Colne | |
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Location | |
Country | England |
Counties | Hertfordshire, Greater London, Buckinghamshire, Surrey, Berkshire |
Towns | Watford, Rickmansworth, Uxbridge, West Drayton, Staines-upon-Thames |
Physical characteristics | |
Source | Unnamed brook |
• location | east of Bell Bar, Brookmans Park |
• coordinates | 51°43′50″N0°10′47″W / 51.7306°N 0.1798°W |
• elevation | 410 feet (120 m) |
2nd source | "Water End" brook |
• location | east side of North Mymms Park (coalesence of two streams, liable-to-flood meadow) |
Mouth | River Thames |
• location | Staines-upon-Thames town centre |
• coordinates | 51°25′58″N0°30′55″W / 51.4329°N 0.5152°W |
• elevation | 48 feet (15 m) |
Length | 58 km (36 mi) |
Discharge | |
• location | Denham, Buckinghamshire (rate at lower coalescence) |
• average | 4.05 m3/s (143 cu ft/s) |
• minimum | 0.74 m3/s (26 cu ft/s)26 August 1976 |
• maximum | 18.4 m3/s (650 cu ft/s)14 October 1993 |
Discharge | |
• location | Berrygrove, Berry Grove Lane, Watford (rate at mid-to-upper coalescence) |
• average | 0.79 m3/s (28 cu ft/s) |
Basin features | |
River system | Thames Basin |
Tributaries | |
• left | Mimmshall Brook, Potters Bar Brook, Tyttenhanger Stream, Tykes Water (The Brook (Radlett)), Hillfield Brook, River Pinn |
• right | Ellen Brook and river: Ver, Gade, Chess, Misbourne |
Number of distributaries including namesake: | 6 |
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The Colne is a river and a tributary of the River Thames in England. Just over half its course is in south Hertfordshire. Downstream, it forms the boundary between Buckinghamshire and the London Borough of Hillingdon. The confluence with the River Thames is on the Staines reach (above Penton Hook Lock) at Staines-upon-Thames.
Two of its distributaries, constructed in the 1600 – 1750 period largely for aesthetic reasons for Hampton Court and for Syon Park, have been maintained. Their main purpose was not drinking water but these can be likened to the New River in scale and in date. Crossing its route, many viaducts and a canal, the intersecting Grand Union Canal, have been recognised for pioneering engineering during the Industrial Revolution.
Digging for gravel and clay along its lower course near Rickmansworth has created a belt of flooded pits below the water table, as established lakes, many of which are well-adapted habitats for wildlife, protected as nature reserves. The river, meadows and lakes form the Colne Valley regional park covering 43 square miles (110 km2).
The Colne becomes universally so-named after two close subterranean streams converge at a spring, or in very wet weather in the meadows above, all along the east side (Tollgate Road) of North Mymms Park in Hertfordshire. The source streams are long, multi-source, in final, northern stages, partly underground tributaries: a north-eastern, which can be considered the upper Colne; and the Mimmshall Brook. Their main sources are 2.5 to 4 mi (4.0 to 6.4 km): in western Northaw, Brookmans Park, Hadley, London and Borehamwood, draining much of those places. [1] A seasonal, intra-parochial stream runs under the seven-building village of North Mymms draining most of the park, which, with adjoining woods is a small square plateau, sloping down to its corners except the south-west. [2] [3]
Shallow swallow holes of the two brooks are in North Mymms' Water End, centred on so-named combined surface flow. From the Water End Swallow Holes the Colne runs west, longer NNW, then west then receives the Ellen Brook and turns SSW, then meanders south-west, bounding central and residential Watford and Oxhey, also bounding Rickmansworth and Batchworth, then for a similar total stretch bounding Greater London (and Spelthorne), east and (through anabranch ditches) Buckinghamshire, west. Specifically, it passes between West Hyde, near Maple Cross, and Harefield, passes Denham Green then passes Uxbridge, where it parallels the Grand Union Canal and its first main anabranch, the Frays River which is co-fed by the Pinn between Cowley and Yiewsley, Greater London. The Colne Brook splits off as a distributary between New Denham and Uxbridge. After this, at West Drayton, the Frays rejoins and the Wraysbury River, the second main anabranch, and Duke of Northumberland's River divide off.
Soon after, at Longford, the intake is given to the Longford River, a 12-mile (19 km) artificial channel created in 1610 for King Charles I to supply the water features in Bushy Park and the rectangular lakes in Hampton Court Park. [4]
The Colne's drainage basin extends almost as far north again as its northern limit – the inflowing Gade, Ver and Misbourne extend well into the Chilterns. Opposite, the other 2⁄3 of outer west and north-west London is drained by the Pymmes Brook, Brent, or Crane sub-basins of the Thames. In the north-west, centred on Tring's northern boundary the Chiltern ridge is most noticeable, a watershed of this basin and that of the River Great Ouse, north and east towards the Wash.
The villages of Colney Heath east of St Albans, London Colney south of St Albans, Colney Street (almost wholly a large business park) north of Radlett and Colnbrook between Slough and Heathrow take their name from the river. Three Rivers District Council covers part of Hertfordshire and is named after the River Colne and its two tributaries, the River Chess and the River Gade.
Among early proposals to link the river to London was one in 1641 by Sir Edward Forde for a navigable canal, the main purpose of which seems to have been the supply of clean water, and two in 1766, for canals from Marylebone to the river at Uxbridge and another from Marylebone to West Drayton. [5]
The river underwent considerable change in the 1790s, when the Grand Junction Canal (which became part of the Grand Union Canal in 1929) was routed along the valley and still takes the river channel for part of its course. Construction began from Brentford, where it used for 3 miles (4.8 km) the channel of the River Brent, and progressed westwards then northwards, with it reaching Uxbridge in November 1794. To reach the Midlands it continued along the river channel until its junction with the River Gade, which it ran parallel to, but did not take over the channel. [6] The Slough Arm was built in 1882 which required three aqueducts to carry it close to its junction with the Grand Junction, to cross the Fray's River, the River Colne and the Colne Brook. [7]
Between Croxley Green, where the River Gade joins the Colne, and Thorney/West Drayton, below the Slough Arm, the river channels thread their way between many large lakes, some of which were once watercress beds, some chalk pits, [8] and some of which were the result of brickmaking, an industry that developed over several miles of the valley after 1800, when the Grand Junction Canal company advertised the presence of good brick earth, discovered during the construction of the canal. [5]
There are two London Coal Duty markers beside the river, which mark points at which duty became payable on coal entering the London area. The first is on the north side of the river in Colney Heath Local Nature Reserve, and is a square-section cast iron pillar made by Henry Grissell at his Regents Canal ironworks and erected in 1861 or 1862. It is 5 feet (1.5 m) high and is painted white. [9] The second is a stone obelisk, 13 feet (4.0 m) high, with a square base, which was erected at Colne Bridge in 1861. It was moved from its original position to the other side of the river in 1984 when it was repaired by Watford Borough Council. [10] It is close to the five-arched Colne Viaduct, which was built in 1837 to carry the London to Birmingham Railway over the river. Each of the arches spans around 40 feet (12 m) and is 45 feet (14 m) high. The structure was designed by Robert Stephenson, and is grade II listed. [11]
At London Colney, there is a seven-arched brick bridge which carries Barnet Road over the river. It dates from 1774 and is called Telford's Bridge, although it is not thought to have been designed by Thomas Telford. It was modified in the 20th century when parapets and railings were added. [12]
There was a long-running dispute over water levels in the Batchford area, following the construction of the Grand Junction Canal, which were resolved in 1825, when an 8.2-foot (2.5 m) obelisk was erected in a pond, to act as a water gauge. The obelisk records the agreement made between the canal company, John Dickinson who was the owner of papermills at Batchworth, and R. Williams of Moor Park, who was the landowner. [13]
From its mouth to its source, the Colne's named tributaries, anabranches and to-Thames distributaries are:
The Grand Union Canal in England is part of the British canal system. It is the principal navigable waterway between London and the Midlands. Starting in London, one arm runs to Leicester and another ends in Birmingham, with the latter stretching for 137 miles (220 km) with 166 locks from London. The Birmingham line has a number of short branches to places including Slough, Aylesbury, Wendover, and Northampton. The Leicester line has two short arms of its own, to Market Harborough and Welford.
Yiewsley is a large suburban village in the London Borough of Hillingdon, England, 2 miles (3 km) south of Uxbridge, the borough's commercial and administrative centre. Yiewsley was a chapelry in the ancient parish of Hillingdon, Middlesex. The population of the ward was 12,979 at the 2011 Census.
Colnbrook is a village in the Slough district in Berkshire, England. It lies within the historic boundaries of Buckinghamshire, and straddles two distributaries of the Colne, the Colne Brook and Wraysbury River. These two streams have their confluence just to the southeast of the village. Colnbrook is centred 3 miles (4.8 km) southeast of the Slough town centre, 4 miles (6.4 km) east of Windsor, and 19 miles (31 km) west of central London.
Rickmansworth is a town in south-west Hertfordshire, England, located approximately 17 miles (27 km) north-west of central London, 5 miles (8 km) south-west of Watford and inside the perimeter of the M25 motorway. The town is mainly to the north of the Grand Union Canal and the River Colne.
Uxbridge Vine Street station opened on 8 September 1856 as Uxbridge Station and was the earliest of three railway stations in Uxbridge, London.
Longford is a suburban village in the London borough of Hillingdon, England. It is immediately northwest of London Heathrow Airport, which is in the same borough. It is the westernmost settlement in Greater London, very close to the borders of both Berkshire and Surrey.
The River Crane, a tributary of the River Thames, runs 8.5 miles (13.6 km) in West London, England. It forms the lower course of Yeading Brook. It adjoins or passes through three London boroughs: Hillingdon, Hounslow and Richmond upon Thames, in the historic county of Middlesex. The drainage basin is heavily urbanised but many of the Hayes to Whitton flood-meadows have been conserved, forming a narrow, green vale, opening out to what remains of Hounslow Heath in the centre – a near-continuous belt of semi-natural habitat.
The River Ash is a small, shallow river in Surrey, England. Its course of 10 kilometres (6.2 mi) is just outside Greater London. Work has been carried out to re-align, clear and build up a small, Littleton head of water and create two backwaters. One backwater dates to the medieval period; the other to the 1990s. It flows as one of the six distributaries of the River Colne from the south of Staines Moor immediately south of the Staines Bypass eastwards through the rest of the borough of Spelthorne before meeting the River Thames.
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 of about 5 miles (8 km) into the Crane; its lower section of about 1.8 miles (2.9 km) 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.
The Watford and Rickmansworth Railway (W&RR) ran services between Watford and Rickmansworth in Hertfordshire, England. The company was incorporated in 1860; the line opened in 1862. The Rickmansworth branch was closed in 1952, and the remaining line was gradually run down and eventually closed in 1996.
Maple Cross is a village in Hertfordshire, England, which up until the Second World War consisted of an inn, a blacksmith's shop and a few cottages. Today there are around 800 postwar council houses. Some of these have been sold into private ownership. The area is close by junction 17 of the M25 motorway, which makes up the western boundary of the village. It lies on the western fringe of Rickmansworth, about 5 miles (8.0 km) west of Watford and 6 miles north of Uxbridge.
Stanwell Moor is a village and moor in the Borough of Spelthorne, approximately 17 miles (27 km) west of central London. Historically part of the county of Middlesex, it was transferred to Surrey in 1965. West of its generally narrow moor is the M25 London Orbital Motorway and the village is 1 mile (1.6 km) southwest of Heathrow Airport Terminal 5.
Staines Moor is a 510.8-hectare (1,262-acre) biological Site of Special Scientific Interest north of Staines-upon-Thames in Surrey. It is part of the South West London Waterbodies Ramsar site and a Special Protection Area
The Colne Brook is a river in England that is a distributary of the River Colne which runs from Uxbridge Moor, there forming the western border of Greater London, to the River Thames just below Bell Weir Lock in Hythe End, Wraysbury, Berkshire.
The Wraysbury River is an anabranch of the River Colne to the west of London.
Frays River is a semi-canalised short river in England that branches off the River Colne at Uxbridge Moor and rejoins it at West Drayton. It is believed to be a mainly man-made anabranch north of the confluence with the River Pinn to feed watermills in the Parish of Hillingdon. The river is believed to be named after John Fray who owned Cowley Hall in the fifteenth century. Other names for the river are the Uxbridge and Cowley Mill Stream, the Cowley Stream or the Colham Mill Stream. Two of the three mills in Hillingdon Parish recorded in the Domesday book are believed to have been located on the southern section of the river.
The Pinn is a suburban, outer west London river. It has dendritic headwaters, the furthest is considered its source – in Harrow Weald. Its confluence with Frays River makes it a tributary of the Colne. It is one of three principal rivers wholly in the historic county of Middlesex.
Otter Dock was a branch of the Grand Junction Canal in Yiewsley, Middlesex.
National Cycle Route 61 is part of the National Cycle Network managed by the charity Sustrans. It runs for 34 miles from Maidenhead (Berkshire) to Rye House (Hertfordshire) via Uxbridge, Watford, St Albans, Hatfield, Welwyn Garden City and Hertford in the United Kingdom.