The River Welland is a lowland river in the east of England, some long. It drains part of the Midlands eastwards to The Wash. The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke. It is a major waterway across the part of the Fens called South Holland, and is one of the Fenland rivers which were laid out with washlands. There are two channels between widely spaced embankments with the intention that flood waters would have space in which to spread while the tide in the estuary prevented free egress.
Introduction
River Welland
River Welland | Introduction
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where does the river welland start and finish
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The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke
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what is the total length of this watercourse?
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what are some of its tributaries?
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The river flows under two navigable aqueducts: the Welland Recreational Waterway and the new alignment of the Welland Canal. An important tributary of the river is Coyle Creek, a picturesque and thickly forested creek that flows into the river on the north bank. A stream of the river branches off shortly before its mouth. This canal quickly turns an open-cut hydropower channel through the city of Niagara Falls on its way to the Sir Adam Beck Hydroelectric Generating Stations in Queenston. It drains an area of . The International Control Dam, a weir in the Niagara River, causes the Welland River to reverse its direction twice a day when the flow of water over the Niagara Falls is reduced overnight and the water heads back up the river as far back as Wellandport.
Welland River | Geography
When the water flow is restored, the water direction of the Welland River changes once again to flow towards the Niagara River.
Welland River | Geography
Wildlife in the river varies along its length, the faster headwaters being a habitat for trout and the slower lower reaches for perch. The estuary conditions and flat landscapes beyond Fosdyke favour wading birds and migratory species.
River Welland | Introduction
The River Welland is a lowland river in the east of England, some long. It drains part of the Midlands eastwards to The Wash. The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke. It is a major waterway across the part of the Fens called South Holland, and is one of the Fenland rivers which were laid out with washlands. There are two channels between widely spaced embankments with the intention that flood waters would have space in which to spread while the tide in the estuary prevented free egress.
River Welland | Introduction
The river, in its upper reaches, supports a wild brown trout population and the occasional grayling. Chub and perch dominate the middle reaches around Stamford, with pike, perch, zander, roach, bream, rudd, ruffe, gudgeon and eels inhabiting the lower lengths around Spalding. A collaboration between the Welland Rivers Trust, the Wild Trout Trust and the Environment Agency has resulted in the construction of a rock ramp, to allow migrating sea trout to pass up the river beyond the weir on the Maxey Cut, which was acting as a barrier. Some 300 tons of rock, with 50 tons of finer material forming a top layer, were used to create the ramp.
River Welland | Wildlife
The finer material ensures that water mainly flows over the ramp, rather than through it. The ramp also enables young eels or elvers to move up the river, and provides habitat for stone loach and bullheads. Large numbers of swans and geese use the river around Crowland, and out to sea. Smaller populations of each can be seen around the Stamford Meadows, and further upstream.
River Welland | Wildlife
The River Welland, with its tributaries, form a river system with a catchment area of . Within this area, of waterway are designated as "main river", and are therefore managed for flood control by the Environment Agency under the River Welland Catchment Flood Management Plan (CFMP). Of this total, the below Spalding are tidal, and have sea walls to protect the adjacent land from flooding, while are fresh water, but run through low-lying land, and are therefore embanked. Within the catchment area, are below sea level, and would be flooded without such defences. The basin runs in a broadly south-west to north-east direction, with an extension to the north around the West Glen and East Glen rivers.
River Welland | Geography
Macmillan Way, a long distance footpath, crosses on its way from Abbotsbury in Dorset to Boston, Lincolnshire. Medbourne Brook joins from the north, after which the river approaches a dismantled railway and is joined by the Stoke Albany Brook, approaching from the south. The river remains on the south side of the railway, while the county border follows a meandering course to the north of it, but rejoins the river near the Bringhurst to Cottingham road. The bridge over the river is plain, but to the north of it is an eighteenth-century causeway, some long, which is made of stone and pierced by seven large arches and numerous smaller arches for drainage pipes.
River Welland | Market Harborough to Stamford
The Welland rises in the Hothorpe Hills in the parish of Sibbertoft, Northamptonshire and it issues at Spring Croft, Church Street. Sibbertoft sits astride one of the principal watersheds in England. Within , the small stream forms the border between Northamptonshire and Leicestershire. It flows westwards, before looping round, passing through the grounds of Hothorpe Hall in Theddingworth, now a conference centre, to flow generally eastwards through Lubenham to Market Harborough. One of the driveways to Thorpe Lubenham Hall is carried over the river by an early nineteenth century ashlar bridge which is a Grade II listed structure. To the east of Lubenham, the river passes Old Lubenham Hall, part of an H-plan house built in the late sixteenth century and modified in the early eighteenth century.
River Welland | Course
The underlying geology consists of Lias clays at the western end of the catchment, with Lincolnshire limestone in the centre, including the valleys of the Glen. The eastern third is mostly alluvial soils, and it is this part that relies on artificial pumping to prevent flooding. Rainfall over the area varies between per year, which is quite light, and because the land is efficiently drained during the winter months, there are few reserves, making the area prone to drought in the summer months. For much of its length the Welland forms the county boundary between Northamptonshire and Leicestershire or Rutland, and lower down between Lincolnshire and Cambridgeshire.
River Welland | Geography
The Welland River (originally called the Chippawa Creek) is a river in the Golden Horseshoe that passes through the Southern Ontario cities of Welland and Niagara Falls. It flows from its source just south of Hamilton, Ontario to meet the Niagara River.
Welland River | Introduction
The area of the headwaters of the Tweed would have been frequented by wild boar in Anglo-Saxon times. The other example of wella in the watershed is "Twitchell". Brook Farm, west of Stoke Golding takes its name from the unnamed stream running north towards the Tweed at the foot of Ambion Hill.
River Sence | Names related to the watercourses
The source of the River Welland is in the parish and it issues as a spring at Spring Croft, Church Street. Sibbertoft sits astride one of the principal watersheds in England and the plateau of land towards Naseby contains the sources of four rivers flowing west, south and east. Coombe Hill Hollow, north of the village, is a Site of Special Scientific Interest.
Sibbertoft | Geography
King Charles I is believed to have stayed there before the Battle of Naseby. Three arms of a square moat surround the house, and the site is a scheduled ancient monument.
River Welland | Course
The following rivers are tributaries to the river Tecșe (from source to mouth):
Tecșe | Tributaries
This first lists the tributaries of the River Thames from the sea to the source, in England. The secondary lists are of backwaters of the river itself and the waterways branching off. Note: the River Medway shares the saline lower Thames Estuary.
Tributaries of the River Thames | Introduction
Vernatt's Drain passes through a sluice to join the river, while the sluice that protects the entrance to the River Glen is navigable, to allow boats to reach Tongue End, some upstream from its mouth. There are pumping stations for Sea Dike and Lords Drain, and the outfalls of the Risegate Eau and Five Towns drainage channels before the final bridge at Fosdyke is reached. After it is joined by the Holbeach River, it is bordered by salt marshes, and finally flows into The Wash at "The Cots" in "Fosdyke Wash". Beyond the river banks, much of the fertile arable land is composed of marine silt, which suits the bulb-growing for which Spalding is famous.
River Welland | Spalding to the Wash
The Partnach has the following tributaries which join it at or near the river kilometre shown in brackets:
Partnach | Tributaries
The following rivers are tributaries to the river Nechit (from source to mouth):
Nechit | Tributaries
Among the medieval forms of the name 'Welland' is Weolod; the river could have thus been named from its silty nature. In contrast, the Glen flowed from clays and limestone. Areas with clay-based soils tended to remain as woodland whilst the limestone areas provided grassland for pasture. Consequently, the River Glen did not carry much sediment. The modern Welsh for clean is "glân". The relative amounts of silt deposited in the fens around Maxey and around Thurlby respectively, by the two rivers, support this view.
River Glen, Lincolnshire | Naming
The river is bounded on the north and west by a bank, while the New River, a drainage channel to the south and east of it, is bounded by another bank. The land between the channels forms Crowland High Wash, Crowland Fodder Lots and Cowbit Wash. The southern bank is variously named Corporation Bank, Wash Bank and Barrier Bank. These wash lands were designed to be flooded "in extremis", although the building of the Coronation flood relief channel has made this purpose obsolete.
River Welland | Stamford to Spalding
The River Gwash, a tributary of the River Welland, flows through the English counties of Leicestershire, Rutland and Lincolnshire. It rises just outside the village of Knossington in Leicestershire, near the western edge of Rutland. It is about long.
River Gwash | Introduction
This confluence is located at:
Weller River | Geography
"The length of each tributary is given in parentheses:"
Poronay | List of tributaries
The Wells River is a tributary of the Connecticut River, approximately long, in the U.S. state of Vermont. The Wells River begins at the outlet of Ricker Pond at the southern boundary of Groton State Forest in the town of Groton. The river flows generally southeast through the towns of Ryegate and Newbury, reaching the Connecticut River at the village of Wells River. U.S. Route 302 follows the river for most of its length.
Wells River (Vermont) | Introduction
The following rivers are tributaries to the river Wetter (from source to mouth):
Wetter (river) | Tributaries
Its source is a spring called "Boiling Well" on the dissected plateau of the Long Mynd, adjacent to a number of Long barrows. From this point it flows south east through the V shaped valley known as Ashes Hollow, to reach the village of Little Stretton. After passing through Little Stretton, the watercourse heads south towards Marshbrook and Strefford. To the north of Strefford, it is joined by its main tributary the Byne Brook. The now larger brook is forded at Strefford from where it flows south-westerly to The Grove and Berrymill cottage, south of Wistanstow, where it joins the River Onny.
Quinny Brook | Course
The Wellow Brook is a small river in Somerset, England. It rises near Ston Easton Park in the village of Ston Easton and flows east to Midsomer Norton. West of Radstock, it is joined by the River Somer and a tributary from Kilmersdon (formed itself from Snails Brook and Kilmersdon Brook) to the south. It then flows through Wellow before joining the Cam Brook at Midford to form Midford Brook, before joining the River Avon close to the Dundas Aqueduct. The Environment Agency does not recognise the Midford Brook, instead identifying the Wellow Brook as continuing to the Avon. On this basis the length of the Wellow Brook, from Radstock to the Avon, is .
Wellow Brook | Introduction
At that time it was known as the Wellstream or Old Wellenhee, and parts of that course are marked by the Old Croft River and the border between Cambridgeshire and Norfolk. After major inland flood events in the early 13th century it breached another watershed near Denver and took over the channel of the old Wiggenhall Eau, and so achieved a new exit and so joined the Wash at Kings Lynn. Parts of the old course were later used for the River Lark, which flows in the reverse direction along the section below Prickwillow, after the main river was moved further to the west.
River Great Ouse | History: drainage and navigation
This list shows those tributaries that are over 3.0 km long, together with the direction and location of their confluence. They are listed in order from source to mouth. For the full list of tributaries with additional data, see .
Brigach | Tributaries
The River Spodden falls 235 metres in its length of 12 kilometres, and is fed by nine direct tributary brooks and a further four indirect brooks.
River Spodden | Source and course
The availability of a suitable geological feature on which to build this bank determined the shape of the washes, and its location can be traced back through antiquity. To quote Wheeler: The right bank of the Welland between Crowland and Spalding is placed at a distance from the channel of the river varying from a quarter to half a mile leaving an area of about 2500 acres which is covered with water whenever the Welland is in flood. The depth of water in this land in high floods is as much as 5 feet. Originally, no doubt, the land by the side of the Wellland was little better than a Morass, and the banks were placed on the nearest firm ground.
New River (Fens) | Introduction
These meanders were flooded by means of a dam at Port Dalhousie, Ontario to create Martindale Pond. Further upstream, the first canal generally followed the bends in the creek, but most were straightened for the second canal resulting in the lower creek now being almost straight.
Twelve Mile Creek (Ontario) | The early Welland Canal
The following rivers are tributaries to the river Adige (from source to mouth):
Adige | Tributaries
The following rivers are tributaries to the river Sălaj:
Sălaj (river) | Tributaries
Notable tributaries include River Loud, Trough Brook, and River Dunsop.
River Hodder | Tributaries
Several of the tributary brooks in that valley also flow subterraneously for some parts of their course.
Hönne | Introduction
The causeway has two large semi-circular passing places on its western side. The Welland passes to the north of Corby near Rockingham, and then to the south of Caldecott, where it becomes the county border between Northamptonshire and Rutland, and the Eye Brook, which has been dammed to form the Eyebrook Reservoir, joins from the north. As it flows past Harringworth, the river forms two channels, with the county border following the smaller, northern channel. It is crossed by the Welland Viaduct, with its 82 brick arches, which was completed in 1879, and carries the Oakham to Kettering Line over the valley.
River Welland | Market Harborough to Stamford
Its tributary is the River Cray.
Rivers of Kent | River Darent
During the 1960s and 1970s, several sections of the river above Stamford were made straighter and deeper, to reduce the risk of flooding of agricultural land. To address the habitat and environmental issues causes by such engineering work, the Welland Rivers Trust, a limited company and charitable trust, was set up in 2010. They are seeking to direct regeneration of the river by co-ordinating various organisations, which are known collectively as the Welland Valley Partnership. They published a major document outlining their proposals in February 2013.
River Welland | The Outfall
Alphabetical listing of tributaries, extracted from the Water Framework Directive list of water bodies for the River Trent:
River Trent | List of tributaries
The following rivers are tributaries to the river Cracău (from source to mouth):
Cracău | Tributaries
Beyond Stamford, the river passes the site and ruins of the Benedictine St Leonard's Priory. Hudd's Mill marks the point at which the Stamford Canal left the river. The present mill building dates from 1751 and 1771. The River Gwash, which the canal crossed on the level, joins from the north, and the remains of the canal follow the river on its north bank. Below Uffington, the county border follows the old course of the river, first to the south to Tallington and then to the north, while the main course now flows along the Maxey Cut to Peakirk. The old course consists of two streams, fed by sluices from the Maxey Cut, which meander to The Deepings.
River Welland | Stamford to Spalding
Along its short course, a few smaller streams join the river.
Cadoxton River | Tributaries
The following rivers are tributaries of the Wipper:
Wipper (Saale) | Tributaries
The following rivers are tributaries to the river Cigher:
Cigher | Tributaries
The eastern stream supplied power to Lolham and Maxey mills, while the western stream did the same for Tallington Mill, which dates from around 1700, West Deeping mill, and Molecey's mill, which still retains its seventeenth-century undershot waterwheel, modified in the 19th century to Poncelet's improved design, and the only surviving waterwheel of its type in Lincolnshire. At the western edge of Market Deeping the two streams join, and they are also joined by the Greatford Cut, which has carried the diverted waters of the West Glen river since the early 1950s. This section is crossed by King Street, which follows the course of a Roman road.
River Welland | Stamford to Spalding
The following rivers are tributaries to the river Olteț (from source to mouth):
Olteț | Tributaries
The following rivers are tributaries to the river Cricovul Sărat (from source to mouth):
Cricovul Sărat | Tributaries
The following rivers are tributaries to the river Ier:
Ier | Tributaries
The Serein has the following tributaries over 10 km length: "note: R=Right L=Left"
Serein | Main tributaries of the Serein and their length
The river holds a variety of fish species, including roach, dace and chubb. White-clawed crayfish are known to be in the river, which puts them at risk, as invasive species of crayfish are known to be in the Welland.
River Chater | Wildlife
The river has a total length of and a catchment size of . The Avon's tributaries include the Rivers Leam, Stour, Sowe, Dene, Arrow, Swift, Isbourne and Swilgate as well as many minor streams and brooks. A long distance footpath has been created which follows the river from its source to the River Severn at Tewkesbury. The route is marketed as Shakespeare's Avon Way, and is long. It uses existing footpaths and tracks to stay as close to the river as is reasonably possible.
River Avon, Warwickshire | Course
The Janon's other tributaries are the Combe Noire and Langonand.
Janon | Course
The following rivers are tributaries to the river Săsar:
Săsar | Tributaries
The river was originally called the Chippawa Creek since it drained into the Niagara River at Chippawa. Like many other places in Niagara, it was renamed by John Graves Simcoe, the first lieutenant governor of Upper Canada in 1792. The present name was taken from the river of the same name in Lincolnshire, Eastern England. The Welland River is occasionally referred to as Chippawa Creek, especially by those in the Chippawa area itself. The Welland Canal was named after the river since it originally was planned to link Lake Ontario to Welland River. The city of Welland was later named after both waterways which crossed in the city.
Welland River | History
The following rivers are tributaries to the river Teleajen (from source to mouth):
Teleajen | Tributaries
The following rivers are tributaries to the river Argeș (from source to mouth):
Argeș (river) | Tributaries
Main tributaries from source to mouth: "N.B. : (R) = right tributary; (L) = left tributary"
Dordogne (river) | Tributaries
The following rivers are tributaries to the river Orăștie (from source to mouth):
Orăștie (river) | Tributaries
The following rivers are tributaries to the Ampoi (from source to mouth):
Ampoi | Tributaries
The river is about 21 miles (34 km long), rising at a height of about 920 feet (280m) on Bodmin Moor and flowing into the Tamar Estuary near Plymouth. It has four main tributaries, the largest of which is the River Tiddy. The smaller tributaries include Deans Brook, Withey Brook, Marke Valley and Darleyford streams and Kelly Brook.
River Lynher | Geography
A limestone ashlar bridge with four arches crosses the river, dating from the fifteenth century but widened in 1919. After the river passes under a railway bridge at Ketton, its flow is swelled by the River Chater. The county border again leaves the river to the west of Stamford while below the town the river forms the border between Lincolnshire and Cambridgeshire.
River Welland | Market Harborough to Stamford
The following rivers are tributaries to the river Nidda (from source to mouth):
Nidda (river) | Tributaries
The following rivers are tributaries to the river Berheci:
Berheci | Tributaries
The following illustration depicts the profile of the Welland Canal. The horizontal axis is the length of the canal. The vertical axis is the elevation of the canal segments above mean sea level.
Welland Canal | Profile
Its major watercourses are the rivers Aln, Till, Coquet, Fallowlees Burn, Font and Rede.
Northumberland Sandstone Hills | Introduction
The following rivers are tributaries to the river Someș:
Someș | Tributaries
The Gauley's largest tributaries all flow into the main river from the east (flowing in a westerly direction) and are described as follows:
Gauley River | Tributaries
Passing through Spalding, where most of the flow is diverted through the Coronation channel, the town is protected by Marsh Road sluice and a sea lock to the east. Below the town, it is approached by Vernatt's Drain, which runs parallel to the river carrying water pumped from Deeping Fen, and is crossed by the A16 road bridge. Nearby is Pinchbeck Marsh Pumping Station, which houses the last beam engine and scoop wheel to be used in the Fens for land drainage. It was built in 1833, and ran until 1952, when it was replaced by electric pumps. It now forms part of a museum of land drainage run by the Welland and Deepings Internal Drainage Board, in partnership with South Holland District Council.
River Welland | Spalding to the Wash
List of places along the river. List of tributaries
River Nore | Course
As figures of the discharge, /s are given
River Ythan | Introduction
This list comprises the principal instances; longest ex-mill races (leats), with own articles are included; the main weirstream/river stream of each Thames lock is omitted and the smallest such associated instances but the Sheepwash Channel is included for its importance in Oxford.
Tributaries of the River Thames | Backwaters and cuts
The following rivers are tributaries to the river Baraolt:
Baraolt (river) | Tributaries
The following rivers are tributaries to the river Vâlsan (from source to mouth):
Vâlsan | Tributaries
The following rivers are tributaries to the river Šušvė (from source to mouth):
Šušvė | Tributaries
The following rivers are tributaries to the river Hășdate (from source to mouth):
Hășdate (river) | Tributaries
The main tributaries of the Adour are, from source to mouth:
Adour | Tributaries
This is a list of tributaries of the River Tees from its source at Teeshead to its mouth at Middlesbrough.
List of tributaries of the River Tees | Introduction
The headwaters of the river rise below Three Wells near Broomehill. The river flows in a south-westerly direction parallel with the Great Southern Highway as far as Tambellup then veers westward and crosses the Albany Highway north of Cranbrook and discharges into the Frankland River of which it is a tributary. The river flows through a number of pools during its journey including; Balbalingup Pool, Ballingup Pool, Boyacup Pool and Poolyup Pool. The river has four tributaries; Wadjekanup River, Cowenup Brook, Slab Hut Gully and Uannup Brook.
Gordon River (Western Australia) | Location and features
The topography, geology and land use of the Trent catchment all have a direct influence on the hydrology of the river. The variation in these factors is also reflected in the contrasting runoff characteristics and subsequent inflows of the principal tributaries. The largest of these is the River Tame, which contributes nearly a quarter of the total flow for the Trent, with the other significant tributaries being the Derwent at 18%, Soar 17%, the Dove 13%, and the Sow 8%. Four of these main tributaries, including the Dove and Derwent which drain the upland Peak District, all join within the middle reaches, giving rise to a comparatively energetic river system for the UK.
River Trent | Hydrology
The following rivers are tributaries to the river Bahlueț (from source to mouth):
Bahlueț | Tributaries
The following rivers are tributaries to the river Vaser:
Vaser | Tributaries
The following is a list of rivers in the Marlborough Region:
List of rivers of the Marlborough Region | Introduction
Portions of the Welland Canal pass through Thorold.
Thorold | Welland Canal
He sold one-third of the land to finance the project, and began work in 1730. Cowbit sluice on the Welland had six wide gates which were operated by chains connected to a treadwheel. At high tide, water was penned in Cowbit Wash, between banks which were set well back from the main channel. The bed of the river below the sluice was loosened by dragging wooden rollers with iron spikes over it. At low tide, the sluice gates were opened, and the flow scoured out the silt for some downstream. A navigation lock was constructed beside the sluice, so that vessels could still gain access to the river above.
River Welland | Deeping Fen
The following rivers are tributaries to the river Wupper (from source to mouth):
Wupper | Tributaries
Since the Broadback River flows relatively close to the northern edge of its basin, most of its major tributaries are left tributaries. Major tributaries in downstream order include: Tributaries above Lake Evans: Tributaries below Lake Evans:
Broadback River | Tributaries
The origin of the name for the river is unknown but appears to be Pre-English. In Old English the form was "Weolud" and may have changed to the Middle English form due to folk-etymology or Scandinavian influence. The Welland ("Weolud") is first mentioned in the "Anglo-Saxon Chronicle" for 921 AD. Richard de Rulos, who was Lord of Deeping Fen during the reign of William the Conqueror erected a strong embankment to prevent flooding of the meadows adjoining the river, which then became fertile fields and a pleasure garden. During the reign of Henry III (1207–1272), complaints were made that of the two channels below Crowland, the one to Spalding was more favourable to the passage of barges, but the Abbot of Crowland had obstructed and narrowed its course by planting willow trees.
River Welland | History
The following rivers are tributaries to the river Niraj (from source to mouth):
Niraj | Tributaries
Various tributaries feed into the River Darent. They also powered a number of watermills.
River Darent | Tributaries
Other tributaries include the Nant Wtre-wen, Crygnant, Nant y Llyn Mawr and Dolgar Brook. It is bridged and forded at numerous points, one of which is an aqueduct carrying the Montgomery Canal over it at Berriew. At the eastern end of the river is Glansevern Hall and gardens.
River Rhiw | Introduction
The following rivers are tributaries to the river Lotrioara (from source to mouth):
Lotrioara | Tributaries
The following rivers are tributaries to the river Vasilat (from source to mouth):
Vasilat | Tributaries
Another pair of early nineteenth-century bridges, built of coursed limestone with ashlar dressings, carry the road over the northernmost channel. The bridge at Deeping Gate carries the date 1651, and is a Grade II* listed stone structure with three round arches. After the remains of Deeping High lock and Deeping Low lock, there is a junction where the old course, the Maxey Cut, the South Drain and the Folly River, also a drain, meet. The river is officially navigable below this point. Through Crowland and Cowbit to the edge of Spalding, the river is laid out with washlands, which were historically used as pasture, because the river was allowed to flood the land when tidal levels prevented the water discharging into the sea.
River Welland | Stamford to Spalding
“The Brook” is a tributary to the River Test.
Over Wallop | Introduction
The following rivers are tributaries to the river Jagst (from source to mouth):
Jagst | Tributaries
The following rivers are tributaries of the Vedea (from source to mouth):
Vedea | Tributaries
Its tributaries are stormwater drains, including the Banyule.
Delacombe, Victoria | Introduction
This is a list of rivers longer than that flow into the Durance. They are listed in order of the confluence, starting upstream.
Durance | Summary of tributaries