River Wye (Afon Gwy)
River
The Wye at Hay-on-Wye
Country	United Kingdom
Parts	Wales, England
Tributaries
- left	River Lugg, Bachawy, Afon Edw, more
- right	River Trothy, River Monnow, Dulas Brook, more
Source
- location	Plynlimon
- elevation	690 m (2,264 ft)
- coordinates	52°28′5.170″N 3°45′56.282″W / 52.4681028°N 3.76563389°W / 52.4681028; -3.76563389
Mouth
- location	Chepstow, Severn Estuary
- elevation	0 m (0 ft)
- coordinates	51°36′36.086″N 2°39′42.423″W / 51.61002389°N 2.66178417°W / 51.61002389; -2.66178417
Length	215 km (134 mi)
Basin	4,136 km2 (1,597 sq mi)

The Wye at Chepstow, showing the castle and the road bridge linking Monmouthshire (on the left) with Gloucestershire

The River Wye (Welsh: Afon Gwy) is the fifth-longest river in the UK and for parts of its length forms part of the border between England and Wales. It is important for nature conservation and recreation.

Etymology[link]

The Roman name for the River Wye was the "Vaga", which stems from vagus meaning to roam (vagor) or the wanderer.^{[citation needed]} The Tithe map references a Vagas Field in both Whitchurch and Chepstow. ^[1]. The modern Welsh name "Gwy" may have entitled from the old Welsh "Gwybiol" or "Gwyr" (crooked wandering hills). ^[2]

Description[link]

The source of the Wye is in the Welsh mountains at Plynlimon. It flows through or past several towns and villages including Rhayader, Builth Wells, Hay-on-Wye, Hereford (the only city on the River Wye), Ross-on-Wye, Symonds Yat, Monmouth and Tintern, meeting the Severn estuary just below Chepstow. The total length is 215 km.^[3]

The Wye itself is a Site of Special Scientific Interest, a Special Area of Conservation and one of the most important rivers in the UK for nature conservation. Much of the lower valley is an Area of Outstanding Natural Beauty. The Wye is largely unpolluted and used to be considered^{[by whom?]} one of the best rivers for salmon fishing in the United Kingdom, outside of Scotland. However, in recent years the runs of salmon in the Wye have declined dramatically and according to the Environment Agency rod catch returns for 2009 it is not even the most productive salmon river in Wales, as more salmon were caught from the Welsh Dee. In England the Tyne, Ribble, Wear, Lune and Eden all had larger catches in 2009. In 1967 the Wye rod catch was 7,864; as recently as 1988 it was 6,401 but by 2002 it was only 357, a low from which it is recovering only very slowly despite the extensive habitat improvement work carried out by the Wye and Usk Foundation that was set up to restore the spring salmon runs. The Wye was particularly famous for its large "spring" salmon that had spent three or more years at sea before returning to spawn. They used to enter the river between January and June and sometimes reached weights of over 50 lbs, the largest recorded being 59 lbs 8oz landed after a long fight by Miss Doreen Davey from the Cowpond Pool at Ballingham on 13 March 1923. The last recorded 50 lb rod-caught salmon from the Wye was taken in 1963 by Donald Parrish and weighed 51 lbs 8oz. These large spring salmon have virtually disappeared over the past two or three decades.

It is also a popular river with canoeists due to the relatively slow-flowing water, making it good for beginners. The Symonds Yat Rapids are more challenging. There is a public right of navigation downstream from Hay. Walkers can enjoy the Wye Valley Walk which follows the route of the River Wye from Coed Hafren to Chepstow along a series of well-maintained way-marked paths.

A viewpoint near The Biblins on the Wye is known as 'Three Counties View', the meeting place of the counties of Herefordshire, Gloucestershire and Monmouthshire. The lower 16 miles (26 km) of the river from Redbrook to Chepstow forms the border between England and Wales.

Tributaries[link]

The Wye's tributaries include the rivers Lugg and Arrow, Elan, Dulas, Irfon, Marteg, Monnow, Trothy, Ithon, Llynfi, Letton Lake, Tarennig (the Wye's first tributary) and Bidno.

This list is incomplete; you can help by expanding it.

History[link]

The river between Tintern and Chepstow

The Romans constructed a bridge of wood and stone just upstream of present day Chepstow. The River Wye was and still is navigable up to Monmouth at least since the early 14th century. It was improved from there to a short distance below Hereford by Sir William Sandys in the early 1660s with locks to enable vessels to pass weirs. According to Herefordshire Council Archaeology, these were flash locks.^[4] The work proved to be insufficiently substantial and in 1696 a further Act of Parliament authorised the County of Hereford to buy up and demolish the mills on the Wye and Lugg. All locks and weirs were removed, except that at New Weir Forge below Goodrich, which survived until about 1815. This was paid for by a tax on the County. Weirs were removed all along the Wye in Herefordshire, making the river passable to the western boundary, and beyond it at least to Hay on Wye. A horse towing path was added in 1808, but only up to Hereford; previously, as on the River Severn, barges were man-hauled. Money was spent several times improving the River Lugg from Leominster to its confluence with the Wye at Mordiford, but its navigation is likely to have been difficult. The Wye remained commercially navigable until the 1850s, when commercial traffic moved to railways. It is still used by pleasure craft.

Kayaking near Hay on Wye

Water transport at Symonds Yat

Navigation and sport[link]

The Environment Agency is the navigation authority for the river. The Normal Tidal Limit (NTL) of the river is Bigsweir and navigation below this point is under the control of the Gloucester Harbour Trustees as Competent Harbour Authority.

The River Wye provides for canoeing and kayaking as it has sections suitable for all ranges of skills and free access all the way downstream from Glasbury through Hay-on-Wye to Hereford and the Severn Estuary.^[5]

There are a wide range of canoe hire and supervised trips, as well as campsites at key points on the river. Symonds Yat has a particularly popular series of rapids that was purchased by the British Canoe Union in 2003 to preserve the rapids for recreational use.^[6]

There are three rowing clubs on the river at Hereford, Ross-on-Wye and Monmouth. Annual regattas are held at Ross-on-Wye and Monmouth for rowers and scullers of all abilities, next to the local rowing club.

Cultural references[link]

The Romantic poet William Wordsworth includes an apostrophe to the Wye in his famous poem "Lines Written a Few Miles Above Tintern Abbey" published 1798 in Lyrical Ballads

How oft, in spirit, have I turned to thee,

O sylvan Wye! thou wanderer thro' the woods,

How often has my spirit turned to thee!

Views of the river[link]

• 

  Ross-on-Wye, Herefordshire

• 

  Chepstow

• 

  St Peter's Church, Dixton

• 

  Landscape with View on the River Wye by Thomas Jones

• 

  Eagle's Nest, Symonds Yat

Bridges on the river[link]

• 

  The old railway bridge at Redbrook

• 

  Monmouth viaduct and Duke of Beaufort Bridge at Monmouth

• 

  Chepstow Castle and bridge

• 

  Brockweir Bridge

• 

  Biblins Bridge

• 

  Wye Bridge, Monmouth

• 

  Wilton Bridge, Ross on Wye

• 

  Chepstow Bridge at very high tide

• 

  Victoria Bridge, Hereford

• 

  River Wye estuary and M48 Wye road bridge

See also[link]

Wikimedia Commons has media related to: River Wye

• Wye Valley
• Wye Valley Walk
• Wye Valley Railway
• List of rivers of England
• List of rivers of Wales
• List of bridges in Wales

References[link]

Further reading[link]

• I. Cohen, 'The non-tidal Wye and its navigation' Trans. Woolhope Nat. Fld. Club 34 (1955), 83-101;
• V. Stockinger, The Rivers Wye and Lugg Navigation: a documentary history 1555-1951 (Logaston Press 1996);
• P. King, 'The river Teme and other Midlands River Navigations' Journal of Railway and Canal Historical Society 35(50 (July 2006), 350-1.
•  Chisholm, Hugh, ed. (1911). "Wye". Encyclopædia Britannica (11th ed.). Cambridge University Press. 

External links[link]

• The River Wye described from Source to Sea

v t e Transport in Monmouthshire Road M4 motorway European route E30 M48 motorway A40 road A449 road A465 road A472 road A4042 road A4136 road Bus Stagecoach Wales National Cycle Network Celtic Trail National Cycle Route 4 National Cycle Route 47 National Cycle Route 42 Railway lines South Wales Main Line Gloucester to Newport Line Welsh Marches Line Railway stations Abergavenny Caldicot Chepstow Pontypool and New Inn Severn Tunnel Junction Waterways Monmouthshire & Brecon Canal River Wye

A river is a natural watercourse,^[1] usually freshwater, flowing towards an ocean, a lake, a sea, or another river. In a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. Small rivers may also be called by several other names, including stream, creek, brook, rivulet, tributary and rill. There are no official definitions for generic terms, such as river, as applied to geographic features,^[2] although in some countries or communities a stream may be defined by its size. Many names for small rivers are specific to geographic location; one example is "burn" in Scotland and northeast England. Sometimes a river is said to be larger than a creek,^[3] but this is not always the case, because of vagueness in the language.^[4]

Rivers are part of the hydrological cycle. Water within a river is generally collected from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, and the release of stored water in natural ice and snowpacks (e.g., from glaciers). Potamology is the scientific study of rivers.

Topography[link]

Melting toe of Athabasca Glacier, Jasper National Park, Alberta, Canada.

The water in a river is usually confined to a channel, made up of a stream bed between banks. In larger rivers there is also a wider floodplain shaped by flood-waters over-topping the channel. Flood plains may be very wide in relation to the size of the river channel. This distinction between river channel and floodplain can be blurred especially in urban areas where the floodplain of a river channel can become greatly developed by housing and industry.

The term upriver refers to the direction leading to the source of the river, which is against the direction of flow. Likewise, the term downriver describes the direction towards the mouth of the river, in which the current flows

The river channel typically contains a single stream of water, but some rivers flow as several interconnecting streams of water, producing a braided river. Extensive braided rivers are now found in only a few regions worldwide, such as the South Island of New Zealand. They also occur on peneplains and some of the larger river deltas. Anastamosing rivers are similar to braided rivers and are also quite rare. They have multiple sinuous channels carrying large volumes of sediment.

The River Cam from the Green Dragon Bridge, Cambridge UK

Nile River delta, as seen from Earth orbit. The Nile is an example of a wave-dominated delta that has the classic Greek letter delta (Δ) shape after which river deltas were named.

A river flowing in its channel is a source of energy which acts on the river channel to change its shape and form. In 1757, the German hydrologist Albert Brahms empirically observed that the submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed.^[5] (This formulation is also sometimes called Airy's law.^[6]) Thus, if the speed of flow were doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. In U-shaped glaciated valleys, the subsequent river valley can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where the river may flow over flatter land, meanders may form through erosion of the river banks and deposition on the inside of bends. Sometimes the river will cut off a loop, shortening the channel and forming an oxbow lake or billabong. Rivers that carry large amounts of sediment may develop conspicuous deltas at their mouths, if conditions permit. Rivers whose mouths are in saline tidal waters may form estuaries.

Throughout the course of the river, the total volume of water transported downstream will often be a combination of the free water flow together with a substantial contribution flowing through sub-surface rocks and gravels that underlie the river and its floodplain (called the hyporheic zone). For many rivers in large valleys, this unseen component of flow may greatly exceed the visible flow.

Subsurface streams[link]

Most but not all rivers flow on the surface. Subterranean rivers flow underground in caves or caverns. Such rivers are frequently found in regions with limestone geologic formations. Subglacial streams are the braided rivers that flow at the beds of glaciers and ice sheets, permitting meltwater to be discharged at the front of the glacier. Because of the gradient in pressure due to the overlying weight of the glacier, such streams can even flow uphill.

Permanence of flow[link]

An intermittent river (or ephemeral river) only flows occasionally and can be dry for several years at a time. These rivers are found in regions with limited or highly variable rainfall, or can occur because of geologic conditions such as having a highly permeable river bed. Some ephemeral rivers flow during the summer months but not in the winter. Such rivers are typically fed from chalk aquifers which recharge from winter rainfall. In the UK these rivers are called Bournes and give their name to place such as Bournemouth and Eastbourne.

Classification[link]

Rivers have been classified by many criteria including their topography, their biotic status, their relevance to white water rafting or canoeing activities.

Topographical classification[link]

Rivers can generally be classified as either alluvial, bedrock, or some mix of the two. Alluvial rivers have channels and floodplains that are self-formed in unconsolidated or weakly consolidated sediments. They erode their banks and deposit material on bars and their floodplains. Bedrock rivers form when the river downcuts through the modern sediments and into the underlying bedrock. This occurs in regions that have experienced some kind of uplift (thereby steepening river gradients) or in which a particular hard lithology causes a river to have a steepened reach that has not been covered in modern alluvium. Bedrock rivers very often contain alluvium on their beds; this material is important in eroding and sculpting the channel. Rivers that go through patches of bedrock and patches of deep alluvial cover are classified as mixed bedrock-alluvial.

Alluvial rivers can be further classified by their channel pattern as meandering, braided, wandering, anastomose, or straight. The morphology of an alluvial river reach is controlled by a combination of sediment supply, substrate composition, discharge, vegetation, and bed aggradation.

At the turn of the 20th century William Morris Davis devised the "cycle of erosion" method of classifying rivers based on their "age". Although Davis's system is still found in many books today, after the 1950s and 1960s it became increasingly criticized and rejected by geomorphologists. His scheme did not produce testable hypotheses and was therefore deemed non-scientific.^[7] Examples of Davis's river "ages" include:

• Youthful river: A river with a steep gradient that has very few tributaries and flows quickly. Its channels erode deeper rather than wider. Examples include the Brazos, Trinity and Ebro rivers.

• Mature river: A river with a gradient that is less steep than those of youthful rivers and flows more slowly. A mature river is fed by many tributaries and has more discharge than a youthful river. Its channels erode wider rather than deeper. Examples include the Mississippi, Saint Lawrence, Danube, Ohio, Thames and Paraná rivers.

• Old river: A river with a low gradient and low erosive energy. Old rivers are characterized by flood plains. Examples include the Yellow, Ganges, Tigris, Euphrates, Indus and Nile rivers.

• Rejuvenated river: A river with a gradient that is raised by tectonic uplift.

The way in which a river's characteristics vary between the upper course and lower course of a river are summarized by the Bradshaw model. Power-law relationships between channel slope, depth, and width are given as a function of discharge by "river regime".

Biotic classification[link]

There are very many systems of classification based on biotic conditions typically assigning classes from the most oligotrophic or unpolluted through to the most eutrophic or polluted.^[8] Other systems are based on a whole eco-system approach such as developed by the New Zealand Ministry for the Environment.^[9] In Europe, the requirements of the Water Framework Directive has led to the development of a wide range of classification methods including classifications based on fishery status^[10] A system of river zonation used in francophone communities^[11][12] divides rivers into three primary zones:

• The crenon is the uppermost zone at the source of the river. It is further divided into the eucrenon (spring or boil zone) and the hypocrenon (brook or headstream zone). These areas are characterized by low temperatures, reduced oxygen content and slow moving water.
• The rhithron is the upstream portion of the river that follows the crenon. It is characterized by relatively cool temperatures, high oxygen levels, and fast, turbulent flow.
• The potamon is the remaining downstream stretch of river. It is characterized by warmer temperatures, lower oxygen levels, slow flow and sandier bottoms.

Whitewater classification[link]

The International Scale of River Difficulty is used to rate the challenges of navigation—particularly those with rapids. Class I is the easiest and Class VI is the hardest.

Stream order classification[link]

The Strahler Stream Order ranks rivers based on the connectivity and hierarchy of contributing tributaries. Headwaters are first order while the Amazon River is twelfth order. Approximately 80% of the rivers and streams in the world are of the first and second order.

Uses[link]

Leisure activities on the River Avon at Avon Valley Country Park, Keynsham, United Kingdom. A boat giving trips to the public passes a moored private boat.

Rivers have been used as a source of water, for obtaining food, for transport, as a defensive measure, as a source of hydropower to drive machinery, for bathing, and as a means of disposing of waste.

Rivers have been used for navigation for thousands of years. The earliest evidence of navigation is found in the Indus Valley Civilization, which existed in northwestern Pakistan around 3300 BC.^[13] Riverine navigation provides a cheap means of transport, and is still used extensively on most major rivers of the world like the Amazon, the Ganges, the Nile, the Mississippi, and the Indus. Since river boats are often not regulated, they contribute a large amount to global greenhouse gas emissions, and to local cancer due to inhaling of particulates emitted by the transports.^[14][15]

In some heavily forested regions such as Scandinavia and Canada, lumberjacks use the river to float felled trees downstream to lumber camps for further processing, saving much effort and cost by transporting the huge heavy logs by natural means.

Rivers have been a source of food since pre-history.^[16] They can provide a rich source of fish and other edible aquatic life, and are a major source of fresh water, which can be used for drinking and irrigation. It is therefore no surprise to find most of the major cities of the world situated on the banks of rivers. Rivers help to determine the urban form of cities and neighbourhoods and their corridors often present opportunities for urban renewal through the development of foreshoreways such as riverwalks. Rivers also provide an easy means of disposing of waste-water and, in much of the less developed world, other wastes.

Watermill in Belgium

Fast flowing rivers and waterfalls are widely used as sources of energy, via watermills and hydroelectric plants. Evidence of watermills shows them in use for many hundreds of years such as in Orkney at Dounby Click Mill. Prior to the invention of steam power, water-mills for grinding cereals and for processing wool and other textiles were common across Europe. In the 1890s the first machines to generate power from river water were established at places such as Cragside in Northumberland and in recent decades there has been a significant increase in the development of large scale power generation from water, especially in wet mountainous regions such as Norway.

The coarse sediments, gravel, and sand, generated and moved by rivers are extensively used in construction. In parts of the world this can generate extensive new lake habitats as gravel pits re-fill with water. In other circumstances it can destabilise the river bed and the course of the river and cause severe damage to spawning fish populations which rely on stable gravel formations for egg laying.

In upland rivers, rapids with whitewater or even waterfalls occur. Rapids are often used for recreation, such as whitewater kayaking.

Rivers have been important in determining political boundaries and defending countries. For example, the Danube was a long-standing border of the Roman Empire, and today it forms most of the border between Bulgaria and Romania. The Mississippi in North America and the Rhine in Europe are major east-west boundaries in those continents. The Orange and Limpopo Rivers in southern Africa form the boundaries between provinces and countries along their routes.

Ecosystem[link]

The organisms in the riparian zone respond to changes in river channel location and patterns of flow. The ecosystem of rivers is generally described by the River continuum concept, which has some additions and refinements to allow for spatial (dams, waterfalls) and temporal (extensive flooding). The basic idea is that the river can be described as a system that is continuously changing along its length in the physical parameters, the availability of food particles and the composition of the ecosystem. The food (energy) that is the leftover of the upstream part is being utilized downstream.

The general pattern is that the first order streams contain particulate matter (decaying leaves from the surrounding forests), which is processed there by shredders like Plecoptera larvae. The leftovers of the shredders are utilized by collectors, such as Hydropsychidae, and further downstream algae that create the primary production become the main foodsource of the organisms. All changes are gradual and the distribution of each species can be described as a normal curve with the highest density where the conditions are optimal. In rivers succession is virtually absent and the composition of the ecosystem stays fixed in time.

Chemistry[link]

The chemistry of rivers is complex and depends on inputs from the atmosphere, the geology through which it travels and the inputs from man's activities. The chemistry of the water has a large impact on the ecology of that water for both plants and animals and it also affects the uses that may be made of the river water. Understanding and characterising river water chemistry requires a well designed and managed sampling and analysis.

Like many other Aquatic ecosystems, rivers too are under increasing threat of pollution. According to a study of the WWF's Global Freshwater Programme, the 10 most polluted rivers are: Ganges, Indus, Yangtze, Salween-Nu, Mekong-Lancang, Rio Grande/Rio Bravo, Río de la Plata, Danube, Nile-Lake Victoria, and the Murray-Darling.^[17]

Brackish water[link]

Some rivers generate brackish water by having their river mouth in the ocean. This, in effect creates a unique environment in which certain species are found.

Flooding[link]

Flash flooding caused by heavy rain falling in a short amount of time

Flooding is a natural part of a river's cycle. The majority of the erosion of river channels and the erosion and deposition on the associated floodplains occur during flood stage. In many developed areas, human activity has changed river channel form, altering different magnitudes and frequencies of flooding. Some examples of this are the building of levees, the straightening of channels, and the draining of natural wetlands. In many cases human activities in rivers and floodplains have dramatically increased the risk of flooding. Straightening rivers allows water to flow more rapidly downstream increasing the risk of flooding places further downstream. Building on flood plains removes flood storage which again exacerbates downstream flooding. The building of levees may only protect the area behind the levees and not those further downstream. Levees and flood-banks can also increase flooding upstream because of back-water pressure as the upstream water has to squeeze between the levees.

Flow[link]

Studying the flows of rivers is one aspect of hydrology.^[18]

Direction[link]

A common misconception is that most, or even all, rivers flow from north to south.^[19][20][21] Rivers in fact flow downhill regardless of compass direction. Sometimes downhill is from north to south, but equally it can be from south to north, and usually is a complex meandering path involving all directions of the compass.^[22][23][24] Three of the ten longest rivers in the world—the Nile, Yenisei, and Ob—flow north, as do other major rivers such as the Rhine, Mackenzie, and Nelson.

Rivers flowing downhill, from river source to river mouth, do not necessarily take the shortest path. For alluvial streams, straight and braided rivers have very low sinuosity and flow directly down hill, while meandering rivers flow from side to side across a valley. Bedrock rivers typically flow in either a fractal pattern, or a pattern that is determined by weaknesses in the bedrock, such as faults, fractures, or more erodible layers.

Rate[link]

Volumetric flow rate, also called discharge, volume flow rate, and rate of water flow, is the volume of water which passes through a given cross-section of the river channel per unit time. It is typically measured in cubic meters per second (cumec) or cubic feet per second (cfs), where 1 m³/s = 35.51 ft³/s; it is sometimes also measured in litres or gallons per second.

Volumetric flow rate can be thought of as the mean velocity of the flow through a given cross-section, times that cross-sectional area. Mean velocity can be approximated through the use of the Law of the Wall. In general, velocity increases with the depth (or hydraulic radius) and slope of the river channel, while the cross-sectional area scales with the depth and the width: the double-counting of depth shows the importance of this variable in determining the discharge through the channel.

Sediment yield[link]

Sediment yield is the total quantity of particulate matter (suspended or bedload) reaching the outlet of a drainage basin over a fixed time frame. Yield is usually expressed as kilograms per square kilometre per year. Sediment delivery processes are affected by a myriad of factors such as drainage area size, basin slope, climate, sediment type (lithology), vegetation cover, and human land use / management practices. The theoretical concept of the 'sediment delivery ratio' (ratio between yield and total amount of sediment eroded) captures the fact that not all of the sediment eroded within a catchment reaches the outlet (due to, for example, deposition on floodplains). Such storage opportunities are typically increased in catchments of larger size, thus leading to a lower yield and sediment delivery ratio.

Management[link]

River bank repair

Rivers are often managed or controlled to make them more useful, or less disruptive, to human activity.

• Dams or weirs may be built to control the flow, store water, or extract energy.
• Levees, known as dikes in Europe, may be built to prevent river water from flowing on floodplains or floodways.
• Canals connect rivers to one another for water transfer or navigation.
• River courses may be modified to improve navigation, or straightened to increase the flow rate.

River management is a continuous activity as rivers tend to 'undo' the modifications made by people. Dredged channels silt up, sluice mechanisms deteriorate with age, levees and dams may suffer seepage or catastrophic failure. The benefits sought through managing rivers may often be offset by the social and economic costs of mitigating the bad effects of such management. As an example, in parts of the developed world, rivers have been confined within channels to free up flat flood-plain land for development. Floods can inundate such development at high financial cost and often with loss of life.

Rivers are increasingly managed for habitat conservation, as they are critical for many aquatic and riparian plants, resident and migratory fishes, waterfowl, birds of prey, migrating birds, and many mammals.

Gallery[link]

• 

  The Irrawaddy River is in a fairly untamed condition, with wide-reaching "arms and fingers" leading off the main water-flow

• 

  A false-color satellite photograph of the Amazon River in Brazil

See also[link]

Wikimedia Commons has media related to: River

Look up river in Wiktionary, the free dictionary.

	Environment portal
	Ecology portal

References[link]

Further reading[link]

• Jeffrey W. Jacobs. "Rivers, Major World". Water Encyclopaedia. http://www.waterencyclopedia.com/Re-St/Rivers-Major-World.html. 
• Luna B. Leopold (1994). A View of the River. Harvard University Press. ISBN 0-674-93732-5. OCLC 28889034. ISBN.  — a non-technical primer on the geomorphology and hydraulics of water.

External links[link]

• River Network - Connecting people, saving rivers (Environmental organization)

v t e Rivers, streams and springs Rivers Alluvial river Braided river Blackwater river Channel (geography) Channel pattern Channel types Confluence Distributary Drainage basin Subterranean river River bifurcation River ecosystem River source Tributary more... Streams Arroyo (creek) Burn Chalk stream Coulee Current (stream) Gill (stream) Stream Stream bed Stream channel Stream gradient Stream pool Perennial stream Winterbourne (stream) more... Springs Geyser Sacred spring Hot spring Mineral spring Rhythmic spring Spring Spring horizon more... Sedimentary processes and erosion Abrasion (geology) Anabranch Aggradation Armor (hydrology) Bed load Bed material load Granular flow Debris flow Deposition (geology) Dissolved load Downcutting Erosion Headward erosion Knickpoint Palaeochannel Progradation Retrogradation Saltation (geology) Secondary flow Sediment transport Suspended load Wash load Water gap Fluvial landforms Ait Alluvial fan Antecedent drainage stream Avulsion (river) Bank (geography) Bar (river morphology) Bayou Billabong Canyon Chine Cut bank Estuary Fluvial terrace Gulch Gully Glen Meander scar Mouth bar Oxbow lake Riffle-pool sequence Point bar Ravine Rill River island Rock-cut basin Sedimentary basin Sedimentary structures Strath Thalweg River valley Wadi Fluvial flow Helicoidal flow International Scale of River Difficulty Meander Plunge pool Rapid Riffle Shoal Waterfall Whitewater Surface runoff Agricultural wastewater treatment Effluent First flush Urban runoff Wastewater Floods and stormwater 100-year flood Crevasse splay Flash flood Flood Flood barrier Flood control Flood forecasting Flood-meadow Floodplain Flood pulse concept Flooded grasslands and savannas Storm Water Management Model Return period River measurement and modelling Baer's law Baseflow Bradshaw model Discharge (hydrology) Drainage density Exner equation Groundwater model Hack's law Hjulström curve Hydrograph Hydrological modelling Hydrological transport model Infiltration (hydrology) Main stem Playfair's Law Relief ratio River continuum concept Rouse number Runoff curve number Runoff model (reservoir) Stream gauge Universal Soil Loss Equation WAFLEX Wetted perimeter Volumetric flow rate River engineering Aqueduct Balancing lake Canal Check dam Dam Drop structure Daylighting (streams) Detention basin Erosion control Fish ladder Floodplain restoration Flume Infiltration basin Leat Levee Retention basin Revetment Riparian zone restoration Stream restoration Weir River sports Canyoning Rafting River surfing Riverboarding Whitewater canoeing Whitewater kayaking Whitewater slalom Other topics Aquifer Aquatic toxicology Body of water Limnology Riparian zone River civilization River cruise Surface water World Rivers Day Lists of rivers Rivers by continent Rivers by length Rivers by discharge rate Drainage basins Whitewater rivers Flash floods River name etymologies

chu:Ó'he'elez:ВацӀ