River Maun

Last updated

River Maun
Mansfield, Notts (Maun Valley) - geograph.org.uk - 3045084.jpg
The urban nature of the River Maun in Mansfield can be clearly seen here in the Rock Valley area with the deep-culverting, part of the town centre flood-alleviation scheme
Location
Country England
County Nottinghamshire
Physical characteristics
Source 
  location Kirkby in Ashfield
Mouth River Idle
  location
Markham Moor
Basin features
Tributaries 
  left River Meden
  rightCauldwell Water, Vicar Water, Rainworth Water
River Maun
BSicon uexCONTg.svg
River Idle
BSicon uexSKRZ-Auq.svg
BSicon uexABZgr.svg
River Poulter
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
River Meden and River Maun
BSicon uexSTR.svg
BSicon uxMILL.svg
Rockley mill (dis)
BSicon uexSKRZ-Au.svg
BSicon uexSKRZ-Au.svg
A1 bridges, West Drayton
BSicon uexSTR.svg
BSicon uexABZgl.svg
BSicon uexSTRq.svg
Bevercotes Beck
BSicon uexmKRZu.svg
BSicon uexmKRZu.svg
BSicon exSTRq.svg
disused Bevercotes Colliery railway
BSicon uexSTR.svg
BSicon uexSTR.svg
BSicon uexSKRZ-Yu.svg
BSicon uexSKRZ-Yu.svg
B6387 bridges Bothamsall
BSicon uexSTR.svg
BSicon uxMILL.svg
Haughton mill (dis)
BSicon uexSTRl.svg
BSicon uxWEIRl.svg
River Meden weir
BSicon uexSTRq.svg
BSicon uexABZgr.svg
River Meden
BSicon uexSTR.svg
BSicon uxMILL.svg
Ollerton water mill
BSicon uexSKRZ-Au.svg
A614 bridge
BSicon uexABZgl.svg
BSicon uexSTRq.svg
Rainworth Water (from Rufford)
BSicon uexSKRZ-Yu.svg
B6034 Rufford Road bridge
BSicon STRq.svg
BSicon uxmKRZu.svg
BSicon ABZq+lr.svg
Clipstone Junction
BSicon uexABZgl.svg
BSicon uexSTRq.svg
Vicar Water
BSicon uexSKRZ-Au.svg
A6117 bridge
BSicon uexSKRZ-Yu.svg
B6033 Bath Lane bridge
BSicon uexSKRZ-Au.svg
A6009 bridge
BSicon uxSTRbm.svg
Town Mill (public house)
BSicon uexSKRZ-Au.svg
A6009 bridge
BSicon uexSKRZ-Au.svg
A60 bridge
BSicon uexBHF.svg
Dam
BSicon uexABZgl.svg
BSicon uexSTRq.svg
Cauldwell Water
BSicon uexSKRZ-Eu.svg
Sheepbridge Lane
BSicon uexSKRZ-Eu.svg
Hermitage Lane bridge
BSicon uxSTRbm.svg
Hermitage Mill (warehouse)
BSicon uxmKRZu.svg
viaduct
BSicon uexBHF.svg
Dam
BSicon uexmKRZu.svg
viaduct
BSicon uexBHF.svg
Kings Mill Reservoir
BSicon uexSKRZ-Au.svg
A617 bridge
BSicon uexSKRZ-Yu.svg
B6139 Coxmoor Road bridge
BSicon uexSKRZ-Yu.svg
B6022 Station Road bridge
BSicon uexSKRZ-Yu.svg
B6021 Penny Emma Way bridge
BSicon STRq.svg
BSicon uxmKRZu.svg
BSicon BHFq.svg
Sutton Parkway station
BSicon uexKHSTe.svg
source

The River Maun is a river in Nottinghamshire, England. Its source lies in Kirkby-in-Ashfield, and from there it flows north east through Mansfield (which takes its name from the river), Edwinstowe and Ollerton, these being the heart of the Sherwood Forest area. It becomes known as Whitewater near the village of Walesby and connects to the River Meden temporarily where the Robin Hood Way crosses them. They diverge, and near Markham Moor it merges again with the River Meden this time becoming the River Idle. Its main tributaries are Rainworth Water, Vicar Water and Cauldwell Water.

Contents

The river has been an important source of power, from at least 1086, when there was a watermill in Mansfield. A big increase in the number of mills began in the 1780s, when the frame knitting industry was decimated by the advent of Richard Arkwright's water-powered spinning frame. William Cavendish-Bentinck, 3rd Duke of Portland, encouraged the building of textile mills to relieve unemployment and poverty. Most were converted to do "cotton doubling", and several later became hosiery mills. The conversion of watermills which had formerly ground corn to textile mills led to the building of windmills to carry on milling corn. Although water power has largely ceased, there is still an operational water-mill at Ollerton.

Course

The river rises on the north side of Kirkby-in-Ashfield, just to the south of Sutton Parkway railway station. It is a little above the 490-foot (150 m) contour at this point. It crosses under the railway line, and there are two short culverted sections as it crosses under the B6022 road, to emerge in the Maun Valley Industrial Park. Passing under the B6139 and the A617 roads, it feeds King's Mill Reservoir. [1] The reservoir was once a medieval mill pond, but in 1837, William Bentinck, the fourth Duke of Portland agreed with the millers who leased mills further down the river that a large head of water was required to maintain the water supply throughout the year. He built a dam, and 72 acres (29 ha) of farmland were flooded, some of which he bought from the Unwin family. The work was completed by 1839, when rates to be paid by the millers were agreed, which were to be reduced after 20 years. [2] A 1.5-mile (2.4 km) walk has been created around the lake, from where some of the waterfowl which live on it can be seen. It is also used for sailing. [3] At the exit from the reservoir, the river is crossed by Kings Mill viaduct, built around 1819 for the Mansfield and Pinxton Railway. The engineer for the project was Josias Jessop, and the bridge was the location for the opening ceremony of the railway. A local newspaper described it as "the beautiful five-arched bridge, constructed under the direction of Mr. Jessop, the engineer", when reporting the opening. [4] The central arch carries the date 1817. [5] It was adapted for locomotive traffic in 1847, was restored in 1990, and is a grade II listed structure. [6] It is now used as a footpath, as the railway line was historically diverted around it.

The diverted railway line forms part of the Robin Hood Line, which crosses another millpond just below the reservoir. This supplied the late eighteenth century Hermitage Mill, originally a textile mill, which was then used as a building-materials depot, but has been disused for many years. [7] After crossing under some minor roads and Sheepbridge Lane, where there was another eighteenth-century textile mill, repurposed as a joinery works, and then an internet gaming centre [8] the river is spanned by the disused Drury Dam railway viaduct, [1] this one built in 1875, and consisting of ten round arches, constructed of brick and rock-faced stone. At its west end, a cast-iron arch carries it over Quarry Lane. It is grade II listed, was restored in 1989, and is used as a footpath. [9] Part of it spans the Quarry Lane local nature reserve, on the south bank of the river, where a sculpture created by Lewis Morgan was installed in December 2009. [10] The river continues to weave through the east of Mansfield, where it has been culverted in places. At Bridge Street, the former Town Mill public house was originally the mill owner's house adjacent to the watermill, built around 1775, and restored in the late twentieth century. [11] To the north of the B6033 Bath Lane, there is a disused textile mill, built between 1822 and 1831, which used water power. W. Goldie and Co. extended it in 1880, and altered it to work as a hosiery mill, which it continued to be until 1984. Part of it has been re-used as apartments. [12] Next, the river passes through Carr Bank, with woodland to the east, and a large sewage treatment works to the west. [1] The outflow from the works contributes a significant portion of the flow below this point.

After passing under the A6117 road, the river enters Maun Valley Park, a local nature reserve covering 42 acres (17 ha), which includes water meadows and other wetland habitats. [13] New Mill Lane lies at its northern edge, after which the river passes through more rural scenery. Approaching Clipstone, Cavendish Woods lie to the south east, while extensive fish ponds are located on the other bank. Vicar Water, which flows northwards from Vicar Park, joins on the east bank, before the river is crossed by a railway at Clipstone Junction. It flows eastwards to the south of Edwinstowe, to be joined on the western edge of Ollerton by Rainworth Water, flowing northwards from Rufford Abbey. [1] To the east of the A614 road is Ollerton Watermill, which is still operational, and is open to the public on Sundays in the summer. [14] Passing to the west of New Ollerton, the river flows northwards through open countryside to join the River Meden. After a short distance, two channels are created by a weir, the southern one still called the River Maun, and both proceed eastwards, before turning northwards near Markham Moor roundabout on the A1 road, and joining again to form the River Idle. [1] [15] There are two disused water mills on this stretch, one at Haughton and one called Jacket Mill at Rockley. There were two water mills in Haughton in the reign of King Edward III, during the fourteenth century. [16] Jacket Mill is of red brick construction, and much of it dates from the late eighteenth century, although parts were altered in the nineteenth century. [17]

Mills

The river has provided an important source of power in the past. The Domesday book, produced in 1086, mentions that Mansfield had a watermill, and there are many references to watermills thereafter. In 1292, a fulling mill is mentioned. This was situated to the north of the town, probably near to the later Stanton's Mill, and was part of the process for making woollen cloth. [18]

Mansfield had a cottage industry, which by 1800 consisted of around 700 knitting frames. It operated as a social service, as most of the workers were either orphaned children, or children from families who would otherwise be destitute. Following the invention of the "water-frame", a spinning frame that was powered by a water wheel, which had been invented by Richard Arkwright in 1771 and used in his mills at Cromford, the cottage industry could not compete, and there was widespread unemployment and poverty in Mansfield. In an attempt to remedy the situation, William Cavendish-Bentinck, 3rd Duke of Portland, who was the landowner, and who later became Home Secretary, organised a programme of building water-powered spinning mills along the river. Hermitage Mill was the first to be built, in 1782, and still stands on Hermitage lane. Little Matlock Mill was built three years later on Sheepbridge Lane, and again still stands. [2] Field Mill on Nottingham Road was converted to work with cotton in 1785. Immediately above it was Drury Mill, a corn mill run by Daniel Drury, but this had to be closed in 1791 when the water level in Field Mill Dam was raised, preventing Drury's wheel from working efficiently. [19] Field Mill was in use as a leather works by 1916 [20] and was demolished in 1925. [2]

The next mill on the river was Town Mill, which had been built in 1744, and was used for grinding corn and malt. The miller, William Smith, negotiated with the Duke, and in 1785 he sold the corn milling equipment and refitted it for working with cotton. Having also refitted Field Mill in the autumn, he started a Sunday School in 1786, so that his young workers would be equipped with basic reading and mathematical skills, as well as moral instruction. The practice spread, and Mansfield became known for the good education of its young people. [19] Town Mill became Old Town Mill in 1870, when a steam-powered mill was built to the east of the river, which became known as New Town Mill. [21] Stantons Mill, the next downstream, was built in 1795. [2] By 1900, it had been taken over by Luke Weatherall, who made workmen's boots there. [22] The final textile mill on the river in Mansfield at the time was Bath Mill, on Bath Lane, which began operation in 1792 producing worsted cloth. Benjamin Bagshaw, John Radford and George Simes were the men behind the venture, but it was not a success, and the mill had become a cotton mill by 1800, when it also became one of the first locations in the vicinity to install a steam engine. [23] One effect of the conversion of mills for cotton, rather than grinding corn, was that a number of windmills were built, since corn still had to be milled into flour. The number of windmills in Mansfield rose from three to thirteen between 1774 and 1824. [21]

To the south of Mansfield, the Maun is joined by Cauldwell Water at Bleakhills. Charles and George Stanton chose Bleakhills as a suitable site for a new mill in 1795, and negotiated with the Duke of Portland for permission to build both the mill and cottages for the workers. The cost was about £300. [23]

By 1887, most of the textile mills, including Bleakhills Mill, were marked on maps a being "cotton doubling" mills, a process in which multiple strands of cotton were wound together to form thicker threads. [24] In 1899, only Field Mill and Bath Mill were still marked in this way. Most of the rest were then marked "Hosiery", although Stanton Mill was marked "Boot and Shoe". [25]

There were other mills besides the textile mills. Between Field Mill and Town Mill, there was an iron foundry, called Meadow Foundry, which was built by William Bradshaw and John Sansom in 1852. The site had previously been occupied by a water-powered bark mill, and remained in the ownership of the Duke of Portland. In 1867, Bradshaw and Sansom negotiated a new 14-year lease with the Duke, which included the supply of water from King's Mill reservoir, but they became bankrupt during the following year. It was taken over by James Bownes, who formed a limited company to operate it, and it remained in use until 1960, when the firm moved to new premises, and the site was redeveloped by the Mansfield Brewery. [26] Below the foundry was Borough Mills, which operated as a saw mill. [25] Between Town Mills and Stanton Mill was the Rock Valley Mill, which was operated by Dickenson Ellis as a mustard mill in the early nineteenth century. It was taken over by David Cooper Barringer in 1839, who formed Barringer and Company to operate it. In 1873, they decided to pack the mustard in decorated tin boxes, instead of wooden ones, and made the boxes on site from pre-printed metal sheet. Soon they were making tin boxes for other companies, and the separate Rock Valley Tin Works was formed in 1889. Three years later, a printing works was established, to print the metal sheets, and it became a limited company in 1895. Following several takeovers, it remains in business as Carnaud Metal Box Engineering. [27]

Water Quality

The Environment Agency measure water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at the quantity and varieties of invertebrates, angiosperms and fish. Chemical status, which compares the concentrations of various chemicals against known safe concentrations, is rated good or fail. The Maun is designated as "heavily modified", which means that the channels have been altered by human activity, and the criteria for this designation are defined by the Water Framework Directive. [28]

The water quality of the Maun and its tributaries was as follows in 2019.

SectionEcological StatusChemical StatusLengthCatchmentChannel
Maun from Source to Vicar Water [29] Moderate Fail 11.3 miles (18.2 km)14.61 square miles (37.8 km2)heavily modified
Vicar Water from Source to Maun [30] Poor Fail 2.8 miles (4.5 km)14.61 square miles (37.8 km2)
Maun from Vicar Water to Rainworth Water [31] Moderate Fail 3.5 miles (5.6 km)6.10 square miles (15.8 km2)heavily modified
Rainworth Water from Gallow Hole Dyke to Maun [32] Poor Fail 1.9 miles (3.1 km)2.41 square miles (6.2 km2)
Maun from Rainworth Water to Poulter [33] Moderate Fail 10.0 miles (16.1 km)10.84 square miles (28.1 km2)heavily modified
Bevercotes Beck Catchment (trib of Maun) [34] Moderate Fail 6.7 miles (10.8 km)7.43 square miles (19.2 km2)

Like many rivers in the UK, the chemical status changed from good to fail in 2019, due to the presence of polybrominated diphenyl ethers (PBDE), perfluorooctane sulphonate (PFOS) and mercury compounds, none of which had previously been included in the assessment.

Points of interest

Map all coordinates using: OpenStreetMap  
Download coordinates as: KML

Bibliography

Related Research Articles

<span class="mw-page-title-main">River Wensum</span> River in Norfolk, England

The River Wensum is a chalk river in Norfolk, England and a tributary of the River Yare, despite being the larger of the two rivers. The river is a biological Site of Special Scientific Interest and Special Area of Conservation.

<span class="mw-page-title-main">River Don, Yorkshire</span> River in South Yorkshire and the East Riding of Yorkshire, England

The River Don is a river in South Yorkshire and the East Riding of Yorkshire, England. It rises in the Pennines, west of Dunford Bridge, and flows for 69 miles (111 km) eastwards, through the Don Valley, via Penistone, Sheffield, Rotherham, Mexborough, Conisbrough, Doncaster and Stainforth. It originally joined the Trent, but was re-engineered by Cornelius Vermuyden as the Dutch River in the 1620s, and now joins the River Ouse at Goole. Don Valley is a UK parliamentary constituency near the Doncaster stretch of the river.

<span class="mw-page-title-main">River Dearne</span> River in South Yorkshire, England

The River Dearne South Yorkshire, England flows roughly east for more than 30 kilometres (19 mi), from its source just inside West Yorkshire. It flows through Denby Dale, Clayton West, Darton, Barnsley, Darfield, Wath upon Dearne, Bolton on Dearne, Adwick upon Dearne and Mexborough to its confluence with the River Don at Denaby Main. Its main tributary is the River Dove, which joins it at Darfield. The river was one of those affected by the 2007 United Kingdom floods.

<span class="mw-page-title-main">Ollerton</span> Town in Nottinghamshire, England

Ollerton is a town in the Newark and Sherwood District, Nottinghamshire, England, on the edge of Sherwood Forest in the area known as the Dukeries. It forms part of the civil parish of Ollerton and Boughton. The population of this civil parish at the 2011 census was 9,840.

<span class="mw-page-title-main">River Meden</span> River in Nottinghamshire, England

The River Meden is a river in Nottinghamshire, England. Its source lies just north of Huthwaite, near the Derbyshire border, and from there it flows north east through Pleasley and Warsop before merging temporarily with the River Maun near Bothamsall. The rivers divide after a short distance and go on separately to a point near Markham Moor where they once more combine to form the River Idle.

<span class="mw-page-title-main">River Rother, West Sussex</span> River in Hampshire and West Sussex, England

The River Rother flows from Empshott in Hampshire, England, to Stopham in West Sussex, where it joins the River Arun. At 52 kilometres (32 mi) long, most of the river lies within West Sussex except for the first 10 kilometres (6.2 mi) which lie in Hampshire. The upper river, from its source to Midhurst, has been used to power watermills, with the earliest recorded use being in 1086, when the Domesday survey was conducted. Although none are still operational, many of the buildings which housed the mills still exist, and in some cases, still retain their milling machinery. This upper section is also noted for a number of early bridges, which have survived since their construction in the fifteenth, sixteenth and seventeenth centuries.

<span class="mw-page-title-main">River Poulter</span> River in England

The River Poulter which rises near Scarcliffe in Derbyshire, England is a tributary river of the River Idle in Nottinghamshire. It supplied power to mills along its route, most of which are now gone, although their mill ponds remain. Cuckney mill building is used as a primary school. The river has been dammed to create several lakes in the Dukeries estates of Welbeck Abbey and Clumber House now the National Trust property of Clumber Park. The ornamental Gouldsmeadow Lake, Shrubbery Lake and Great Lake on the Welbeck estate are supplied by a tributary of the Poulter, while Carburton Forge Dam and Carburton Dam were built to power a forge and a mill. Clumber Lake, consisting of an upper and lower lake, which is spanned by a Grade II* listed ornamental bridge, is part of the Clumber estate, and has suffered from subsidence.

<span class="mw-page-title-main">Ollerton and Boughton</span> Civil parish of Nottinghamshire, England

Ollerton and Boughton is a civil parish in the Newark and Sherwood district of Nottinghamshire, England. The main settlements are the town of Ollerton and the villages of New Ollerton and Boughton. The civil parish was formed in 1996, when the civil parishes of Ollerton and Boughton were merged. The population of the civil parish at the time of the 2011 census was recorded as 9,840.

<span class="mw-page-title-main">Peasey Beck</span> Stream in Cumbria, England

Peasey Beck is a 19.6-kilometre-long (12.2 mi) beck flowing through Cumbria, England. It rises on Lambrigg Fell where it is known as the Sparishaw Beck, flows through Killington Reservoir and converges with Stainton Beck to form the River Bela at Milnthorpe. Prior to 1913, it was known as the River Beela throughout its length.

<span class="mw-page-title-main">Stainton Beck</span> Stream in Cumbria, England

Stainton Beck is a watercourse in Cumbria, England. Its upper reaches are known as St. Sunday's Beck.

<span class="mw-page-title-main">Rainworth</span> Village in Nottinghamshire, England

Rainworth is a village in the ceremonial county of Nottinghamshire in the East Midlands of England. It is split between the local government districts of Newark and Sherwood and Mansfield.

<span class="mw-page-title-main">Rainworth Water</span> Tributary of the River Maun near Rainworth, Nottinghamshire, England

Rainworth Water is a watercourse that is a tributary of the River Maun near Rainworth, Nottinghamshire, England. It is characterised by a number of lakes, including that which forms part of the country park at Rufford Abbey. L Lake at Rainworth forms part of the Rainworth Lakes Site of Special Scientific Interest. There are two designated Local Nature Reserves along its length, one of which is also known by the name Rainworth Water. The Rainworth Water LNR is owned and managed by Nottinghamshire County Council.

<span class="mw-page-title-main">River Teise</span> River

The River Teise is a tributary of the River Medway in Kent, England.

<span class="mw-page-title-main">River Drone</span> River in Derbyshire, England

The River Drone is a river which flows south from its source on the Sheffield, South Yorkshire, border. It flows through Dronfield, Unstone and Unstone Green in Derbyshire before merging at Sheepbridge to the north of Chesterfield with the Barlow Brook. Below the junction, it is often referred to as the River Whitting. It then flows south-east till it merges with the River Rother at Brimington Road North (B6050) at Chesterfield. It is one of the three main tributaries of the Rother.

<span class="mw-page-title-main">River Dove, Barnsley</span> River in South Yorkshire, England

The River Dove is a river that extends through the Low Valley in Barnsley, England. It flows from Worsbrough Reservoir to its confluence with the River Dearne.

<span class="mw-page-title-main">Vicar Water</span> River in Nottinghamshire, England

Vicar Water is a small river in Nottinghamshire, England. It is a tributary of the River Maun, and runs through an area which was once the royal hunting ground of Clipstone Park. It gained its present name in the early nineteenth century, and was dammed in 1870, in order to make a trout fishery, which was used to stock the lakes at nearby Welbeck Abbey. Since the cessation of coal mining, much of it has been incorporated into a country park, and is a designated Local Nature Reserve.

<span class="mw-page-title-main">Bentley Brook, Bradbourne</span> River in England

The Bentley Brook or Bradbourne Brook is a small tributary of the River Dove in Derbyshire, England, and is 14.5 kilometres long

<span class="mw-page-title-main">Eller Beck</span> River in North Yorkshire, England

The Eller Beck is a small river in North Yorkshire, England, that flows through the town of Skipton and is a tributary of the River Aire. Its channel was heavily modified to supply water to mills in the 18th and 19th centuries, and although all the mills have closed, the water now supplies power to the National Grid, generated by a turbine at High Corn Mill. The beck flows through several underground culverts in Skipton that contribute to the flood risk. To alleviate flooding in Skipton town centre, a scheme involving two flood water storage reservoirs was designed and eventually completed in 2017.

<span class="mw-page-title-main">Roman River</span> River in Essex, England

The Roman River is a river that flows entirely through the English county of Essex. It is a tributary of the River Colne, flowing into its tidal estuary below Colchester. The lower end of the Roman River is also tidal, with tidal water flowing upstream to just above Fingringhoe.

<span class="mw-page-title-main">Walverden Water</span> River in Lancashire, England

Walverden Water is a minor river in Lancashire, England. It is approximately 2.6 miles (4.2 km) long and has a catchment area of 5.04 square miles (1,304.23 ha).

References

  1. 1 2 3 4 5 Ordnance Survey, 1:25000 map
  2. 1 2 3 4 "The History of Kingsmill Reservoir". Kings Mill. Archived from the original on 3 July 2017. Retrieved 3 June 2011.
  3. "King's Mill Reservoir". Ashfield District Council. Archived from the original on 10 April 2011. Retrieved 3 June 2011.
  4. Skempton 2002 , p. 363
  5. "King's Mill Viaduct (centre arch)". Geograph.
  6. Historic England. "Railway Viaduct, Kings Mill Lane (1288554)". National Heritage List for England . Retrieved 3 June 2011.
  7. Historic England. "Hermitage Mill, Mansfield (1288578)". National Heritage List for England . Retrieved 11 June 2011.
  8. Historic England. "Matlock Mill, Mansfield (1279862)". National Heritage List for England . Retrieved 11 June 2011.
  9. Historic England. "Drury Dam Railway Viaduct, Mansfield (1207187)". National Heritage List for England . Retrieved 3 June 2011.
  10. "Quirky sculpture unveiled in Quarry Lane Nature Reserve, Mansfield". Nottinghamshire County Council. Archived from the original on 20 March 2012. Retrieved 3 June 2011.
  11. Historic England. "Town Mill public house, Mansfield, now a restaurant (1279885)". National Heritage List for England . Retrieved 11 June 2011.
  12. Historic England. "Bath Mill, Mansfield (1207153)". National Heritage List for England . Retrieved 11 June 2011.
  13. "Maun Valley Park Local Nature Reserve". Chad. Archived from the original on 4 March 2016. Retrieved 11 June 2011.
  14. "Heritage Museums". Nottinghamshire County Council. Archived from the original on 6 September 2008. Retrieved 11 June 2011.
  15. CAMS 2006, p. 31.
  16. Brown 1896
  17. Historic England. "Jacket Watermill, West Drayton (1266858)". National Heritage List for England . Retrieved 11 June 2011.
  18. Morley & Bradbury 1996 , p. 3
  19. 1 2 Morley & Bradbury 1996 , p. 16
  20. Ordnance Survey, 1:2500 map, 1916
  21. 1 2 Morley & Bradbury 1996 , p. 18
  22. Morley & Bradbury 1996 , p. 12
  23. 1 2 Morley & Bradbury 1996 , p. 17
  24. Ordnance Survey, 1:2500 map, 1887
  25. 1 2 Ordnance Survey, 1:2500 map, 1899
  26. Morley & Bradbury 1996 , pp. 21–22
  27. Morley & Bradbury 1996 , pp. 30–31
  28. "Glossary (see Biological quality element; Chemical status; and Ecological status)". Catchment Data Explorer. Environment Agency. 17 February 2016.
  29. "Maun from Source to Vicar Water". Catchment Data Explorer. Environment Agency.
  30. "Vicar Water from Source to Maun". Catchment Data Explorer. Environment Agency.
  31. "Maun from Vicar Water to Rainworth Water". Catchment Data Explorer. Environment Agency.
  32. "Rainworth Water from Gallow Hole Dyke to Maun". Catchment Data Explorer. Environment Agency.
  33. "Maun from Rainworth Water to Poulter". Catchment Data Explorer. Environment Agency.
  34. "Bevercotes Beck Catchment (trib of Maun)". Catchment Data Explorer. Environment Agency.

Commons-logo.svg Media related to River Maun at Wikimedia Commons

Coordinates: 53°15′N0°57′W / 53.250°N 0.950°W / 53.250; -0.950