River Whitewater

Last updated

Whitewater
GreywellMill(AndrewSmith)Apr2006.jpg
Greywell Mill on the upper reaches of the River Whitewater
Location
Country England
Counties Hampshire
Physical characteristics
Source 
  location Bidden
  coordinates 51°14′15″N0°59′14″W / 51.2376°N 0.9871°W / 51.2376; -0.9871
Mouth River Blackwater
  location
South-east of Swallowfield
  coordinates
51°21′59″N0°56′10″W / 51.3663°N 0.9361°W / 51.3663; -0.9361
Length12.2 mi (19.6 km)
Basin features
Tributaries 
  right River Hart

The River Whitewater rises at springs near Bidden Grange Farm between Upton Grey and Greywell in Hampshire, England. It flows northeast and is a tributary of the River Blackwater near Swallowfield. Its headwaters flow over chalk and there is little pollution making the River Whitewater rich in wildlife. [1] It was noted on Jansson's map of Hampshire of 1646. [2]

Contents

The settlements of Greywell, North Warnborough, Hook, Hartley Wintney, Rotherwick, West Green, Mattingley, Bramshill and Heckfield lie on the River Whitewater. [3]

The river contains a variety of species of fish. Fishing on part of the river is controlled by Farnborough and District Angling Society which has separate coarse and fly fishing sections. Like many rivers in the south of England, non-indigenous mink and signal crayfish are present.

Route

River Whitewater
BSicon uexCONTg.svg
River Blackwater
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
River Whitewater
BSicon uexSTR.svg
BSicon uexSTRl.svg
BSicon uexCONTgeq.svg
River Blackwater
BSicon uexSKRZ-Eu.svg
Bridge
BSicon uexABZgl.svg
BSicon uexSTR+r.svg
BSicon uxMILL.svg
BSicon uexSTR.svg
Riseley Mill
BSicon uxWEIRr.svg
BSicon uexSTRr.svg
BSicon uexSKRZ-Eu.svg
Heckfield Bridge, Bramshill Rd
BSicon uexABZgl.svg
BSicon uexSTRq.svg
BSicon uexCONTgeq.svg
River Hart
BSicon uexABZgl.svg
BSicon uexSTR+r.svg
BSicon uxMILL.svg
BSicon uexSTR.svg
Holdshott Mill
BSicon uexSKRZ-Yu.svg
BSicon uexSKRZ-Yu.svg
B3011 Holdshott bridge
BSicon uxWEIRr.svg
BSicon uexSTRr.svg
BSicon uexKBHFaq.svg
BSicon uexSKRZ-Euq.svg
BSicon uexABZgr.svg
Highfield Park lake
BSicon uexSKRZ-Eu.svg
Mattingley Clappers Bridge
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
BSicon uexSTR.svg
BSicon uxMILL.svg
Dipley Mill
BSicon uexSTRl.svg
BSicon uxWEIRl.svg
BSicon uexSKRZ-Eu.svg
Dipley Bridge
BSicon uexABZgl.svg
BSicon uexSTR+r.svg
BSicon uxMILL.svg
BSicon uexSTR.svg
Hook Mill
BSicon uxWEIRr.svg
BSicon uexSTRr.svg
BSicon uexSKRZ-Au.svg
A30 Crooked Billet Bridge
BSicon CONTgq.svg
BSicon uxmKRZu.svg
BSicon CONTfq.svg
Railway bridge
BSicon uexSKRZ-Bu.svg
UK-Motorway-icon.svg M3 motorway bridge
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
BSicon uexSTR.svg
BSicon uxMILL.svg
Poland Mill
BSicon uexSTRl.svg
BSicon uxWEIRl.svg
BSicon uxWEIRf.svg
weirs
BSicon uexSKRZ-Au.svg
A287 bridge
BSicon uexSTR.svg
BSicon uSTR+l.svg
BSicon uCONTfq.svg
Basingstoke Canal
BSicon uexSKRZ-Yu.svg
BSicon uSKRZ-Yu.svg
B3349 Hook Road Bridges
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
BSicon uSTR.svg
BSicon uexSTR.svg
BSicon uxMILL.svg
BSicon uSTR.svg
Warnborough Mill, Odiham
BSicon uexSKRZ-Eu.svg
BSicon uexSKRZ-E.svg
BSicon uLIFT.svg
North Warnborough
ford and lift bridge
BSicon uexSTRl.svg
BSicon uxWEIRl.svg
BSicon uSTR.svg
BSicon uexSTR+l.svg
BSicon uexABZgr.svg
BSicon uSTR.svg
BSicon uexSTR.svg
BSicon uxMILL.svg
BSicon uSTR.svg
Castle Mill
BSicon uexSTRl.svg
BSicon uxWEIRl.svg
BSicon uSTR.svg
BSicon uSTR+l.svg
BSicon uxKRZu.svg
BSicon uSTRr.svg
BSicon uextSTReq.svg
BSicon uKBHFe.svg
BSicon uexKBHFeq.svg
BSicon uexSTR.svg
Greywell Tunnel (derelict)
BSicon uxWEIRf.svg
weirs
BSicon uexSKRZ-Eu.svg
Deptford Bridge
BSicon uexABZgl.svg
BSicon uexSTR+r.svg
BSicon uxMILL.svg
BSicon uexSTR.svg
Greywell Mill
BSicon uxWEIRr.svg
BSicon uexSTRr.svg
BSicon uexABZgl.svg
BSicon uexKHSTeq.svg
spring
BSicon uexKHSTe.svg
springs at Bidden

The Whitewater rises as a series of springs and channels near Bidden, in the Odiham Fen Site of Special Scientific Interest (SSSI). The underlying chalk aquifer supplies base-rich water which encourages the growth of fen vegetation, notably lesser tussock-sedge and giant spearmoss. [4] Almost immediately, the channels form into a pond called Mill Head, which formed part of the infrastructure for Greywell Mill. The small mill building, with an attached house, is a grade II listed structure. [5] There are further springs and channels as the river heads north eastwards, to reach Deptford Bridge. Close by is the eastern portal of Greywell Tunnel, a 1,230-yard (1,120 m) tunnel built in 1792 for the Basingstoke Canal. The portal was restored in 1975, [6] and although the canal is now navigable almost to its entrance, the tunnel is unlikely to be restored, as part of the roof collapsed, it has been colonised by a large number of bats, and the M3 motorway has been built over the original route beyond the tunnel. [7] Beyond Deptford Bridge, there are two weirs, and Greywell Pumping Station stands on the right bank. This has extracted groundwater from the underlying chalk aquifer for use as drinking water since the early 1900s. Around 6 to 7 Ml per day are extracted, and in 2012 a study was carried out to see what effects the extraction was having on the Odiham Fen SSSI. There is a second part of the SSSI beyond the pumping station. [4]

The canal crosses over the river on an aqueduct, and the river curves around the edge of Odiham Castle. Only a small part of the grade I listed octagonal keep, construction of which may have been for King John, remains. [8] It was built between 1207 and 1212, and the grounds of the moated site are a scheduled monument, although parts of the earthworks and moat were damaged when the Basingstoke Canal was built. [9] To the east of the castle is the site of Castle Mill, [10] a ford where Mill Lane crosses the river, and then the mill pond for Warnborough Mill at Warnborough Green. The mill itself consisted of two storeys and an attic, with a two-storey house attached. It dates from the 18th century, and has been converted into a restaurant. [11] Just beyond the tailrace the river is crossed by the B3499 Hook Road, and the A287 road, with a weir between the two bridges. Several more weirs follow, as the river threads its way between Lodge Farm on the right bank, the core of which is a grade II* listed timber framed hall-house, dating from the 15th century, [12] and the site of a Roman villa on the left bank. [13] Next comes Poland Mill, a large two-storey 18th century rectangular building, which originally had six water wheels, of which one with a cast iron frame remains. [14]

The next section, which follows a more northerly course, is marked by bridges carrying the M3 motorway, the South West Main Line railway and the A30 road over the river, to the east of Hook. Beyond them is Hook Mill, with two storeys and an attic, and an attached house with two storeys. They date from the 17th and 18th centuries, and both now form part of a single house, in which the huge timbers of the mill building are still visible. [15] Dipley Bridge carries a road over the river at the hamlet of Dipley, beyond which is Dipley Mill. The building is predominantly 18th century with modern additions, but clearly has earlier origins. [16] After Mattingley Clappers Bridge there is a long rural section where a stream from the lake in Highfield Park joins the left bank, but there are no road crossings until the B3011 road is reached at Holdshott Farm, near the village of Hazeley. [17] Holdshott farm house is a late 18th century building with two storeys and an attic. A timber-framed mill adjoins the north end, but it has been extensively renovated, and the cladding is modern. [18]

The main tributary of the Whitewater is the River Hart, which joins on the right bank, before the combined flow passes under Heckfield Bridge. It has a single cambered arch, and was constructed of red brick in the mid-19th century. [19] Riseley Mill is located on the final stretch, before the river crosses under another bridge to join the Blackwater River on its left bank. [17] The mill building is the tallest on the river, having four storeys. [20]

Ecology

In its upper reaches, the Whitewater is a classic chalk stream. Its water is derived from an underlying chalk aquifer, as a series of spring in the Odiham Fen SSSI. Although it flows through peat in the fen, the water is clear, and the flows are stable. As the river approaches Hook, the geology alters, with the underlying chalk replaced by clay and gravel substrates. Here the flow becomes less stable, the banks are somewhat steeper, and the water becomes slightly coloured. The Water Framework Directive was a Europe-wide initiative introduced in 2000 to improve the status of water bodies, but the Whitewater has not achieved good ecological status, due to the poor condition of its fish population. This is largely due to the number of weirs that have historically been associated with milling, making it difficult for fish to move upstream and fragmenting the habitat. [21] The river contains game fish, particularly brown trout, and coarse fish, including barbel, chub, dace, perch, pike, and roach. Fishing takes place along much of the river. [22]

Several sections of the river are used as trout fisheries, where the wild trout are augmented by the addition of stock from a hatchery. In 2012 the Wild Trout Trust carried out a survey of the 1.9-mile (3.1 km) section from below Hook Mill to Dipley Bridge, just above Dipley Mill, because the Whitewater Syndicate who have managed that part of the river as a fishery for 30 years were concerned that river flows seemed to be reducing, and that the growth of aquatic plants was declining. Lack of plants resulted in fewer flies, a major source of food for trout, and a general decline in the fishery. [23] The survey identified a number of factors contributing to the state of the fishery. At the downstream end, the effects of Dipley Mill are that there is a long section of deep, slow-moving water, which is not ideal for trout. There were sections where weed growth was affected by a lack of light, caused by large Alder trees growing on the banks. Trout need dappled shade, and selective coppicing of the trees would result in improved weed growth. There were areas where water was leaking through the banks, which have been raised historically to impound the water for milling. Such leakage poses a threat to the integrity of the bank, and this is exacerbated by the arrival of the non-native North American signal crayfish, which burrow into banks causing further erosion. [24]

A number of low weirs had been built across the stream bed, in an attempt to improve water levels, but had resulted in slower flows depositing fine silt behind them, reducing their effectiveness. The report recommended that some of them should be removed, and replaced with large woody debris on the verges of the channel, to create faster-flowing water and help to scour silt from the bed, resulting in better conditions for plants, invertebrates and fish such as trout that prefer faster flows. [25] Further upstream, there was evidence of water-crowfoot growing in the water. This depends on the river bed being composed of gravel, and fast flows, and is a typical chalk stream plant. It provides important habitat for upwing river flies. [26]

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. [27]

The water quality of the Whitewater was as follows in 2019.

SectionEcological StatusChemical StatusOverall StatusLengthCatchment
Whitewater [28] Poor Fail Poor 12.2 miles (19.6 km)42.37 square miles (109.7 km2)

Reasons for the quality being less than good include discharge from sewage treatment works; runoff from agricultural land; physical barriers such as weirs and impounding of the water which prevent the free migration of fish and other species; and the presence of the North American signal crayfish, an invasive species. The biological status is high for invertebrates and good for aquatic plants, but the barriers to fish movement result in the overall status being poor.

Milling

There is clear evidence for eight water mills along the course of the Whitewater. All of them were corn mills in 1883. [29] Taylor's map of 1759 shows three mills on the river, labelled Paper Mill at Wolson Bridge, Polern Mill (now Poland Mill) and Odiam Mill (now Warnborough Mill, Odiham). [30] Greenwood's 1826 map shows Riseley Mill, Holdshott Mill, Dipley Mill, Paper Mill and Poland Mill. [31]

There has been a mill on the site of Greywell Mill since at least 1600, which in 1608 was known as Cutmill or Grewell Mill. [32] The present three-storey building dates from the 18th century and a two-storey mill house is attached. [5] The river was embanked, to provide sufficient head for a wooden breastshot waterwheel. This powered two pairs of stones, mounted in a hurst frame. The mill races and sluices have survived, and some of the machinery is still in situ, but most is missing. The first known miller was Robert Hawkins who insured the brick and tiled grist mill and mill tackle for £200 in 1767. In the 1910s the wooden buckets on the wheel were replaced with iron ones, which were not particularly suitable because of their weight. The wheel was supplemented by a steam engine, located in another building. The mill stopped working in 1932 when the mechanism failed, and the owner did not repair it because fishing on the river was better when it was not working. Part of the mill pond was used for growing watercress until about 1970. [33]

When the Domesday Book was compiled in 1086, there were eight water mills listed in Odiham. Some of them were owned by Robert the Parker around 1200, from whom King John took 20 acres (8.1 ha) on which to build Odiham Castle. Robert's mills were burnt by the king, and in 1235 his rent was reduced by 20 shillings on account of the meadows he had lost to the king. During the reigns of Edward I and Edward III, one of Robert's descendants, William Parker, held a mill and half a hide of land. Warnborough Mill was destroyed by a fire in 1337–38, but was rebuilt in 1345–46. Records mention a fulling mill in North Warnborough in 1555–56, and a mill in Warnborough in 1630, but it is not clear if they were the same or different mills. [34]

The river above Castle Mill was embanked, and although the sluices survive, the mill itself burnt down in 1910, and was not rebuilt. It was described as a large fulling mill at that time, and produced woolen and worsted cloth, while weaving was carried out in the local cottages. After the fire, Sir John Humphries rebuilt most of the mill house in the 1920s, and lived at King's Mill while the work was done. He also landscaped the surrounding area. [35]

As Odiham was officially the Royal Manor of Odiham, Warnborough Mill became known as King's Mill, and was owned by Lords of the Manor until 1920, when the estate was sold. John Hooker was the miller in 1615, and Sydney Loader was the last miller to use it to grind corn in 1895. Around 1904 the machinery was removed, the building was renovated and it became a private house until the early 1990s, when it was converted into the Mill House Restaurant. As part of the conversion, the mill wheel was restored in 1995, and again in 2011. [36] There is a small 3.5-foot (1.1 m) overshot waterwheel in the garden of the restaurant, which may have once been used to generate electricity. [37]

Poland Mill was in the manor of Polling, called Pulling in the 15th century and Polands or Poleing in the 18th, and together with Poland Farm, recalls the name of the earlier manor. [34] The present building dates from the 18th century, and once had six water wheels. [14] The building has been offered for sale several times in the 2010s, when it has been called Whitewater Mill, while the mill house has been referred to as Poland Mill. A room on the ground floor retains some mill wheels, and is used as a cellar. [38]

The parish of Newnham has had two corn mills and a paper mill at various points in its history, as well as a foundry and two brickworks. The eastern boundary of the parish was once on the River Whitewater, and it is probable that one of the two mills was at Hook on the Whitewater, and the other was Lyde Mill on the River Lyde. [39] Newnham village church was served by monks from West Sherborne Priory, and this was facilitated by Henry de Port, who gave money to the priory. A charter that he made in 1130 in this context mentions tithes from two mills in the parish, [40] while in 1766, Edward Chamberlain of Paper Mill was responsible for the upkeep of four panels of the churchyard fence. At the same time, David Crimble of Lyde Mill was responsible for the upkeep of a further two panels. [41] Paper Mill was on the Whitewater below Wolson Bridge, now the Crooked Billet Bridge on the A30 road. The first known mention of a paper maker in the area was in 1749, and Edward Chamberlain was the last known paper maker, mentioned in 1816. The paper mill is marked on I. Taylor's 1759 map of Hampshire, T. Milne's map of 1791, Mudge's map of 1817 and Greenwood's map of 1826. [42] When it ceased to be used for making paper, it became a corn mill, known as Hook Mill. The present building dates from the 17th and 18th centuries, when it was still a paper mill, and together with the adjoining mill house it is now part of a private residence. [15]

Dipley Mill was a three-storey building made of red bricks with a tiled roof. It probably had four pairs of stones, and two water wheels. [43] The mill was listed in the Domesday Book, when it belonged to Alfsi son of Brictsi. During the 19th century, a second water wheel was added, but was not entirely successful, as the building shook when the wheels worked in tandem. Milling continued until 1927, when the building was converted into a country house, and the house and gardens were renovated after 2000. [44]

Heckfield had a mill when the Domesday Book was compiled in 1086. The mill and a fishery worth 100 eels a year was given to the Prior and convent of Merton by John de Port some time before 1208, and a survey of the parish in 1341 listed two mills, one at Holdshott and the other at Mattingley. When the abbey was dissolved, ownership of a fulling mill and a watermill reverted to the Lord of the Manor. Holdshott was sold to Charles Shaw-Lefevre in 1817, and the sale included four mills. The mill at Mattingley was also given to the Prior and convent of Merton in 1206, and was probably one of the two mentioned in 1341. It was situated just upstream of Mattingley Clappers Bridge, and was demolished in the late 19th century. [45]

Riseley Mill is the final mill on the river, and the present building dates from the late 18th century. [46] The first recorded miller was Francis Belcher in 1792, who insured the mill for £100 and the nearby granary for £500. The corn mill was originally powered by a wooden undershot water wheel, 10 feet (3.0 m) wide and 13 feet (4.0 m) in diameter. In 1910, the wheel was proving unreliable, but a new iron waterwheel was found to be too small when it arrived, and was never fitted. At some point an oil engine was used to power the machinery, which included four pairs of stones on a hurst frame, and another two on the second floor. During the Second World War, all of the machinery was removed and it was used as a pill-box, protected by thick brickwork around the base. It is probable that the mill was also a bakery, as a huge baker's oven was found in a shed in 1966. The mill building and mill house were sold by the Duke of Wellington's Stratfield estate in 1968, and both became private homes. A fire in the mill in 1991 severely damaged the roof, which had to be replaced. [20] [47]

Bibliography

Related Research Articles

<span class="mw-page-title-main">Basingstoke Canal</span> English canal in Hampshire and Surrey

The Basingstoke Canal is an English canal, completed in 1794, built to connect Basingstoke with the River Thames at Weybridge via the Wey Navigation.

<span class="mw-page-title-main">Hart District</span> Non-metropolitan district in England

Hart is a local government district in Hampshire, England, named after the River Hart. Its council is based in Fleet. It was formed on 1 April 1974 under the Local Government Act 1972, as a merger of the urban district of Fleet, and the Hartley Wintney Rural District. It was named the best place to live in the UK in the 2017 Halifax quality of life study.

<span class="mw-page-title-main">River Lugg</span> River in Radnorshire, Wales and Herefordshire, England

The River Lugg rises near Llangynllo in Radnorshire, Wales. It flows through the border town of Presteigne and then through Herefordshire, England, where it meets its main tributary, the River Arrow, to the south of Leominster. It flows into the River Wye downstream of Hereford at Mordiford, around 63 miles (101 km) from its source. Its name comes from a Welsh root, and means "bright stream".

<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 Blackwater (River Loddon)</span> Tributary of the River Loddon in England

The River Blackwater is a tributary of the Loddon in England and sub-tributary of the Thames. It rises at two springs in Rowhill Nature Reserve between Aldershot, Hampshire and Farnham, Surrey. It curves a course north then west to join the Loddon in Swallowfield civil parish, central Berkshire. Part of the river splits Hampshire from Surrey; a smaller part does so as to Hampshire and Berkshire.

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

The River Loddon is a tributary of the River Thames in southern England. It rises at Basingstoke in Hampshire and flows northwards for 28 miles (45 km) to meet the Thames at Wargrave in Berkshire. Together, the Loddon and its tributaries drain an area of 400 square miles (1,036 km2).

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

The River Kent is a short river in the county of Cumbria in England. It originates in hills surrounding Kentmere, and flows for around 20 miles (32 km) into the north of Morecambe Bay. The upper reaches and the western bank of the estuary are located within the boundaries of the Lake District National Park. The river flows in a generally north to south direction, passing through Kentmere, Staveley, Burneside, Kendal and Sedgwick. Near Sedgwick, the river passes through a rock gorge which produces a number of low waterfalls. This section is popular with kayakers as it offers high quality whitewater for several days after rain. The village of Arnside is situated on the east bank of the Kent estuary, just above Morecambe Bay, and a tidal bore known as the Arnside Bore forms in the estuary at this point on high spring tides.

<span class="mw-page-title-main">Basingstoke (UK Parliament constituency)</span> Parliamentary constituency in the United Kingdom, 1885 onwards

Basingstoke is a constituency in Hampshire represented in the House of Commons of the UK Parliament since 2005 by Maria Miller, a member of the Conservative Party who served as Culture Secretary and Minister for Women and Equalities from 2012 to 2014 under Prime Minister David Cameron.

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

The River Frome, once also known as the Stroudwater, is a small river in Gloucestershire, England. It is to be distinguished from another River Frome in Gloucestershire, the Bristol Frome, and the nearby River Frome, Herefordshire. The river is approximately 25 miles (40 km) long.

<span class="mw-page-title-main">Odiham Castle</span> Ruined castle in Hampshire, UK

Odiham Castle is a ruined castle situated near Odiham in Hampshire, United Kingdom.

Greywell is a small village and civil parish in Hampshire, England – a past winner of the Best Kept Village in Hampshire competition and a recent winner of Best Small Village in Hampshire. It lies on the west bank of the River Whitewater, 6 miles east of Basingstoke and 1.5 miles west of Odiham. The area is popular with walkers and cyclists. Many photographers also take pictures of some of the local architecture. There are 29 Grade II listed buildings or entries in the area, and 2 Grade II* listed buildings. The nearby medieval Odiham Castle is of historical interest. At the centre of the village is the Fox and Goose public house.

Rotherwick is a village and civil parish in the Hart district of Hampshire, England.

<span class="mw-page-title-main">South Warnborough</span> Village in Hampshire, England

South Warnborough is a small village and civil parish in the English county of Hampshire. In the 2001 census, the population was 407. In the 2016 census, the population was estimated to be 509.

North Warnborough is a village in the Hart district of Hampshire, England. It is in the civil parish of Odiham. It is located less than 2 miles (3.2 km) south of the town of Hook, on the opposite side of the M3 motorway, and just north-west of the village of Odiham. The Basingstoke Canal passes through the village, and the River Whitewater flows to the north.

<span class="mw-page-title-main">River Hart</span> Tributary of the River Whitewater in north Hampshire, England

The River Hart is a tributary of the River Whitewater in north Hampshire, England. It rises at Ashley Head spring in Crondall and flows north to meet the Whitewater at Bramshill.

<span class="mw-page-title-main">Wish Stream</span> River in Berkshire and Surrey, England

Wish Stream is a small, steep English river, which is a tributary of the River Blackwater. Mostly it demarcates Berkshire and Surrey. It rises on heath land to the north of Camberley, and descends in a south-westerly direction, passing through the grounds of the Royal Military Academy Sandhurst. Two large lakes have been made before it leaves the grounds, to pass through a culvert under a retail park and bridges under major roads to discharge into the Blackwater.

<span class="mw-page-title-main">River Lyde (Hampshire)</span> River in Hampshire, England

The River Lyde or Lyde River is a small river in the English county of Hampshire. It rises near Mapledurwell, where the water is used in watercress beds before entering the main channel. It flows in a generally northerly direction, and used to supply power to watermills along its route. Near Sherfield on Loddon it joins the River Loddon, which is a tributary of the River Thames.

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

Painswick Stream is a small river in Gloucestershire, England. It is a tributary of the River Frome, and flows generally southwards, passing around the village of Painswick and through the town of Stroud. It used to join the Frome at its mouth, but was diverted into the then-derelict Stroudwater Navigation as part of a flood relief scheme in the 1950s. Despite its small size, it has been used to power a significant number of mills, many of which were associated with cloth manufacture until the industry was hit by a series of depressions in the 1820s and 1830s. Some found other uses, being used for grinding corn and for the manufacture of walking sticks and umbrella sticks, another prominent local industry. Many were subsequently demolished, but a number survive which have been granted listed building status.

References

  1. "Blackwater valley".
  2. "Jansson's Hampshire 1646, rivers". www.geog.port.ac.uk.
  3. "Whitewater Valley Preservation Society". Archived from the original on 6 March 2019.
  4. 1 2 Low 2012.
  5. 1 2 Historic England. "Greywell Mill (1092309)". National Heritage List for England . Retrieved 2 July 2020.
  6. Historic England. "Greywell Tunnel (1339863)". National Heritage List for England . Retrieved 2 July 2020.
  7. Cumberlidge 2009, pp. 71–72.
  8. Historic England. "Odiham Castle (1092165)". National Heritage List for England . Retrieved 2 July 2020.
  9. Historic England. "Odiham Castle (1008705)". National Heritage List for England . Retrieved 2 July 2020.
  10. Ordnance Survey, 1:2500 map, 1896
  11. Historic England. "Mill House Restaurant (1339908)". National Heritage List for England . Retrieved 2 July 2020.
  12. Historic England. "Lodge Farmhouse (1092163)". National Heritage List for England . Retrieved 2 July 2020.
  13. Historic England. "Roman villa at Lodge Farm, North Warnborough (1001879)". National Heritage List for England . Retrieved 2 July 2020.
  14. 1 2 Historic England. "Poland Mill, Odiham (1244450)". National Heritage List for England . Retrieved 2 July 2020.
  15. 1 2 Historic England. "Hook Mill, Odiham (1339892)". National Heritage List for England . Retrieved 2 July 2020.
  16. Historic England. "Dipley Mill, Hartley (1339892)". National Heritage List for England . Retrieved 2 July 2020.
  17. 1 2 Ordnance Survey, 1:2500 map
  18. Historic England. "Holdshott Farm House (1258529)". National Heritage List for England . Retrieved 2 July 2020.
  19. Historic England. "Heckfield Bridge (1258496)". National Heritage List for England . Retrieved 2 July 2020.
  20. 1 2 Ellis 1968, p. 130.
  21. Thomas 2012, p. 3.
  22. "Welcome". Farnborough and District Angling Society. Archived from the original on 24 January 2019.
  23. Thomas 2012, pp. 3–4.
  24. Thomas 2012, pp. 4–6.
  25. Thomas 2012, p. 11.
  26. Thomas 2012, p. 14.
  27. "Glossary (see Biological quality element; Chemical status; and Ecological status)". Catchment Data Explorer. Environment Agency. 17 February 2016. UKOpenGovernmentLicence.svg Text was copied from this source, which is available under an Open Government Licence v3.0. © Crown copyright.
  28. "Whitewater". Catchment Data Explorer. Environment Agency.
  29. Ordnance Survey, 1:2500 map, 1883
  30. Taylor 1759, Section 75.
  31. Greenwood 1826, Section 86.
  32. Page 1911a, pp. 76–79.
  33. Vaidya 2013, pp. 62–64.
  34. 1 2 Page 1911c, pp. 87–98.
  35. Vaidya 2013, p. 65.
  36. Millard 2011.
  37. Vaidya 2013, pp. 66–67.
  38. Keel 2019.
  39. "Newnham Introduction" (PDF). Victoria County History - draft new edition. August 2019. p. 3. Archived (PDF) from the original on 2 July 2020.
  40. Bell 2004, pp. 4, 9.
  41. Bell 2004, p. 14.
  42. Shorter 1953, p. 9.
  43. Ellis 1968, p. 132.
  44. "The history of Dipley Mill". Dipley Mill. Archived from the original on 4 July 2020. Retrieved 3 July 2020.
  45. Page 1911b, pp. 44–51.
  46. "Monthly walk in October 2019". Blackwater Valley Countryside Trust. October 2019. Archived from the original on 4 July 2020.
  47. Vaidya 2013, pp. 81–83.