Английская Википедия:Duke of Northumberland's River
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The Duke of Northumberland's River or D. O. N. River consists of separate upper and lower artificial watercourses in west London, United Kingdom. The older name Isleworth Mill Stream/River more accurately describes the economic motivation behind its construction. The first section draws water via a sluice from the Colne — a source river which has seven distributaries, many of which are man-made — today an extended distance (to bypass Heathrow Airport) of about Шаблон:Convert into the Crane; its lower section of about Шаблон:Convert draws water from that small river in Whitton, Twickenham and discharges it via neighbouring Isleworth, passing Mill Plat into the tidal Thames. A sluice underneath Mill Plat feeds the main lake in Syon Park.
Western section
The western section was constructed during the reign of King Henry VIII of England to augment the flow supplying existing mills and to supply new mills, a source of revenue for the Duke of Northumberland's estate with the further benefit of irrigation for his tenants' fields. Most of the local topsoil was quite thin, on fast-draining gravel.[1] The dukes and their Somerset-styled forebears were lords of the manor of Isleworth (1547–1554 and from 1594)[2]Шаблон:Efn and Twickenham (1538–1541), retaining much of the dwindling agricultural land until the 20th century. The family cemented its foothold in Isleworth by acquiring and rebuilding a former grandiose monastery by the Thames there, which had become Syon House in 1594; it remains the family's home in southern England.
In 1530, a record lists an increase, probably temporary, of 42 labourers working on a new river cut from Longford (probably the Duke of Northumberland's River).[3]
This section diverts a small proportion of water from the River Colne at Longford, south then eastwards to the River Crane. The shallow canal flows through the north of Stanwell, Bedfont and Feltham. For a large part of its early course, it flows alongside its younger "twin", the Longford River. The first part helped to irrigate fields and orchards of Longford, then those of Heathrow and Stanwell.[4] It was diverted west and then south in 1944 when Heathrow Airport was built.[5] Both minor "canals" were moved further under the building scheme for Heathrow Terminal 5. They skirt the western and southern perimeter of Heathrow Airport then diverge after The Two Bridges, which are bridges of the truck road-bypassedШаблон:Clarify Hatton Road in Bedfont.[6]
The river is carvedШаблон:Clarify east to join the Crane in patchy woodland known as Donkey Wood, by Baber Bridge at the west end of Hounslow Heath. Шаблон:Coord
Eastern section
This section diverts water from the Crane in Kneller Gardens, Whitton, Twickenham, eastward then northward past The Stoop and Twickenham Stadium rugby stadiums, through Isleworth (originally to its mill), then onwards to supply the ornamental ponds in the Duke of Northumberland's estate at Syon Park. Further sluices here control the flow into the park and the River Thames at Isleworth Ait.
This part is the older — it was built in the time of Syon Abbey, over 100 years before it was inherited, in 1594, by wife of the "wizard earl", Henry Percy, 9th Earl of Northumberland, Dorothy (née Devereux) which automatically became his own as this inheritance preceded the Married Women's Property Act 1870.
The Duke of Northumberland's River can thus be described as a distributary of the Colne and a tributary of the Crane; it is also a distributary of the Crane and a tributary of the Thames. Шаблон:Coord
See also
Notes
References
Citations
Bibliography
- Sherwood, Philip. (2006) Around Heathrow Past & Present. Stroud: Sutton Publishing Шаблон:ISBN
External links
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- ↑ 'Twickenham: Introduction', in A History of the County of Middlesex: Volume 3, editor: Susan Reynolds (London, 1962), p. 139. British History Online http://www.british-history.ac.uk/vch/middx/vol3/pp139-147. Accessed 18 August 2017.
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ Sherwood 2006, p.11
- ↑ Sherwood 2006, p.10
