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Rio Negro (Amazon)

Coordinates:3°08′00″S59°54′30″W / 3.13333°S 59.90833°W /-3.13333; -59.90833
From Wikipedia, the free encyclopedia
Tributary of the Amazon River
For other uses, seeRio Negro (disambiguation).
Rio Negro
Guainía River
Sunset over the Rio Negro, upstream fromManaus
Map showing the Rio Negro in theAmazon Basin
Native name
Location
Countries
Physical characteristics
Sourcehighlands of Colombia
 • locationGuainía Department,Amazon region,Colombia
 • coordinates1°56′50″N70°1′55″W / 1.94722°N 70.03194°W /1.94722; -70.03194 (approximately)
 • elevation250 m (820 ft) (approximately)
MouthAmazon River
 • location
Manaus,Amazonas State,Brazil
 • coordinates
3°08′00″S59°54′30″W / 3.13333°S 59.90833°W /-3.13333; -59.90833
 • elevation
8 m (26 ft)[1]
LengthRio Negro–Guainía 2,250 km (1,400 mi)[2]
Basin size714,577.6 km2 (275,900.0 sq mi)[3]
Width 
 • average2,450 m (8,040 ft)[4]
Depth 
 • average20 m (66 ft) (Serrinha); 24 m (79 ft) to 31 m (102 ft) (Manaus)[3]
 • maximum60 m (200 ft) (Manaus)[4]
Discharge 
 • locationManaus
 • average(Period: 2015–2019)34,573 m3/s (1,220,900 cu ft/s)[4]
 • minimum4,240 m3/s (150,000 cu ft/s)[3]
 • maximum64,380 m3/s (2,274,000 cu ft/s)[3]
Discharge 
 • locationParicatuba (Anavilhanas)
 • average(Period: 2008–2019)34,444 m3/s (1,216,400 cu ft/s)[5]
 • minimum7,633 m3/s (269,600 cu ft/s) (2009/10)[5]
 • maximum65,510 m3/s (2,313,000 cu ft/s) (2014/06)[5]
Discharge 
 • locationSerrinha,0°28′57.4716″S64°49′36.6492″W / 0.482631000°S 64.826847000°W /-0.482631000; -64.826847000
 • average(Period: 1997–2015)16,845.5 m3/s (594,890 cu ft/s)[7]
 • minimum5,000 m3/s (180,000 cu ft/s)[6]
 • maximum30,000 m3/s (1,100,000 cu ft/s)[6]
Discharge 
 • locationSão Felipe,0°22′11.8056″N67°18′42.9948″W / 0.369946000°N 67.311943000°W /0.369946000; -67.311943000
 • average(Period: 1997–2014)8,314.5 m3/s (293,620 cu ft/s)[7]
 • minimum1,200 m3/s (42,000 cu ft/s)[6]
 • maximum15,500 m3/s (550,000 cu ft/s)[6]
Discharge 
 • locationCucuí
 • average(Period: 1997–2014)5,113.1 m3/s (180,570 cu ft/s)[7]
 • minimum400 m3/s (14,000 cu ft/s)[6]
 • maximum10,500 m3/s (370,000 cu ft/s)[6]
Basin features
ProgressionAmazonAtlantic Ocean
River systemAmazon River
Tributaries 
 • leftCasiquiare,Cauaburi,Marauiá,Macucuaú,Padauari,Demini,Jufari,Branco,Jauaperi,Camanaú,Baependi,Apuaú,Cuieiras,Tarumã Mirim,Tarumã Açu
 • rightGuainía (Upper Negro),Xié,Içana,Uaupés,Curicuriari,Marié,Tea,Uneiuxi, Aiuanã,Urubaxi,Ararirá,Cuiuni,Caurés,Unini,Jaú,Puduari

TheRio Negro (Spanish:Río Negro[ˈri.oˈneɣɾo] "Black River"), orGuainía as it is known in its upper part, is the largest lefttributary of theAmazon River (accounting for about 14% of the water in theAmazon basin), the largestblackwater river in the world,[8] and one of the world's tenlargest rivers by average discharge. It originates in the tepuis of the department ofGuainía,Colombia, and then flows southeastward before finally enteringBrazil. Despite its high flow, the Rio Negro has a lowsediment load (5.76 million tonnes per year on average inManaus).[4]

Geography

[edit]
Rio Negro watershed (Interactive map)

Upper course

[edit]

The source of the Rio Negro lies inColombia, in theDepartment of Guainía where the river is known as theGuainía River.[9] The young river generally flows in an east-northeasterly direction through thePuinawai National Reserve, passing several small indigenous settlements on its way, such as Cuarinuma, Brujas, Santa Rosa and Tabaquén. After roughly 400 km (250 mi) the river starts forming the border between Colombia'sDepartment of Guainía and Venezuela'sAmazonas State. After passing the Colombian community of Tonina and Macanal the river turns southwest.Maroa is the first Venezuelan town the river passes. 120 km (75 mi) further downstream the river receives theCasiquiare canal from the left (north), forming a unique link between theOrinoco and the Amazon river basin.

Middle course

[edit]

The river now continues in a southeastern direction passing the Venezuelan town ofSan Carlos de Río Negro, its largest settlement on the river, and Colombia'sSan Felipe.In this stretch the river is constantly fed with tributaries from both sides, and it quickly grows in size creating large river islands, a common feature for all rivers in the Amazon basin. After forming the border between Colombia and Venezuela for 260 km (160 mi) the Rio Negro reaches thePiedra del Cocuy, an igneous rock formation from the Precambrian era, belonging to theGuyana Shield. Here theTripoint of Colombia, Venezuela and Brazil is found in the middle of the river and it now completely entersAmazonas State, Brazil. After passingCucuí, the river continues south, only temporarily turning west for several kilometers. InMissão Boa Vista theIçana River joins the Rio Negro and in São Joaquim theUaupes River, the largest tributary of the Rio Negro, also enters from the right hand side. The Rio Negro now turns markedly towards the east, forming several rapids and small islets on its way. It then passesSao Gabriel da Cachoeira an important commercial city. After several more rapids and imposing views of the Adormecida mountain chain the river leaves the Guyana shield it traversed in its upper and middle course.

Lower course

[edit]
The confluence of theAmazon River and the Rio Negro atManaus,Brazil.

After theMarié River enters the Rio Negro the river continues its eastward course forming many large islands and becoming very wide at several locations. It passes local communities such asSanta Isabel do Rio Negro. During thewet season, the river floods the country far and wide here, sometimes to a width of 30 km (19 mi), for long distances. During this season, from April until October, it is a succession of lagoons, full of long islands and intricate channels with a lot of water wildlife. Near Carvoeiro the last major tributary of the Rio Negro, theBranco River joins the Rio Negro and the river temporarily forms the border between the state ofRoraima andAmazonas State, Brazil. The river now takes a more southeastern course, becoming again very wide in many stretches before reaching the biggest city on its courseManaus.

TheAnavilhanas National Park, a 350,018 ha (864,910 acres) conservation unit that was originally an ecological station created in 1981, protects part of the Anavilhanas river archipelago in this part of the river.[10]Below the archipelago, it meets theSolimões River to form theAmazon River, creating a phenomenon known as theMeeting of Waters.

Major tributaries

[edit]

List of the major tributaries of the Rio Negro (from the mouth upwards)[11][3][12][13]

Left tributaryRight tributaryLengthBasin sizeAverage discharge
kmmikm2sq mim3/scu ft/s
Rio Negro2,3621,468719,216277,69130,640.81,082,070
Lower Rio Negro
Taruma-Açu139861,37253052.31,850
Cuieiras3,4411,329144.25,090
Apuaú3,799.11,466.8153.65,420
Puduari3,411.51,317.2128.64,540
Camanaú11,832.24,568.440814,400
Jaú40025018,896.67,296.0869.230,700
Jauaperi55434439,823.515,375.91,336.847,210
Unini53033027,43310,5921,501.453,020
Branco1,430890190,789.273,664.15,400190,000
Jufari31119312,590.54,861.2446.615,770
Cauarés7,332.32,831.029610,500
Demini39,769.615,355.11,357.947,950
Cuiuni40025011,776.14,546.8491.617,360
Igarapé Adairá3,294.91,272.2101.13,570
Ararirá3,4251,322114.64,050
Ererê3,2511,255115.74,090
Padauari17,3846,712606.821,430
Daraá3,053.31,178.9114.94,060
Urubaxi2501606,855.92,647.1311.611,000
Aiuanã4,590.71,772.5185.26,540
Uneiuxi12,474.74,816.5488.317,240
Teá6,365.92,457.9201.47,110
Marauiá6,7122,592255.39,020
Igarapé Inambu4,618.81,783.3140.64,970
Cauaburi12,139.34,687.0442.915,640
Middle Rio Negro
Marié80050025,3789,7991,226.843,320
Curicuriari14,202.25,483.5916.832,380
Uaupés1,37585464,370.424,853.64,344.9153,440
Içana69643235,675.313,774.32,278.980,480
Xié8,2223,175488.117,240
Upper Rio Negro
Casiquiare35422042,47816,4012,575.890,960
Guainía61738328,899.511,158.22,432.785,910

Discharge

[edit]
Rio Negro atManaus (1970–2023):[14]
YearAverage discharge (m3/s)
2023
20,000
2022
33,000
2021
35,000
2020
30,000
2019
32,600
2018
29,300
2017
31,200
2016
25,000
2015
34,000
2014
40,000
2013
32,600
2012
29,700
2011
23,200
2010
20,500
2009
32,000
2008
33,000
2007
29,500
2006
25,500
2005
28,200
2004
33,000
2003
31,600
2002
29,400
2001
31,000
2000
31,700
1999
28,000
1998
20,500
1997
29,000
1996
30,000
1995
27,400
1994
38,000
(continues)
YearAverage discharge (m3/s)
1993
33,700
1992
23,000
1991
25,500
1990
29,500
1989
34,500
1988
30,800
1987
44,000
1986
40,300
1985
34,000
1984
32,400
1983
27,800
1982
32,000
1981
27,700
1980
26,500
1979
34,200
1978
38,700
1977
36,000
1976
36,300
1975
42,000
1974
50,800
1973
40,400
1972
40,800
1971
39,000
1970
30,000
1926
17,500

Average discharge

PeriodDischargeRef.
Encontro das Águas
1979–2015

30,640.8 m3/s (1,082,070 cu ft/s)

[11]
1971–200029,615.7 m3/s (1,045,870 cu ft/s)[12]
Manaus

3°8′19.3704″S60°1′39.522″W / 3.138714000°S 60.02764500°W /-3.138714000; -60.02764500

2015–201934,573 m3/s (1,220,900 cu ft/s)[4]
1980–200635,943 m3/s (1,269,300 cu ft/s)[15]
1973–199228,400 m3/s (1,000,000 cu ft/s)[16]
1971–200029,607.4 m3/s (1,045,580 cu ft/s)[12]
Paricatuba

3°4′53.2848″S60°14′0.4812″W / 3.081468000°S 60.233467000°W /-3.081468000; -60.233467000

2008–201934,444 m3/s (1,216,400 cu ft/s)[5]
1971–200029,518.2 m3/s (1,042,430 cu ft/s)[12]
Barcelos

0°58′59.6964″S62°51′32.3892″W / 0.983249000°S 62.858997000°W /-0.983249000; -62.858997000

1971–200019,545.2 m3/s (690,230 cu ft/s)[12]
Serrinha

0°28′57.4716″S64°49′36.6492″W / 0.482631000°S 64.826847000°W /-0.482631000; -64.826847000

1997–201516,845.5 m3/s (594,890 cu ft/s)[7]
1980–200618,082 m3/s (638,600 cu ft/s)[15]
1971–200016,611.9 m3/s (586,640 cu ft/s)[12]
São Gabriel da Cachoeira

0°8′2.9616″S67°5′38.2956″W / 0.134156000°S 67.093971000°W /-0.134156000; -67.093971000

1971–200013,150.7 m3/s (464,410 cu ft/s)[12]
São Felipe

0°22′11.8056″N67°18′42.9948″W / 0.369946000°N 67.311943000°W /0.369946000; -67.311943000

1997–20148,314.5 m3/s (293,620 cu ft/s)[7]
1980–20067,984 m3/s (282,000 cu ft/s)[15]
1971–20008,244.8 m3/s (291,160 cu ft/s)[12]
Cucuí

1°11′16.7316″S66°50′23.46″W / 1.187981000°S 66.8398500°W /-1.187981000; -66.8398500

1997–20145,113.1 m3/s (180,570 cu ft/s)[7]
1980–20064,940 m3/s (174,000 cu ft/s)[15]
1971–20005,065.1 m3/s (178,870 cu ft/s)[12]

History

[edit]

The river was named by the Spanish explorerFrancisco de Orellana, who first came upon it in 1541. By the middle of the 17th century, Jesuits had settled along its banks in the midst of numerous tribes: Manau, Aruák, and Trumá Indians. After 1700 slaving along the river was common, andNative American populations were greatly diminished after contact with Eurasian diseases.[9] In 1800 German scientistAlexander von Humboldt[17] and French botanistAimé Bonpland explored the river.[18] During 1852–1854Richard Spruce andAlfred Russel Wallace made numerous observations and botanical collections.[19] During a 1924–25 expedition,Alexander H. Rice Jr. ofHarvard University traveled up the Orinoco, traversed the Casiquiare canal, and descended the Rio Negro to the Amazon at Manaus. It was the first expedition to use aerial photography andshortwave radio for mapping of the region. In 1968 the Rio Negro was navigated by anSRN6 hovercraft during aNational Geographic expedition.[20] This area was the filming location for Survivor:The Amazon in 2003.[citation needed]

Fauna and flora

[edit]
Rio Negro nearManaus
Victoria amazonica

While the nameRio Negro meansBlack River, its waters are similar in colour to strongtea, which is typical ofblackwater rivers. The dark color comes fromhumic acid due to an incomplete breakdown of phenol-containing vegetation from sandy clearings.[citation needed] The river was named because it looks black from a distance.

Much has been written on the productivity of the Rio Negro and other blackwater rivers. The older idea that these are "hunger rivers" is giving way, with new research, to the recognition that the Rio Negro, for example, supports a large fishing industry and has numerous turtle beaches. If explorers did not find manyIndigenous peoples along the Rio Negro during the 17th century, it is likely that their populations were reduced because of new infectious diseases and warfare rather than low river productivity.

Rio Negro has a very highspecies richness. About 700 fish species have been documented in the river basin, and it is estimated that the total is 800–900 fish species, including almost 100endemics and severalundescribed species.[21] Among these are many that are important in theaquarium trade, including thecardinal tetra.[21] As a result of theCasiquiare canal, many aquatic species are found both in the Rio Negro and Orinoco. Because the Casiquiare includes both blackwater andclear- towhitewater sections, only relatively adaptable species are able to pass through it between the two river systems.[22]

In media

[edit]

The sixth season ofSurvivor,Survivor: The Amazon was filmed in Rio Negro in 2003. AlsoMeeting of the Waters byAnimal Collective was recorded in Rio Negro in 2016.[citation needed]

Henryk Wars and his Orchestra composed and recorded apasodoble named "Rio Negro", with Edward Jasinski in 1938, which became an evergreen hit in Poland.[23]

Notes

[edit]
  1. ^Tannenbaum, Frank (29 August 2012).TEN KEYS LAT AMER. Knopf Doubleday Publishing Group.ISBN 9780307826565. Retrieved9 April 2018 – via Google Books.
  2. ^Ziesler, R.; Ardizzone, G.D. (1979). "Amazon River System".The Inland waters of Latin America.Food and Agriculture Organization of the United Nations.ISBN 92-5-000780-9.Archived from the original on 8 November 2014.
  3. ^abcde"Amazon basin water resources observation service".
  4. ^abcdeRogério Ribeiro, Marinho; Naziano Filizola, Junior; Jean Michel, Martinez; Tristan, Harmel (2022)."Suspended sediment transport estimation in Negro River (Amazon Basin) using MSI/Sentinel-2 data".Revista Brasileira de Geomorfologia.23.doi:10.20502/rbg.v23i1.2076.
  5. ^abcdRogério Ribeiro, Marinho; Paulo Rodrigo, Zanin; Naziano Pantoja, Filizola Junior (2021)."The Negro River in the Anavilhanas Archipelago: Streamflow and geomorphology of a complex anabranching system in the Amazon".Earth Surface Processes and Landforms.47 (4):1108–1123.doi:10.1002/esp.5306.
  6. ^abcdefJuan Gabriel, Leon; Stèphane, Calmont; F., Seyler; Marie-Paule, Bonnet; Mathilde, Cauhopé; Frédéric, Frappart; Naziano, Filizola; Pascal, Fraizy (2010)."Rating curves and estimation of average water depth at the upper Negro River based on satellite altimeter data and modeled discharges".Journal of Hydrology.328 (3–4):481–496.doi:10.1016/J.JHYDROL.2005.12.006.
  7. ^abcdefJamie, Towner (2019)."Assessing the performance of global hydrological models for capturing peak river flows in the Amazon basin"(PDF).
  8. ^"Waters". Amazon Waters. 28 May 2014. Retrieved10 October 2017.
  9. ^abPenn, James R (2001).Rivers of the World: A Social, Geographical and Environmental Sourcebook. Santa Barbara: ABC Clio.
  10. ^PARNA de Anavilhanas (in Portuguese), ISA: Instituto Socioambiental, retrieved2016-04-30{{citation}}: CS1 maint: publisher location (link)
  11. ^ab"PLANO ESTADUAL DE RECURSOS HÍDRICOS DO AMAZONAS, (PERH/AM) - RT 03 - DIAGNÓSTICO, PROGNÓSTICO E CENÁRIOS FUTUROS DO RECURSOS HÍDRICOS DO ESTADO - TOMO III"(PDF). Jan 2019. Archived fromthe original(PDF) on 2021-05-06. Retrieved2021-10-03.
  12. ^abcdefghi"Amazon".
  13. ^Emilio, Mayorga; Miles, G. Logsdon; Maria Victoria, R. Ballester; Jeffrey, E. Richey (2005)."Estimating cell-to-cell land surface drainage paths from digital channel networks, with an application to the Amazon basin".Journal of Hydrology:167–182.doi:10.1016/j.hydrol.2005.03.023.
  14. ^"SGB-CPRM".
  15. ^abcdJosyane, Ronchail (2011)."Assessment of different precipitation datasets and their impacts on the water balance of the Negro River basin".Journal of Hydrology.404 (3–4):304–322.Bibcode:2011JHyd..404..304G.doi:10.1016/j.jhydrol.2011.04.037.
  16. ^Théry, Hervé; Maurence, Pascale (1997).HYDROLOGIE DU BASSIN AMAZONIEN(PDF).ISBN 2-7011-1532-9.
  17. ^Church, George Earl (1911b)."Orinoco" . InChisholm, Hugh (ed.).Encyclopædia Britannica. Vol. 20 (11th ed.). Cambridge University Press. pp. 275–276.
  18. ^Daum, Andreas W. (2024).Alexander von Humboldt: A Concise Biography. Trans. Robert Savage. Princeton, N.J.: Princeton University Press. p. 69.ISBN 978-0-691-24736-6.
  19. ^Huber, Otto and Wurdack, J. J. (1984), History of botanical exploration in Territorio Federal Amazonas, Venezuela (Smithsonian contributions to botany; City of Washington: Smithsonian Institution Press) iii, 83 p.
  20. ^"Graham Clarke".The Daily Telegraph. 2007-10-07. Retrieved2008-07-14.
  21. ^abHales, J., and P. Petry (2013).Rio NegroArchived 2017-12-01 at theWayback Machine. Freshwater Ecoregions of the World. Retrieved 12 February 2013
  22. ^Staeck, W.; Schindler, I. (2015)."Description of a new Heros species (Teleostei, Cichlidae) from the Rio Orinoco drainage and notes on Heros severus Heckel, 1840"(PDF).Bulletin of Fish Biology.15 (1–2):121–136. Archived fromthe original(PDF) on 2020-03-28. Retrieved2017-01-28.
  23. ^"Rio Negro : pasodoble - Stare Melodie".Stare Melodie - przecudny zgrzyt ze starych płyt (in Polish). Retrieved2025-08-26.

References

[edit]
  • Goulding, M., Carvalho, M. L., & Ferreira, E. J. G. (1988).Rio Negro, Rich Life in Poor Water : Amazonian Diversity and Foodchain Ecology as seen through Fish Communities. The Hague: SPB Academic Publishing.ISBN 90-5103-016-9
  • Saint-Paul, U., Berger, U., Zuanon, J., Villacorta Correa, M. A., García, M., Fabré, N. N., et al. (2000). "Fish communities in central Amazonian white- and blackwater floodplains,"Environmental Biology of Fishes, 57(3), 235–250.
  • Sioli, H. (1955). "Beiträge zur regionalen Limnologie des Amazonasgebietes. III. Über einige Gewässer des oberen Rio Negro-Gebietes."Arch. Hydrobiol., 50(1), 1-32.
  • Wallace, A. R. (1853).A narrative of travels on the Amazon and Rio Negro, with an account of the native tribes, and observations on the climate, geology, and natural history of the Amazon Valley. London: Reeve.
  • Wright, R. (2005).História indígena e do indigenismo no Alto Rio Negro. São Paulo, Brazil: UNICAMP & Instituto Socioambiental.ISBN 85-7591-042-6.
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