Adventurers (land Drainage)
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Adventurers (land Drainage)
Adventurers were groups of English engineers and wealthy landowners, who funded large scale land drainage projects in the seventeenth century, in return for rights to some of the land reclaimed. Early entrepreneurs Land drainage works were expensive, and were usually undertaken in sparsely populated areas. In the seventeenth century a number of such schemes were carried out by Adventurers, who acted under parliamentary sanction, but who financed the works carried out themselves. In return, they gained rights to the land reclaimed as a result of the civil engineering works. One such scheme was the draining of the Bedford Levels. The Bedford Level Corporation was in charge of the works, which when conceived in 1630, would create large tracts of "summer lands", which would be suitable for grazing during the summer months, but would still be liable to flooding in the winter. Funds for the work were provided by the Earl of Bedford and thirteen other Adventurers. Of the land reclaimed, th ...
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Bedford Level Corporation
The Bedford Level Corporation (or alternatively the Corporation of the Bedford Level) was founded in England in 1663 to manage the draining of the Fens of East Central England. It formalised the legal status of the Company of Adventurers previously formed by the Duke of Bedford to reclaim 95,000 acres of the Bedford Level. History The low-lying land of East Central England, known as the Fens, consisted traditionally of semi-continuous marshland and peat bog interspersed with isolated patches of higher ground. Agriculture has only been made possible by a co-ordinated system of drainage ditches. During medieval times this was controlled by the great monasteries in the area but fell into disrepute after the dissolution of the monasteries. By the 1600s the general drainage situation was so bad that King Charles I invited Cornelius Vermuyden, the Dutch engineer, to devise a scheme to drain the Great Fen. The Bedford Level The Great Fen, lying between the Wash and Cambridge, is more p ...
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Earl Of Lindsay
Earl of Lindsay is a title in the Peerage of Scotland. It was created in 1633 for John Lindsay, 10th Lord Lindsay, who later inherited the ancient Earldom of Crawford. The two earldoms remained united until the death of the 22nd Earl of Crawford, also sixth Earl of Lindsay, in 1808. Then the earldom of Lindsay passed to David Lindsay, while the earldom of Crawford became dormant because no-one could prove a claim to the title until 1848. Both David, 7th Earl of Lindsay, and his successor Patrick, 8th Earl of Lindsay, died without sons, and the disputed claim over the earldom was resolved by the House of Lords in 1878 in favour of Sir John Trotter Bethune, 2nd Baronet. The subsidiary titles of the Earl are: Viscount of Garnock (created 1703), Lord Lindsay of The Byres (1445), Lord Parbroath (1633) and Lord Kilbirnie, Kingsburn and Drumry (1703), all in the Peerage of Scotland. The title Viscount Garnock is used as the courtesy title for the eldest son and heir to the Earl. The ...
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Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ...
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Reclaimed Land
Land reclamation, usually known as reclamation, and also known as land fill (not to be confused with a waste landfill), is the process of creating new Terrestrial ecoregion, land from oceans, list of seas, seas, Stream bed, riverbeds or lake beds. The land reclaimed is known as reclamation ground or land fill. In some jurisdictions, including parts of the United States, the term "reclamation" can refer to returning disturbed lands to an improved state. In Alberta, Canada, for example, reclamation is defined by the provincial government as "The process of reconverting disturbed land to its former or other productive uses." In Oceania, it is frequently referred to as land rehabilitation. History One of the earliest large-scale projects was the Beemster, Beemster Polder in the Netherlands, realized in 1612 adding of land. In Hong Kong the Praya Reclamation Scheme added of land in 1890 during the second phase of construction. It was one of the most ambitious projects ever tak ...
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The Fens
The Fens, also known as the , in eastern England are a naturally marshy region supporting a rich ecology and numerous species. Most of the fens were drained 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 have been built higher to protect it from flooding. 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 and relatively large quantities of dissolved minerals, but few other plant nutrients. The Fens are a National Character Area, based on their landscape, biodiversity, geodiversity and economic activity. The Fens lie inland of the Wash, and are an area of nearly in Lincolnshire, Cambridgeshire, and Norfol ...
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Twenty, Lincolnshire
Twenty is a hamlet in the South Kesteven district of Lincolnshire, England. It is situated approximately east from the market town of Bourne, and west from Spalding. Agriculture is the major industry. Location Twenty is situated on the A151 road, possibly originally a Roman road or Norman causeway, a road today notable for the very deep drainage dyke that runs alongside it. Nearby are Guthram Gowt and West Pinchbeck. Immediately to the south is the River Glen. No separate population statistic is available for Twenty. The best available report lumps together Dyke, Twenty, South Fen and Spalding Road outside Bourne, with a total of 495, with Dyke being the largest. Modern drainage The area falls within the drainage area of the Black Sluice Internal Drainage Board. They maintain a small electric pumping station to the west of the crossroads, called ''Twenty Pumping Station'' See also * List of places with numeric names This is a list of places with numeric names. 0 ...
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Fen Skating
Fen skating is a traditional form of ice skating in the Fenland of England. The Fens of East Anglia, with their easily flooded meadows, form an ideal skating terrain. Bone skates have been found in the area dating back to the medieval period. It is not known when the first skating matches were held, but by the early nineteenth century they had become a feature of cold winters in the Fens. The golden age of fen skating was the second half of the nineteenth century, when thousands of people turned out to watch such legendary skaters as Larman Register, William "Turkey" Smart, (William) "Gutta Percha" See, and brothers George 'Fish' Smart (1858-1909) and James Smart. Members of the Bury Fen Bandy Club published rules of the game in 1882, and introduced it into other countries. The National Skating Association was set up in Cambridge in 1879 and took the top few fen skaters to the Netherlands, where they had a brief moment of international glory with James Smart becoming Britain ...
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Witham Navigable Drains
The Witham Navigable Drains are located in Lincolnshire, England, and are part of a much larger drainage system managed by the Witham Fourth District Internal Drainage Board. The Witham Fourth District comprises the East Fen and West Fen, to the north of Boston, which together cover an area of . In total there are over of drainage ditches, of which under are navigable. Navigation is normally only possible in the summer months, as the drains are maintained at a lower level in winter, and are subject to sudden changes in level as a result of their primary drainage function, which can leave boats stranded. Access to the drains is from the River Witham at Anton's Gowt Lock. The area is bounded by the River Witham to the south and west, and the Steeping River to the north. Since the 11th century, there have been attempts to prevent the fens from flooding, so that they could be used for agriculture. A major advance was made in the seventeenth century, when Adventurers built drains in ...
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First English Civil War
The First English Civil War took place in England and Wales from 1642 to 1646, and forms part of the 1639 to 1653 Wars of the Three Kingdoms. They include the Bishops' Wars, the Irish Confederate Wars, the Second English Civil War, the Anglo-Scottish war (1650–1652) and the 1649 to 1653 Cromwellian conquest of Ireland. Historians estimate that between 15% to 20% of all adult males in England and Wales served in the military between 1639 to 1653, while around 4% of the total population died from war-related causes. This compares to a figure of 2.23% for World War I, which illustrates the impact of the conflict on society in general and the bitterness it engendered. Conflict over the role of Parliament and religious practice dated from the accession of James VI and I in 1603. These tensions culminated in the imposition of Personal Rule in 1629 by his son, Charles I, who finally recalled Parliament in April and November 1640. He did so hoping to obtain funding that would en ...
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Bourne, Lincolnshire
Bourne is a market town and civil parish in the South Kesteven district of Lincolnshire, England. It lies on the eastern slopes of the limestone Kesteven Uplands and the western edge of the Fens, 11 miles (18 km) north-east of Stamford, 12 miles (19 km) west of Spalding and 17 miles (27 km) north of Peterborough. The population at the 2011 census was 14,456. A 2019 estimate put it at 16,780. History The Ancient Woodland of Bourne Woods is still extant, although much reduced. It originally formed part of the ancient Forest of Kesteven and is now managed by the Forestry Commission. The earliest documentary reference to ''Brunna'', meaning stream, is from a document of 960, and the town appeared in Domesday Book of 1086 as ''Brune''. Bourne Abbey, (charter 1138), formerly held and maintained land in Bourne and other parishes. In later times this was known as the manor of Bourne Abbots. Whether the canons knew that name is less clear. The estate was given by the founder of the ...
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South Forty-Foot Drain
The South Forty-Foot Drain, also known as the Black Sluice Navigation, is the main channel for the land-drainage of the Black Sluice Level in the Lincolnshire Fens. It lies in eastern England between Guthram Gowt and the Black Sluice pumping station on The Haven, at Boston. The Drain has its origins in the 1630s, when the first scheme to make the Fen land available for agriculture was carried out by the Earl of Lindsey, and has been steadily improved since then. Water drained from the land entered The Haven by gravity at certain states of the tide until 1946, when the Black Sluice pumping station was commissioned. The Drain was navigable until 1971, when improvements to the pumping station led to the entrance lock being removed. It is currently being upgraded to navigable status by the Environment Agency, as part of the Fens Waterways Link, with a new entrance lock being completed in December 2008, giving access to the first of the drain, and the upgrading of the southern se ...
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Restoration (England)
The Restoration of the Stuart monarchy in the kingdoms of England, Scotland and Ireland took place in 1660 when King Charles II returned from exile in continental Europe. The preceding period of the Protectorate and the civil wars came to be known as the Interregnum (1649–1660). The term ''Restoration'' is also used to describe the period of several years after, in which a new political settlement was established. It is very often used to cover the whole reign of King Charles II (1660–1685) and often the brief reign of his younger brother King James II (1685–1688). In certain contexts it may be used to cover the whole period of the later Stuart monarchs as far as the death of Queen Anne and the accession of the Hanoverian King George I in 1714. For example, Restoration comedy typically encompasses works written as late as 1710. The Protectorate After Richard Cromwell, Lord Protector from 1658 to 1659, ceded power to the Rump Parliament, Charles Fleetwood and John ...
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