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{{Redirect|Branch river||Branch River (disambiguation)}}
{{more citations needed|date=May 2014}}
{{more citations needed|date=May 2014}}
{{short description|Stream branching off from main stream channel}}
[[Image:Malý Dunaj.jpg|thumb|[[Little Danube]] in [[Slovakia]] - an arm of the [[Danube]]]]
[[File:RMSDeltaNorth.jpg|thumb|[[Rhine–Meuse–Scheldt delta]], with the flow from right to left, showing several streams branching off from their main streams]]
[[Image:Bifurkation-Melle.JPG|thumb|The [[Else (Werre)|Else]] and [[Hase]] distributaries of the Hase at [[Melle, Germany]]]]

[[Image:NearNannilam.jpg|thumb|A seasonal distributary of the [[Kaveri river]] on the Kaveri delta, near [[Nannilam]], [[India]]]]
A '''distributary''', or a '''distributary channel''', is a [[stream]] that branches off and flows away from a main stream channel. They are a common feature of [[river delta]]s. The phenomenon is known as [[river bifurcation]]. The opposite of a distributary is a [[tributary]]. Distributaries usually occur as a stream nears a [[lake]] or an [[ocean]], but they can occur inland as well, such as on [[alluvial fans]] or when a tributary stream bifurcates as it nears its [[confluence]] with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can become the main route.
A '''distributary''', or a '''distributary channel''' is a [[stream]] [[channel (geography)|channel]] that branches off and flows {{em|away from}} a main stream channel. It is the opposite of a ''[[tributary]]'', a stream that flows {{em|towards and into}} another stream or river. Distributaries are a result of [[river bifurcation]] and are often found where a river approaches a [[lake]] or an [[ocean]] and divides into distributary networks; as such they are a common feature of [[river delta]]s.<ref>{{cite journal |title=Modeling river delta formation |last1=Seybold |first1=Hansjörg |last2=Andrade Jr. |first2=José |last3=Hermann |first3=Hans |date=23 October 2007 |volume=103 |number=43 |doi=10.1073/pnas.0705265104 |journal=Earth, Atmospheric, and Planetary Sciences |location=Boston |url=https://www.pnas.org/doi/full/10.1073/pnas.0705265104 |editor=H. Eugene Stanley|arxiv=0711.3283 }}</ref> They can also occur inland, on [[alluvial fan]]s, or where a tributary stream bifurcates as it nears its [[confluence]] with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can later become the main route.


==Related terms==
==Related terms==
Common terms to name individual river distributaries in [[English-speaking countries]] are ''arm'' and ''channel''. They may refer to a distributary that does not rejoin the channel it has branched from (e.g., the North, Middle, and South Arms of the [[Fraser River]], or the West Channel of the [[Mackenzie River]]), or to one that does (e.g. Annacis Channel and Annieville Channel of the [[Fraser River]], separated by [[Annacis Island]]).
Common terms to name individual river distributaries in [[English-speaking world|English-speaking countries]] are ''arm'' and ''channel''. These terms may refer to a distributary that does not rejoin the channel from which it has branched (e.g., the North, Middle, and South Arms of the [[Fraser River]], or the West Channel of the [[Mackenzie River]]), or to one that does (e.g. Annacis Channel and Annieville Channel of the [[Fraser River]], separated by [[Annacis Island]]).


In Australia, the term ''[[anabranch]]'' is used to refer to a distributary that diverts from the main course of the river and rejoins it later. In [[North America]] an anabranch is called a ''braided stream''.
In Australia, the term ''[[anabranch]]'' is used to refer to a distributary that diverts from the main course of the river and rejoins it later. In [[North America]] such a branching river is called a ''[[braided river]]''.<ref name=BristowBest>{{cite journal |title=Braided rivers: perspectives and problems |first1=C. S. |last1=Bristow |first2=J. L. |last2=Best |journal=Geological Society, London, Special Publications |volume=75 |pages=1–11 |date=1 January 1993 |issue=1 |doi=10.1144/GSL.SP.1993.075.01.01|bibcode=1993GSLSP..75....1B |s2cid=129232374 }}</ref>


==North America==
==North America==
[[File:Atchafalaya River.png|thumb|[[Atchafalaya River]]]]
[[File:Atchafalaya River.png|thumb|[[Atchafalaya River]]]]


In [[Louisiana]], the [[Atchafalaya River]] is an important distributary of the [[Mississippi River]]. Because the Atchafalaya takes a steeper route to the [[Gulf of Mexico]] than the main channel, over several decades it has captured more and more of the Mississippi's flow, after the Mississippi meandered into the [[Red River of the South]]. The [[Old River Control Structure]], a [[dam]] which regulates the outflow from the Mississippi into the Atchafalaya, was completed by the [[United States Army Corps of Engineers|Army corps of engineers]] in 1963. It is intended to prevent the Atchafalaya from capturing the main flow of the Mississippi and stranding the ports of [[Baton Rouge]] and [[New Orleans]].<ref>[[John McPhee]], [[The Control of Nature]] </ref>
In [[Louisiana]], the [[Atchafalaya River]] is an important distributary of the [[Mississippi River]]. Because the Atchafalaya takes a steeper route to the [[Gulf of Mexico]] than does the Mississippi, over several decades the Atchafalaya has captured more and more of the Mississippi's flow, after the Mississippi meandered into the [[Red River of the South]]. The [[Old River Control Structure]], a [[dam]] which regulates the outflow from the Mississippi into the Atchafalaya, was completed by the [[United States Army Corps of Engineers|Army Corps of Engineers]] in 1963. The dam is intended to prevent the Atchafalaya from capturing the main flow of the Mississippi and stranding the ports of [[Baton Rouge]] and [[New Orleans]].<ref>[[John McPhee]], [[The Control of Nature]]</ref>


In [[British Columbia]], Canada, the [[Fraser River]] has numerous sloughs and side-channels which may be defined as distributaries. Its final stretch has three main distributaries: the [[North Arm of the Fraser|North Arm]] and the [[South Arm of the Fraser|South Arm]], and a few smaller ones adjoining them.
In [[British Columbia]], Canada, the [[Fraser River]] has numerous sloughs and side-channels which may be defined as distributaries. This river's final stretch has three main distributaries: the [[North Arm of the Fraser|North Arm]] and the [[South Arm of the Fraser|South Arm]], and a few smaller ones adjoining them.


Examples of inland distributaries:
Examples of inland distributaries:
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==South America==
==South America==
The [[Casiquiare]] is an inland distributary of the upper [[Orinoco]], which flows southward into the [[Rio Negro (Amazon)|Rio Negro]] and forms a unique natural [[canal]] between the Orinoco and [[Amazon River|Amazon]] river systems. It is the largest river on the planet that links two major river systems.
The [[Casiquiare canal]] is an inland distributary of the upper [[Orinoco]], which flows southward into the [[Rio Negro (Amazon)|Rio Negro]], forming a unique natural [[canal]] between the Orinoco and [[Amazon River|Amazon river]] systems. It is the largest river on the planet that links two major river systems.


==Europe==
==Europe==
[[File:Maas_Delta1.jpg|thumb|right|250px|Satellite image of part of the [[Rhine–Meuse–Scheldt delta]]]]
[[File:Maas_Delta1.jpg|thumb|right|250px|Satellite image of part of the [[Rhine–Meuse–Scheldt delta]]]]
*The [[IJssel]], the [[Waal (river)|Waal]] and the [[Nederrijn]] (Lower Rhine) are the three principal distributaries of the [[Rhine]]. These are formed by two separate bifurcations within the [[Rhine–Meuse–Scheldt delta]].
*The [[IJssel]], the [[Waal (river)|Waal]] and the [[Nederrijn]] (Lower Rhine) are the three principal distributaries of the [[Rhine]]. These are formed by two separate bifurcations within the [[Rhine–Meuse–Scheldt delta]].
*The [[Akhtuba River]] is a major distributary of the [[Volga]]. The bifurcation occurs close to, but before, the [[Volga Delta]].
*The [[Akhtuba River]] is a major distributary of the [[Volga]]. The bifurcation occurs close to, but before, the [[Volga Delta]].
* The [[Tärendö River]] in northern [[Sweden]] is an '''inland distributary''', far from the mouth of the river. It begins at the [[Torne River]] and ends at the [[Kalix River]].
* The [[Tärendö River]] in northern [[Sweden]] is an '''inland distributary''', far from the mouth of the river. It begins at the [[Torne (Finnish and Swedish river)|Torne River]] and ends at the [[Kalix River]].
* The [[Little Danube]] in [[Slovakia]] branches off from the [[Danube]] near Bratislava, and flows into the [[Vah]] before rejoining the main river near [[Komárno]]. The area in the middle is the largest freshwater island in Europe.
* The [[Little Danube]] in [[Slovakia]] branches off from the [[Danube]] near Bratislava, and flows into the [[Vah]] before rejoining the main river near [[Komárno]]. The area in the middle is the largest freshwater island in Europe.
* The [[Abbey River, Limerick|Abbey River]], [[Limerick]], in [[Ireland]] is a distributary arm of the [[River Shannon]]. It rejoins the Shannon to form an island upon which [[King John's Castle (Limerick)|King John's Castle]] is built.
* The [[Abbey River, Limerick|Abbey River]], [[Limerick]], in [[Ireland]] is a distributary arm of the [[River Shannon]]. It rejoins the Shannon to form an island upon which [[King John's Castle (Limerick)|King John's Castle]] is built.
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The [[Huai River]] in China splits into three streams. The main stream passes through the Sanhe Sluice, goes out of the Sanhe river, and enters the [[Yangtze|Yangtze River]] through [[Baoying County|Baoying]] Lake and [[Gaoyou Lake]]. On the east bank of [[Hongze Lake]], another stream goes out of [[Hongze District|Gaoliangjian]] Gate and enters the [[Yellow Sea]] at the [[port]] of Bidan through Subei Guan'gai Zongqu, the main [[irrigation]] channel of Northern [[Jiangsu]]); its total length is 168 kilometers. The third stream leaves the Erhe lock on the northeast bank of Hongze Lake, passes the Huaishuhe River to the north of [[Lianyungang]] city, and flows into Haizhou Bay through the Hongkou.
The [[Huai River]] in China splits into three streams. The main stream passes through the Sanhe Sluice, goes out of the Sanhe river, and enters the [[Yangtze|Yangtze River]] through [[Baoying County|Baoying]] Lake and [[Gaoyou Lake]]. On the east bank of [[Hongze Lake]], another stream goes out of [[Hongze District|Gaoliangjian]] Gate and enters the [[Yellow Sea]] at the [[port]] of Bidan through Subei Guan'gai Zongqu, the main [[irrigation]] channel of Northern [[Jiangsu]]); its total length is 168 kilometers. The third stream leaves the Erhe lock on the northeast bank of Hongze Lake, passes the Huaishuhe River to the north of [[Lianyungang]] city, and flows into Haizhou Bay through the Hongkou.

===Southeast Asia===

The [[Tha Chin River]] and [[Noi River]] are distributaries of the [[Chao Phraya River]] in [[Thailand]], splitting off from the latter about 200 kilometers upstream from the [[Bay of Bangkok]].

The [[Brantas River]] in [[East Java]], [[Indonesia]], branches off into two distributaries, [[Mas River]], also known as Surabaya River, and [[Porong River]].<ref>{{cite conference |last1=Valiant |first1=Raymond |title=TANTANGAN DALAM PENGELOLAAN SUMBERDAYA AIR UNTUK MENCAPAI LINGKUNGAN LESTARI BERKELANJUTAN: POTRET DAERAH ALIRAN SUNGAI (DAS) BRANTAS |url=https://kmc-pengairan.bappenas.go.id/knowledge-management/download/340 |conference=Seminar Pekan DAS Brantas 2014 |publisher=Fakultas Teknik Universitas Brawijaya Malang |date=2014 |access-date=28 March 2024}}</ref>


===Indian Subcontinent===
===Indian Subcontinent===
[[Image:NearNannilam.jpg|thumb|A seasonal distributary of the [[Kaveri|Kaveri River]] on the Kaveri delta, near [[Nannilam]], [[India]]]]
* [[Kollidam River]] is a distributary of the [[Kaveri River]].
* [[Kollidam River]] is a distributary of the [[Kaveri River]].
* [[Himalaya]]n rivers including Ganges, Brahmaputra and [[Indus]] plus many tributaries form inland distributaries over vast [[alluvial fans]] as they transition from the mountain region to the flat [[Indo-Gangetic Plain]]. These areas are highly flood-prone, for example the [[2008 Bihar flood]] on the [[Kosi River]].
* [[Himalaya]]n rivers including Ganges, Brahmaputra and [[Indus]] plus many tributaries form inland distributaries over vast [[alluvial fans]] as they transition from the mountain region to the flat [[Indo-Gangetic Plain]]. These areas are highly flood-prone, for example the [[2008 Bihar flood]] on the [[Kosi River]].
* [[Padma River]] is the main distributary of the [[Ganges]] in [[Bangladesh]].
* [[Hoogli River]] is a [[Ganges]] distributary that flows through [[India]], whereas most of the Ganges-[[Brahmaputra]] complex enters the sea through [[Bangladesh]].
* [[Hoogli River]] is a [[Ganges]] distributary that flows through [[India]], whereas most of the Ganges-[[Brahmaputra]] complex enters the sea through [[Bangladesh]].
* [[Nara Canal|Nara River]] is a distributary of the [[Indus River]].
* [[Nara Canal|Nara River]] is a distributary of the [[Indus River]].


==Africa==
==Africa==
* The [[Nile River]] has two distributaries, the [[Rosetta]] and the [[Damietta]] branches. According to [[Pliny the Elder]] it had in ancient times seven distributaries (east to west):
* The [[Nile River]] has two distributaries, the [[Rosetta]] and the [[Damietta]] branches. According to [[Pliny the Elder]] it had in ancient times seven distributaries (east to west):
** The Pelusiac
** The Pelusiac
** The Tanitic
** The Tanitic
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===New Zealand===
===New Zealand===
New Zealand's second-longest river, the [[Clutha River]], splits into two arms, the ''Matau'' and the ''Koua'', some 10 kilometres from the South Island's Pacific Coast. A large island, [[Inch Clutha]], lies between the two arms. Many of the rivers crossing the [[Canterbury Plains]] in the central South Island are [[braided river]]s, and several of these split into separate branches before reaching the coast. Notable among these is the [[Rangitata River]], the two arms of which are separated by the low-lying [[Rangitata Island]].
New Zealand's second-longest river, the [[Clutha River]], splits into two arms, the ''[[Matau River|Matau]]'' and the ''[[Koua River|Koua]]'', some 10 kilometres from the South Island's Pacific Coast. A large island, [[Inch Clutha]], lies between the two arms. Many of the rivers crossing the [[Canterbury Plains]] in the central South Island are [[braided river]]s, and several of these split into separate branches before reaching the coast. Notable among these is the [[Rangitata River]], the two arms of which are separated by the low-lying [[Rangitata Island]].

==See also==
* [[Tributary]]


==References==
==References==
{{reflist}}
*{{cite journal |last=Olariu |first=Cornel |last2=Bhattacharya |first2=Janok P. |date=2006 |title=Terminal Distributary Channels and Delta Front Architecture of River-Dominated Delta Systems |url=http://eas.uh.edu/docs/geos/faculty-files/pdf/37_olariu_tdc_2006.pdf |journal=Journal of Sedimentary Research |publisher=Society for Sedimentary Geology |volume=76 |issue= |pages=212–233 |doi=10.2110/jsr.2006.026 |accessdate=December 10, 2013 |deadurl=yes |archiveurl=https://web.archive.org/web/20151223195548/http://www.eas.uh.edu/docs/geos/faculty-files/pdf/37_Olariu_TDC_2006.pdf |archivedate=December 23, 2015 |df= }}

=== Citations ===
* {{Cite journal |last1=Olariu |first1=Cornel |last2=Bhattacharya |first2=Janok P. |date=2006 |title=Terminal Distributary Channels and Delta Front Architecture of River-Dominated Delta Systems |url=http://eas.uh.edu/docs/geos/faculty-files/pdf/37_olariu_tdc_2006.pdf |journal=Journal of Sedimentary Research |publisher=Society for Sedimentary Geology |volume=76 |issue=2 |pages=212–233 |doi=10.2110/jsr.2006.026 |bibcode=2006JSedR..76..212O |access-date=December 10, 2013 |url-status=dead |archive-url=https://web.archive.org/web/20151223195548/http://www.eas.uh.edu/docs/geos/faculty-files/pdf/37_Olariu_TDC_2006.pdf |archive-date=December 23, 2015 }}

{{Rivers, streams and springs}}


[[Category:Distributaries| ]]
[[Category:Distributaries| ]]
[[Category:River bifurcations]]
[[Category:River bifurcations|*]]
[[Category:River morphology]]
[[Category:River morphology]]



Latest revision as of 12:36, 28 August 2024

Rhine–Meuse–Scheldt delta, with the flow from right to left, showing several streams branching off from their main streams

A distributary, or a distributary channel is a stream channel that branches off and flows away from a main stream channel. It is the opposite of a tributary, a stream that flows towards and into another stream or river. Distributaries are a result of river bifurcation and are often found where a river approaches a lake or an ocean and divides into distributary networks; as such they are a common feature of river deltas.[1] They can also occur inland, on alluvial fans, or where a tributary stream bifurcates as it nears its confluence with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can later become the main route.

[edit]

Common terms to name individual river distributaries in English-speaking countries are arm and channel. These terms may refer to a distributary that does not rejoin the channel from which it has branched (e.g., the North, Middle, and South Arms of the Fraser River, or the West Channel of the Mackenzie River), or to one that does (e.g. Annacis Channel and Annieville Channel of the Fraser River, separated by Annacis Island).

In Australia, the term anabranch is used to refer to a distributary that diverts from the main course of the river and rejoins it later. In North America such a branching river is called a braided river.[2]

North America

[edit]
Atchafalaya River

In Louisiana, the Atchafalaya River is an important distributary of the Mississippi River. Because the Atchafalaya takes a steeper route to the Gulf of Mexico than does the Mississippi, over several decades the Atchafalaya has captured more and more of the Mississippi's flow, after the Mississippi meandered into the Red River of the South. The Old River Control Structure, a dam which regulates the outflow from the Mississippi into the Atchafalaya, was completed by the Army Corps of Engineers in 1963. The dam is intended to prevent the Atchafalaya from capturing the main flow of the Mississippi and stranding the ports of Baton Rouge and New Orleans.[3]

In British Columbia, Canada, the Fraser River has numerous sloughs and side-channels which may be defined as distributaries. This river's final stretch has three main distributaries: the North Arm and the South Arm, and a few smaller ones adjoining them.

Examples of inland distributaries:

South America

[edit]

The Casiquiare canal is an inland distributary of the upper Orinoco, which flows southward into the Rio Negro, forming a unique natural canal between the Orinoco and Amazon river systems. It is the largest river on the planet that links two major river systems.

Europe

[edit]
Satellite image of part of the Rhine–Meuse–Scheldt delta

Asia

[edit]

Eastern Asia

[edit]

The Huai River in China splits into three streams. The main stream passes through the Sanhe Sluice, goes out of the Sanhe river, and enters the Yangtze River through Baoying Lake and Gaoyou Lake. On the east bank of Hongze Lake, another stream goes out of Gaoliangjian Gate and enters the Yellow Sea at the port of Bidan through Subei Guan'gai Zongqu, the main irrigation channel of Northern Jiangsu); its total length is 168 kilometers. The third stream leaves the Erhe lock on the northeast bank of Hongze Lake, passes the Huaishuhe River to the north of Lianyungang city, and flows into Haizhou Bay through the Hongkou.

Southeast Asia

[edit]

The Tha Chin River and Noi River are distributaries of the Chao Phraya River in Thailand, splitting off from the latter about 200 kilometers upstream from the Bay of Bangkok.

The Brantas River in East Java, Indonesia, branches off into two distributaries, Mas River, also known as Surabaya River, and Porong River.[4]

Indian Subcontinent

[edit]
A seasonal distributary of the Kaveri River on the Kaveri delta, near Nannilam, India

Africa

[edit]
  • The Nile River has two distributaries, the Rosetta and the Damietta branches. According to Pliny the Elder it had in ancient times seven distributaries (east to west):
    • The Pelusiac
    • The Tanitic
    • The Mendesian
    • The Phatnitic
    • The Sebennytic
    • The Bolbitine
    • The Canopic
See History of the Nile Delta.
  • The Okavango River ends in many distributaries in a large inland delta called the Okavango Delta. It is an example of distributaries that do not flow into any other body of water.

Oceania

[edit]
Delta of Papua New Guinea's Fly River

Australia

[edit]

A number of the rivers that flow inland from Australia's Great Dividing Range form distributaries, most of which flow only intermittently during times of high river levels and end in shallow lakes or simply peter out in the deserts. Yarriambiack Creek, which flows from the Wimmera River into Lake Coorong, and Tyrrell Creek, which flows from the Avoca River into Lake Tyrrell, are two distributaries in Victoria. The Narran River flows from the Balonne River in Queensland into Narran Lake in New South Wales.

Papua New Guinea

[edit]

Many of Papua New Guinea's major rivers flow into the Gulf of Papua through marshy, low-lying country, allowing for wide, many-branched deltas. These include the Fly River, which splits into three major and several minor rivers close to its mouth. The Bamu River splits into several channels close to its mouth, among them the Bebea, Bina, Dibiri, and Aramia. The Kikori River also splits into a multitude of channels as it crosses the plains close to the Gulf of Papua. The Purari River splits into three major channels as it approaches its mouth.

New Zealand

[edit]

New Zealand's second-longest river, the Clutha River, splits into two arms, the Matau and the Koua, some 10 kilometres from the South Island's Pacific Coast. A large island, Inch Clutha, lies between the two arms. Many of the rivers crossing the Canterbury Plains in the central South Island are braided rivers, and several of these split into separate branches before reaching the coast. Notable among these is the Rangitata River, the two arms of which are separated by the low-lying Rangitata Island.

References

[edit]
  1. ^ Seybold, Hansjörg; Andrade Jr., José; Hermann, Hans (23 October 2007). H. Eugene Stanley (ed.). "Modeling river delta formation". Earth, Atmospheric, and Planetary Sciences. 103 (43). Boston. arXiv:0711.3283. doi:10.1073/pnas.0705265104.
  2. ^ Bristow, C. S.; Best, J. L. (1 January 1993). "Braided rivers: perspectives and problems". Geological Society, London, Special Publications. 75 (1): 1–11. Bibcode:1993GSLSP..75....1B. doi:10.1144/GSL.SP.1993.075.01.01. S2CID 129232374.
  3. ^ John McPhee, The Control of Nature
  4. ^ Valiant, Raymond (2014). TANTANGAN DALAM PENGELOLAAN SUMBERDAYA AIR UNTUK MENCAPAI LINGKUNGAN LESTARI BERKELANJUTAN: POTRET DAERAH ALIRAN SUNGAI (DAS) BRANTAS. Seminar Pekan DAS Brantas 2014. Fakultas Teknik Universitas Brawijaya Malang. Retrieved 28 March 2024.

Citations

[edit]