates. In the Life of Saint Guthlac, a biography of the East Anglian hermit who lived in the Fens during the early 8th century, Saint Guthlac was described as attacked on several occasions by people he believed were Britons, who were then living in the Fens. However, Bertram Colgrave, in the introduction to one edition, doubts this account, because of the lack of evidence of British survival in the region. British place names in the area are "very few".[17]

Monastic life was disrupted by Danish (Anglo-Saxon) raids and centuries of settlement from the 6th century but was revived in the mid-10th-century monastic revival. In the 11th century, the whole area was incorporated into a united Anglo-Saxon England. The Fens remained a place of refuge and intrigue. It was here that Alfred Aetheling was brought to be murdered and here where Hereward the Wake based his insurgency against Norman England.

Fenland monastic houses include the so-called Fen Five (Ely Cathedral Priory, Thorney Abbey, Croyland Abbey, Ramsey Abbey and Peterborough Abbey)[18] as well as Spalding Priory. As major landowners, the monasteries played a significant part in the early efforts at drainage of the Fens.

Royal Forest

During most of the 12th century and the early 13th century, the south Lincolnshire fens were afforested. The area was enclosed by a line from Spalding, along the River Welland to Market Deeping, then along the Car Dyke to Dowsby and across the fens to the Welland. It was deforested in the early 13th century. There is little agreement as to the exact dates of the establishment and demise of the forest, but it seems likely that the deforestation was connected with the Magna Carta or one of its early 13th-century restatements, though it may have been as late as 1240. The forest would have affected the economies of the townships around it and it appears that the present Bourne Eau was constructed at the time of the deforestation, as the town seems to have joined in the general prosperity by about 1280.

Though the forest was about half in Holland (Lincolnshire) and half in Kesteven, it is known as Kesteven Forest.[19]

Draining the Fens

Fens area of Lincolnshire (Janssonius)
Southern Lincolnshire from a mid-17th-century atlas, showing unsettled areas within undrained fens

Early modern attempts to drain the Fens

Though some signs of Roman hydraulics survive, and there were also some medieval drainage works, land drainage was begun in earnest during the 1630s by the various investors who had contracts with King Charles I to do so. The leader of one of these syndicates was the Earl of Bedford, who employed Cornelius Vermuyden as engineer. Contrary to popular belief, Vermuyden was not involved with the draining of the Great Fen in Cambridgeshire and Norfolk in the 1630s, but only became involved with the second phase of construction in the 1650s.[20] The scheme was imposed despite huge opposition from locals who were losing their livelihoods based on fishing and wildfowling. Fenmen known as the Fen Tigers tried to sabotage the drainage efforts.

Two cuts were made in the Cambridgeshire Fens to join the River Great Ouse to the sea at King's Lynn – the Old Bedford River and the New Bedford River, the latter being known also as the Hundred Foot Drain. Both cuts were named after the Fourth Earl of Bedford who, along with some gentlemen adventurers (venture capitalists), funded the construction and were rewarded with large grants of the resulting farmland. The work was directed by engineers from the Low Countries. Following this initial drainage, the Fens were still extremely susceptible to flooding, so windpumps were used to pump water away from affected areas. The Company of Adventurers were more formally incorporated in 1663 as the Bedford Level Corporation.

However, their success was short-lived. Once drained of water, the peat shrank, and the fields lowered further. The more effectively they were drained, the worse the problem became, and soon the fields were lower than the surrounding rivers. By the end of the 17th century, the land was under water once again.

Though the three Bedford Levels together formed the biggest scheme, they were not the only ones. Lord Lindsey and his partner Sir William Killigrew had the Lindsey Level inhabited by farmers by 1638, but the onset of the Civil War permitted the destruction of the works until the 1765 Act of Parliament that led to the formation of the Black Sluice Commissioners.[21]

Stretham Old Engine
Stretham Old Engine,
alongside the River Great Ouse

Many original records of the Bedford Level Corporation, including maps of the Levels, are now held by Cambridgeshire Archives and Local Studies Service at the County Record Office in Cambridge.

Modern drainage

The major part of the draining of the Fens was effected in the late 18th and early 19th century, again involving fierce local rioting and sabotage of the works. The final success came in the 1820s when windpumps were replaced with powerful coal-powered steam engines, such as Stretham Old Engine, which were themselves replaced with diesel-powered pumps, such as those at Prickwillow Museum and, following World War II, the small electric stations that are still used today.

Prickwillow Drainage Engine Museum
Prickwillow Museum, the changing face of the Fens and the story of drainage

The dead vegetation of the peat remained undecayed because it was deprived of air (the peat being anaerobic). When it was drained, the oxygen of the air reached it, since then the peat has been slowly oxidizing. This, together with the shrinkage on its initial drying and the removal of soil by the wind, has meant that much of the Fens lies below high tide level. As the highest parts of the drained fen are now only a few metres above mean sea level, only sizeable embankments of the rivers, and general flood defences, stop the land from being inundated. Nonetheless, these works are now much more effective than they were.

The Fens today are protected by 60 miles (97 km) of embankments defending against the sea and 96 miles (154 km) of river embankments. Eleven internal drainage board (IDB) groups maintain 286 pumping stations and 3,800 miles (6,100 km) of watercourses, with the combined capacity to pump 16,500 Olympic-size swimming pools in a 24-hour period or to empty Rutland Water in 3 days.[22]

Modern farming and food manufacturing in the Fens

As of 2008, there are estimated to be 4,000 farms in the Fens involved in agriculture and horticulture, including arable, livestock, poultry, dairy, orchards, vegetables and ornamental plants and flowers. They employ about 27,000 people in full-time and seasonal jobs. In turn, they support around 250 businesses involved in food and drink manufacturing and distribution, employing around 17,500 people.[22]

Over 70% of the Fens is involved in environmental stewardship schemes, under which 270 miles (430 km) of hedgerow and 1,780 miles (2,860 km) of ditches are managed, providing large wildlife corridors and habitat for endangered animals such as the water vole.[22]

Restoration

In 2003, the Great Fen Project was initiated to return parts of the Fens to their original pre-agricultural state. The periodic flooding by the North Sea, which renewed the character of the Fenlands, was characterised conventionally by the 1911 Encyclopædia Britannica as "ravaged by serious inundations of the sea". The modern approach is to allow a little farmland to be flooded again and turned into nature reserves. By introducing fresh water, the organisers of the project hope to encourage species such as the snipe, lapwing and bittern. Endangered species such as the fen violet will be seeded.

The Fens Waterways Link is a scheme to restore navigation to some of the drainage works. It is planned to bring the South Forty-Foot Drain and parts of the Car Dyke into use as part of a route between Boston and Cambridge.

Sport

The Fens is the origin of English bandy and speed skating. It is the base of Great Britain Bandy Federation[23] and in Littleport there is a project in place aiming at building an indoor stadium for ice sports. If successful it will have the largest sheet of ice in the country with both a bandy pitch and a speed skating oval.[24]

Settlements

Many historic cities, towns and villages have grown up in the fens, sited chiefly on the few areas of raised ground. These include:

Ancient sites include:

In popular culture

Some authors have featured the Fens repeatedly in their work. For example:

  • John Gordon, adolescent fiction writer and author of The Giant Under The Snow, drew inspiration for many of his supernatural fantasies from the Fens. His books with Fenland themes include: Ride The Wind, Fen Runners and The House On The Brink, which was based on Peckover House in Wisbech.
  • Peter F. Hamilton sets a number of his science fiction novels in the Fens, including Mindstar Rising and A Quantum Murder.
  • M. R. James set several of his ghost stories in the fen country.
  • Jim Kelly set The Water Clock, The Moon Tunnel and The Funeral Owl in the Fens.
  • Philippa Pearce, a children's author, set many of her books in the Fens, for example Tom's Midnight Garden.
  • Gladys Mitchell, prolific writer of detective fiction, took her eccentric sleuth, the psychiatrist Mrs Lestrange Bradley, to the Fens in several books, notably The Worsted Viper, Wraiths and Changelings and The Mudflats of the Dead.
  • Robert Louis Stevenson's The Black Arrow has several chapters set in the Fens.
  • Nick Warburton wrote a series of radio plays entitled On Mardle Fen, one of the longest-running series of plays on BBC R4.[26]
  • Susanna Gregory's Matthew Bartholomew chronicles' title character is a fictional physician living in 14th-century Cambridge.
  • G. A. Henty's book Beric the Briton mentions some sections in the Fens.
  • Norah Lofts features a character called Ethelreda Benedict, who comes from a small island in the Fens in the 17th century, in the second book of her "House" trilogy, The House at Old Vine.
  • Louis L'Amour's "To The Far Blue Mountains", the central character Barnabas Sackett from "Sackett's Land" returns to his home in the Fens one last time in the opening chapter.

The following novels, or substantial portions of them, are set in the Fens:

Some films have large portions set in the Fenlands:

The 1974 Look and Read series Cloud Burst was set and filmed in the Fens. The episode Three Miles Up of the 1995 BBC series Ghosts was set in the Fens.

At least one video game has been set in the Fens:

  • The Lost Crown: A Ghost-Hunting Adventure is set in a fictional town called Saxton, located in the Fens.

The 2019 TV show Wild Bill was set in Boston, Lincolnshire.

See also

References

  1. ^ After Lindley, Keith (1982). Fenland riots and the English revolution. Heinemann Educational Books. ISBN 978-0-435-32535-0.
  2. ^ It is debated whether this area includes the fen areas of north Lincolnshire, such as the Isle of Axholme. Some scholars, such as Keith Lindley, include the Isle of Axholme as part of the Fenland, as it has the same kind of environment and a similar environmental and social history. But it is not contiguous with the rest of the East Anglian Fenland, nor was its drainage ever jointly organised with that of any of the main Fenland drainage areas. It is generally designated as a separate area.
  3. ^ Wise, John; Noble, W. Mackreth (1882). Ramsey Abbey: Its Rise and Fall. Huntingdon: Ellis & Cooper. ISBN 0-904701-10-7.
  4. ^ Christian, Anne Hait (1984). The Search for Holmes, Robson, Hind, Steele and Graham Families of Cumberland and Northumberland, England. La Jolla, CA: Search. p. 7. ISBN 0-9613723-0-3.
  5. ^ H. C. A discourse concerning the drayning of fennes and surrounded grounds in the sixe counteys of Norfolk, Suffolke, Cambridge, with the Isle of Ely, Huntington, Northampton and Lincolne. London: 1629. Reprinted in 1647 under title: The Drayner Confirmed, and the Obstinate Fenman Confuted.
  6. ^ "UK's lowest spot is getting lower". BBC. 29 November 2002. Retrieved 26 March 2010.
  7. ^ Isle of Ely, Wheres The Path website
  8. ^ "An Act for settling the Draining of the Great Level of the Fens called Bedford Level", 1663, reproduced in Samuel Wells, The History of the Drainage of the Great Level of the Fens called Bedford Level, (London, 1830), Vol.2, pp.383ff.
  9. ^ Bedford Levels information from Ordnance Survey 1:50 000 First Series Sheets 142 (1974) and 143 (1974). Lincolnshire information from Wheeler, W.H. A History of the Fens of South Lincolnshire 2nd edn. (1896) facsimile edn. Paul Watkins (1990) ISBN 1-871615-19-4
  10. ^ a b c David Hall and John Coles, "Fenland Survey. An essay in landscape and persistence", Archeological Report 1. English Heritage, 1994.
  11. ^ Christopher Taylor. The Cambridgeshire Landscape. Hodder and Stroughton, London, 1973. p30.
  12. ^ Hall, David; Coles, John (1994). Fenland survey: an essay in landscape and persistence. English Heritage. ISBN 978-1-85074-477-1.
  13. ^ Simon Young, AD500 p.245 (Notes & Sources) references Life of Saint Guthlac (Cambridge University Press 1956), pp. 108–11.
  14. ^ a b A Popular Guide to Norfolk Place-names, by James Rye: Dereham, Norfolk: Larks Press, 2000 ; ISBN 0-948400-15-3
  15. ^ Geographical Etymology, (1887), Christina Blackie, J. Murray, London, accessed 21 May 2010
  16. ^ House of Names – Walpole Family Crest and Name History, accessed 21 May 2010
  17. ^ Bertram Colgrave (ed). Felix's Life of Saint Guthlac, (c730). Cambridge University Press, ISBN 978-0-521-31386-5
  18. ^ "ULAS – Thorney". University of Leicester Archaeological Services. 26 February 2007. Retrieved 17 March 2011.
  19. ^ "New Page 1". info.sjc.ox.ac.uk. Retrieved 19 March 2018.
  20. ^ Margaret Albright Knittl, "The design for the initial drainage of the Great Level of the Fens: an historical whodunit in three parts", Agricultural History Review, 55:1 (2007), pp. 23–50. Abstract
  21. ^ "Historyof the Black Sluice Internal Drainage Board". Archived from the original on 28 April 2011.
  22. ^ a b c "Why Farming Matters in the Fens (2)". NFU East Anglia. 2008. Archived from the original (PDF) on 27 April 2011. Retrieved 17 March 2011.
  23. ^ "Members - Federation of International Bandy". www.worldbandy.com. Retrieved 19 March 2018.
  24. ^ "theicestadiumproject". theicestadiumproject. Retrieved 19 March 2018.
  25. ^ Welcome to Wisbech – Capital of the Fens Archived 30 April 2008 at the Wayback Machine
  26. ^ radiolistings.co.uk On Mardle Fen
  27. ^ "honour thy father". Lesley Glaister. Retrieved 19 March 2018.
  28. ^ Thorpe, Adam (2 April 2014). "The Wake by Paul Kingsnorth review 'A literary triumph'". The Guardian. Retrieved 15 September 2015.
  29. ^ Ubisoft (2008). "Locations". Ubisoft. Retrieved 1 April 2011.

Further reading

External links

Coordinates: 52°29′18″N 0°13′52″W / 52.48838°N 0.23118°W

Car Dyke

The Car Dyke was, and to a large extent still is, an 85 miles (137 km)-long ditch which runs along the western edge of the Fens in eastern England. It is generally accepted as being of Roman age and, for many centuries, to have been taken as marking the western edge of the Fens. There, the consensus begins to break down.

Cornelius Vermuyden

Sir Cornelius Vermuyden (Sint-Maartensdijk, 1595 – London, 11 October 1677) was a Dutch engineer who introduced Dutch land reclamation methods to England. Commissioned by the Crown to drain Hatfield Chase in the Isle of Axholme, Lincolnshire, Vermuyden was knighted in 1629 for his work and became an English citizen in 1633. In the 1650s, he directed major projects to drain The Fens of East Anglia, introducing the innovation of constructing washes, to allow periodic flooding of the area by excess waters.

Ditch

A ditch is a small to moderate depression created to channel water. A ditch can be used for drainage, to drain water from low-lying areas, alongside roadways or fields, or to channel water from a more distant source for plant irrigation. Ditches are commonly seen around farmland, especially in areas that have required drainage, such as The Fens in eastern England and much of the Netherlands.

Roadside ditches may provide a hazard to motorists and cyclists, whose vehicles may crash into them and get damaged, flipped over or stuck, especially in poor weather conditions, and in rural areas.

Downham Market

Downham Market, sometimes simply referred to as Downham, is a market town and civil parish in Norfolk, England. It lies on the edge of the Fens, on the River Great Ouse, approximately 11 miles south of King's Lynn, 39 miles west of Norwich and 30 miles north of Cambridge.The civil parish has an area of 5.2 km² and in the 2011 census had a population of 9,994 in 4,637 households. For the purposes of local government, the parish falls within the district of King's Lynn and West Norfolk. It is part of South West Norfolk parliamentary constituency.

It was an agricultural centre, developing as a market for the produce of the Fens with a bridge across the Ouse. During the Middle Ages, it was famed for its butter market and also hosted a notable horse fair.

The market is now held Fridays and Saturdays on the town hall car park.

Notable buildings in the town include its mediaeval parish church, dedicated to St Edmund, and Victorian clock tower, constructed in 1878. The town is also known as the place where Charles I hid after the Battle of Naseby. In 2004 the town completed a regeneration project on the Market Place, moving the market to the town hall car park. The decorative town sign depicts the crown and arrows of St Edmund with horses to show the importance of the horse fairs in the town's history.

A heritage centre, Discover Downham, opened in a former fire station in 2016.

Fenland District

Fenland is a local government district in Cambridgeshire, England. Its council is based in March, and it covers the neighbouring market towns of Chatteris, Whittlesey

and Wisbech; the last is often called the "capital of the fens".The district covers around 500 square kilometres (210.99 square miles) of mostly agricultural land in the extremely flat Fens. The population of the district was 98,262 at the 2011 Census.It was formed on 1 April 1974, with the merger of the Borough of Wisbech, Chatteris Urban District, March Urban District, Whittlesey Urban District, North Witchford Rural District and Wisbech Rural District.

Hilgay Heronry

Hilgay Heronry is a 1.8-hectare (4.4-acre) biological Site of Special Scientific Interest south of Downham Market in Norfolk.This small wood has a nationally important breeding colony of grey herons, with around forty nests each year in larch and ash trees. Nearby drainage dykes on The Fens provide feeding grounds.The site is private land with no public access.

Iceni

The Iceni or Eceni were a Brittonic tribe of eastern Britain during the Iron Age and early Roman era. Their territory included present-day Norfolk and parts of Suffolk and Cambridgeshire, and bordered the area of the Corieltauvi to the west, and the Catuvellauni and Trinovantes to the south. In the Roman period, their capital was Venta Icenorum at modern-day Caistor St Edmund.Julius Caesar does not mention the Iceni in his account of his invasions of Britain in 55 and 54 BC, though they may be related to the Cenimagni, who Caesar notes as living north of the River Thames at that time. The Iceni were a significant power in eastern Britain during Claudius' conquest of Britain in AD 43, in which they allied with Rome. Increasing Roman influence on their affairs led to revolt in AD 47, though they remained nominally independent under king Prasutagus until his death around AD 60. Roman encroachment after Prasutagus' death led his wife Boudica to launch a major revolt from 60–61. Boudica's uprising seriously endangered Roman rule in Britain and resulted in the burning of Londinium and other cities. The Romans finally crushed the rebellion, and the Iceni were increasingly incorporated into the Roman province.

Isleham

Isleham is a small village and civil parish in the English county of Cambridgeshire. It is part of the Fens.

Leziate, Sugar and Derby Fens

Leziate, Sugar and Derby Fens is an 87.9-hectare (217-acre) biological Site of Special Scientific Interest east of King's Lynn in Norfolk.These fens have extensive heaths and areas of wet acidic grassland, and there are smaller areas of damp woodland and species-rich calcareous grassland. There are many ant-hills on Derby Fen.There is public access to the fens, which are in three separate areas.

Lode, Cambridgeshire

Lode is a small village in East Cambridgeshire on the southern edge of The Fens. It lies just north of the B1102 between Quy and Swaffham Bulbeck, 8 miles (13 km) to the north east of Cambridge. It has the highest number of startups per capita of any area in the United Kingdom.

The village's name is derived from its location at the southern end of Bottisham Lode that links it to the River Cam. A lode is an artificial water channel used to drain the Fens, thought to be of Roman origin.

Lode also has the smaller hamlet settlement of Long Meadow as part of the parish to the east along the B1102.

Lode is a comparatively new civil parish, having been separated from Bottisham in 1894.

Methwold

Methwold ("Middle forest") is a civil parish in the English county of Norfolk, on the edge of the Norfolk Fens and Breckland.

With an area of 49.12 km2 (18.97 sq mi) it is the second largest parish in Norfolk. It had a population of 1,476 in 591 households at the 2001 census, increasing to 1,502 at the 2011 Census. For the purposes of local government, it falls within the district of King's Lynn and West Norfolk.

The parish also includes the hamlets of Methwold Hythe, approximately 1 mile (1.6 km) east of the town and on the edge of the fens, and Brookville to the north west.Its economy is based on agriculture with a little light industry. The village is situated about 20 miles (32 km) from King's Lynn and 15 miles (24 km) north west of Thetford (its postal town).

The Duchy of Lancaster Methwold CofE Primary School is located in the parish. The secondary and sixth form departments of Iceni Academy are also located in Methwold, previously being known as Methwold High School.

Methwold parish is the second largest parish in Norfolk in terms of land. The parish currently has approximately 20 farms ranging from about 60 acres (243,000 m2) up to 1,000 acres (4.0 km2). Farming in Methwold and the surrounding areas accounts for a vast majority of jobs in the fens. Even if people don't farm, much of the work is connected with the land.

Methwold became famous for its abundance and excellence of its rabbits which were sold by poulterers as "Muel Rabbits". According to John Marius Wilson, Methwold was formerly a market town given its market charter granted by King James I in 1718 during a brief visit. A meal of Muel Rabbits was reputed to have pleased the king to such an extent that he granted the village a charter for the market to be held.

The village was struck by an F1/T2 tornado on 23 November 1981, as part of the record-breaking nationwide tornado outbreak on that day.

Old Bedford River

The Old Bedford River is an artificial, partial diversion of the waters of the River Great Ouse in the Fens of Cambridgeshire, England. It was named after the fourth Earl of Bedford who contracted with the local Commission of Sewers to drain the Great Level of the Fens beginning in 1630.

The idea of an artificial river running, as the Old Bedford River does, from Earith to Denver was not a new idea; it had been proposed as early as 1604 by the engineer John Hunt. The work on the Old Bedford River was financed by the Earl of Bedford and several other investors and was undertaken between 1630 and 1636, but the supervising engineer is not known.Artificial drainage of low-lying wetlands generally involves one or both of two different practices: excluding water flowing from high areas from entering the low-lying area, and pumping out water which does manage to get into the low-lying area. The Old Bedford River was constructed on the first principle, as were most of the drainage works constructed in the seventeenth century in the English fens. Both the Old Bedford River and the New Bedford River (constructed 20 years later in 1650) were intended to reduce or eliminate flooding of the fens of the Great Level by carrying the bulk of the water from the Great Ouse River from the uplands of Huntingdonshire to the sea in a straight channel, rather than allowing it to meander (and flood) the fens of the Great Level.

The flow in the Great Ouse is maintained for navigation, fisheries and aesthetic reasons but when there is excessive flow, the excess is diverted along the Bedford Rivers of which there are two, the Old and the New. Between them lies the Ouse Washes. This is not to be confused with the estuarine feature of The Wash towards which all this water is flowing. The Ouse Washes is an area in which excess fresh river water is stored until low tide permits its release or until flood levels elsewhere allow. The two rivers have raised banks (which in some parts of the world, would be called levees), so as to keep the flow within them but the outer bank in each case is higher so that when the flow becomes too great, the rivers fill the wash between them but not the farmland of the Middle and South Bedford Levels outside the banks.

To facilitate the drainage of the washland, there is a third, unembanked river between the two Bedford Rivers, alongside the Old Bedford River and known as the River Delph. It drains into the New Bedford River 2 to 3 kilometres (1.2 to 1.9 miles) south of Denver Sluice.

The names of the three waterways are rather inconsistent. At Welches Dam (where the 1651 Forty Foot drain enters from the West) the Old Bedford river moves to the East and the Forty Foot actually enters the Counter Drain. It is the latter waterway which exits into the River Great Ouse just below Salters Lode. The actual Old Bedford River swaps identities in the Welches Dam area and becomes the River Delph. This dates back to when Forty Foot drain (also called Vermuyden's Drain) was cut. The latter sometimes caused water to flow back up the Old Bedford river to Earith. To alleviate this a dam was built by Edmund Welche across the Old Bedford river just upstream of the junction of the two waterways. Unfortunately this caused the wash area between the Old and New Bedford rivers to flood so a new waterway was cut to link the stub of the Old Bedford River (from the point of the ex-dam) straight into the New Bedford river further upstream at Welmore Lake sluice. This new waterway (which kinks to the right at Welches Dam before continuing parallel with the Old Bedford River) was named the River Delph and a flood bank was also built between it and the Old Bedford river to maintain the integrity of the Wash area.

Potter and Scarning Fens, East Dereham

Potter and Scarning Fens, East Dereham is a 6.2-hectare (15-acre) biological Site of Special Scientific Interest south of Dereham in Norfolk. It is part of the Norfolk Valley Fens Special Area of Conservation. Scarning Fen is a Nature Conservation Review site, Grade I, and it is managed by the Norfolk Wildlife Trust.These are valleys with calcareous fens on peat with an exceptionally diverse flora, including uncommon mosses and liverworts. Insects include the nationally rare small red damselfly.The fens are open to the public.

Shippea Hill SSSI

Shippea Hill SSSI is a 27.6 hectare geological Site of Special Scientific Interest east of Ely in Cambridgeshire. It is a Geological Conservation Review site.The succession of sedimentary layers in the Fens in the Holocene epoch, the period since the last ice age, was determined in the 1930s on the basis of Shippea Hill deposits, although this has been amended as the site has been found to be atypical. It is particularly important for dating the "Fen Clay transgression" of the sea into the Fens in the Holocene.In the early 1930s the pioneer of British Mesolithic archaeology, Grahame Clark collaborated with the botanists Harry and Margaret Godwin to gain a deeper understanding of the environment of past societies by integrating archaeological findings with new scientific techniques in geology and plant sciences. They formed the Fenland Research Committee to study the effect of post-glacial environmental changes on Fenland Mesolithic communities, and their first major collaboration was excavation of Shippea Hill.The site is on private land with no public access. It has been filled in and is now a field.

Spalding, Lincolnshire

Spalding is a market town with a population of 28,722 at the 2011 census, on the River Welland in the South Holland district of Lincolnshire, England. Little London is a hamlet directly south of Spalding on the B1172, whilst Pinchbeck, a village to the north, is part of the built-up area.

The town was well known for the annual Spalding Flower Parade, held from 1959 to 2013. The parade celebrated the region's vast tulip production and the cultural links between the Fens and the landscape and people of South Holland. At one time, it attracted crowds of more than 100,000. Since 2002 the town has held an annual Pumpkin Festival in October.

Stagecoach in The Fens

Stagecoach in Huntingdonshire is the trading name of Stagecoach in The Fens Limited, which runs services throughout Huntingdon, the Fens and surrounding areas. It is part of Stagecoach East, itself a subsidiary of the larger Stagecoach Group Plc.

The Fens (Boston, Massachusetts)

The Back Bay Fens, often called The Fens, is a parkland and urban wild in Boston, Massachusetts, in the United States. It was established in 1879. Designed by Frederick Law Olmsted to serve as a link in the Emerald Necklace park system, the Fens gives its name to the Fenway-Kenmore neighborhood, and thereby to Fenway Park, home of the Boston Red Sox.

Welney

Welney is a village and civil parish in the Fens of England, and the county of Norfolk. The village is about 10 miles (16 km) south-west of the town of Downham Market, 20 miles (30 km) south of the town of King's Lynn and 45 miles (70 km) west of the city of Norwich. The county boundary with Cambridgeshire is adjacent, with the city of Cambridge 25 miles (40 km) to the south.Welney is immediately to the west of the Old Bedford River, River Delph and New Bedford River, which are all parallel channels and are here crossed by the A1101 road.

Welney is on the Ouse Washes, an area of wildlife conservation. WWT Welney, near the village, is a nature reserve in the care of the Wildfowl and Wetlands Trust. Nearby, there are also the RSPB Ouse Washes, a reserve managed by the Royal Society for the Protection of Birds.

The parish covers an area of 8 square miles (20 km2) and had a population of 528 in 217 households at the 2001 census; the population increased to 542 at the 2011 Census. For the purposes of local government, the parish falls within the district of King's Lynn and West Norfolk.In the 14th century, Welney was called Wellenhe, meaning "a river called Welle" (the old name of the Old Croft River). In the second half of the 19th century Welney became significant for its skaters. On 21 February 1855, Turkey Smart of Welney became champion skater of the Fens. James Smart of Welney became champion on 21 January 1891. William Loveday of Welney came 2nd to James Aveling of March in the amateur championship.St Mary's Church in Welney is dedicated to the Virgin Mary.

Wynne Godley

Wynne Godley (2 September 1926 – 13 May 2010) was an economist famous for his pessimism toward the British economy and his criticism of the British government.

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