Garonne

The Garonne (/ɡəˈrɒn, ɡæˈ-/, also US: /ɡɑːˈrɔːn/, French: [ɡaʁɔn]; Occitan, Catalan, and Spanish: Garona, Occitan pronunciation: [ɡaˈɾunɔ, ɡaˈɾɔnɔ]; Latin: Garumna[1][2] or Garunna) is a river in southwest France and northern Spain. It flows from the central Spanish Pyrenees to the Gironde estuary at the French port of Bordeaux. Its length is 529 km (329 mi),[3] of which 47 km (29 mi) is in Spain (Val d'Aran);[4] this extends to 602 km (374 mi) if the Gironde estuary is included. Its basin area is 56,000 km2 (22,000 sq mi),[4] which extends to 84,811 km2 (32,746 sq mi) if the Dordogne, which also flows into the Gironde estuary, is included.

Garonne
The Garonne at Bordeaux
Map of the Garonne
Native nameGarona  (Occitan)
Location
CountriesFrance and Spain
Physical characteristics
Source 
 • locationPyrenees
 • coordinates42°36′26″N 0°57′56″E
 • elevation2,600 m (8,500 ft)
Mouth 
 • location
Gironde estuary,
Atlantic Ocean
 • coordinates
45°2′29″N 0°36′24″W
Length529 km (329 mi)
Basin size56,000 km2 (22,000 sq mi), or including Dordogne: 84,811 km2 (32,746 sq mi)
Discharge 
 • average650 m3/s (23,000 cu ft/s)

The Battle of the River Garonne was fought in 732 beside the river near Bordeaux.

Etymology

The name derives from Garumna, a Latinized version of the Aquitanian name meaning "stony river".

Geography

Sources
150º Panorama of the Aran Valley from the Beret Plateau, showing the Ruda-Garona and Beret-Garona confluence. In Vielha the Garonne turns westward (out of sight), and after 12 kilometres (7 mi) receives water from the Joèu (Pic Aneto).
The Main Lake of Saboredo and Pic de Saboredo, the head of the Garonne valley
The water from Barrancs and Escaleta ravines disappears into the ground at Forau de Aigualluts.

The Garonne's headwaters are to be found in the Aran Valley in the Spanish Pyrenees, though three different locations have been proposed as the true source: the Uelh deth Garona at Plan de Beret (42°42′34″N 0°56′43″E), the Ratera-Saboredo cirque 42°36′26″N 0°57′56″E), or the slopes of Pic Aneto (Salterillo-Barrancs ravine 42°38′59″N 0°40′06″E according to the season).

The Uelh deth Garona at 1,862 metres (6,109 ft) above sea level has been traditionally considered as the source of the Garonne. From this point a brook (called the Beret-Garona) runs for 2.5 kilometres (1.6 mi) until the bed of the main upper Garonne valley. The river runs for another 38 kilometres (24 mi) until the French border at Pont de Rei, 40.5 kilometres (25.2 mi) in total.

The Ratera-Saboredo cirque is the head of the upper Garonne valley, and its upper lake at 2,600 metres (8,500 ft) above sea level is the origin of the Ruda-Garona river, running for 16 kilometres (9.9 mi) until the confluence with the Beret-Garona brook, and another 38 kilometres (24 mi) until the French border at Pont del Rei, 54 kilometres (34 mi) in total. At the confluence, the Ruda-Garona carries 2.6 cubic metres per second (92 cu ft/s) of water.[5][6] The Ratera-Saboredo cirque has been pointed by many researchers as the origin of the Garonne.[7][8][9][10]

The third thesis holds that the river rises on the slopes of Pic Aneto at 2,300 metres (7,500 ft) above sea level and flows by way of a sinkhole known as the Forau de Aigualluts (42°40′00″N 0°40′01″E) through the limestone of the Tuca Blanca de Pomèro and a resurgence in the Val dera Artiga above the Aran Valley in the Spanish Pyrenees.[11] This underground route was suggested by the geologist Ramond de Carbonnières in 1787, but there was no confirmation until 1931, when caver Norbert Casteret poured fluorescein dye into the flow and noted its emergence a few hours later 4 kilometres (2.5 mi) away at Uelhs deth Joèu ("Jove's eyes" 42°40′51″N 0°42′28″E) in the Artiga de Lin on the other side of the mountain.[12][13][14] From Aigualluts to the confluence with the main river at the bed of the upper Garonne valley at 800 metres (2,600 ft) above sea level, the Joèu has run for 12.4 kilometres (7.7 mi) (16 kilometres more to get to the French border), carrying 2.16 cubic metres per second (76 cu ft/s) of water, while the main river is carrying 17.7 cubic metres per second (630 cu ft/s).[5][6][15]

Despite the lack of universal agreement upon definition for determining a stream's source, the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution agree that a stream's source should be considered as the most distant point (along watercourses from the river mouth) in the drainage basin from which water runs.[16][17][18][19][20]

The Ratera-Saboredo cirque is the "most distant point (along watercourses from the river mouth) in the drainage basin from which water runs",[21][22] and the source of the Garonne, according to the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution convention upon determining a stream's source.

Course

The Garonne follows the Aran Valley northwards into France, flowing via Toulouse and Agen towards Bordeaux, where it meets the Gironde estuary. The Gironde flows into the Atlantic Ocean (Bay of Biscay). Along its course, the Garonne is joined by three other major rivers: the Ariège, the Tarn, and the Lot. Just after Bordeaux, the Garonne meets the Dordogne at the Bec d'Ambès, forming the Gironde estuary, which after approximately 100 kilometres (62 mi) empties into the Atlantic Ocean. Other tributaries include the Save and the Gers.

The Garonne is one of the few rivers in the world that exhibit a tidal bore.[23][24][25] Surfers and jet skiers could ride the tidal bore at least as far as the village of Cambes, 120 kilometres (75 mi) from the Atlantic, and even further upstream to Cadillac, although the tidal bore appears and disappears in response to changes in the channel bathymetry. In 2010 and 2012, some detailed field studies were conducted in the Garonne's Arcins channel between Arcins Island and the right bank close to Lastrene township.[23] A striking feature of the field data sets was the large and rapid fluctuations in turbulent velocities and turbulent stresses during the tidal bore and flood flow.[24][25][26]

European sea sturgeon conservation
The European sea sturgeon (Acipenser sturio)

The European sea sturgeon (Acipenser sturio), also known as the Atlantic sturgeon or common sturgeon, is now a Critically Endangered species (IUCN) status.[27] This species of sturgeon can reach a length of 6 m (20 ft), weigh up to 400 kg (880 lb) and can reach an age of 100 years.[28] Previously found on most coasts of Europe, it has now become so rare that they only breed in the Garonne river basin in France.[27] Conservation projects are under way to save this fish from extinction via species reintroduction from aquaculture, with the first releases having been made in 1995.[27]

The Garonne at Toulouse

Towns along the river

Main tributaries

Following the flow of the river:

The Garonne plays an important role in inland shipping. The river not only allows seagoing vessels to reach the port of Bordeaux but also forms part of the Canal des Deux Mers, linking the Mediterranean Sea and the Atlantic Ocean.

Seagoing vessels may navigate as far inland as Bordeaux on the Garonne.

From the ocean, ships pass through the Gironde estuary up to the mouth of the Garonne (to the right of the Dordogne when sailing upstream). Ships continue on the tidal river Garonne up to the Pont de Pierre (stone bridge) in Bordeaux. Inland vessels continue upstream to Castets-en-Dorthe, where the Canal de Garonne joins the river. Prior to the building of the Canal lateral à la Garonne, between 1838 and 1856, shallow-draught boats used the Garonne itself as far as Toulouse. However, navigation on the upper river was very uncertain, and this stretch of the river is no longer considered navigable. Instead the lateral canal takes boats through 53 locks to the town of Toulouse, where the canal meets the Canal du Midi.[29]

Hydrography

The upstream part of the river, upstream from Toulouse depends primarily on snow and snow melt. The lower/downstream part is rain fed as well as its main tributaries.

The Garonne also feeds several channels/canals:

  • The Saint-Martory canal - Saint-Martory water intake takes 10 m3/s from the river;[30]
  • The canal latéral à la Garonne - with the water intake in Toulouse by the Brienne canal.

SANDRE assigns to the Garonne a hydrographic identity number 0 --- 00000 and the generic code O --- 000014,15.

Floods of the Garonne

Flood of the Garonne from 1930, breaking of the dike in Thivras (Marmande)

In Toulouse, the Garonne has often been the cause of many floods, especially since its left bank is inhabited.

The earliest records of floods are from around 1177. It is also recorded to have flooded in 1220, 1258, 1430, 1523, 1536 and in 1589, 1608, 1658, 1673, 1675, 1709, 1712, 1727, 1750, 1772, 1788, 1804 and 1810. In 1772, the Garonne reached 8 meters 50.[31] In the recent centuries, in 1827, 1835, 1855 and 1856/7.

In Toulouse, in 1827, the water level of the Garonne rose four meters above the ordinary level and filled the arches of the Pont de Pierre and Pont Neuf.

In 1835, the Garonne rose to five meters above normal and 35 meters above the low water level and flowed through the four arcs of the Pont de Pierre.

Flood of the Garonne in 1835: 7,50 m at Toulouse Pont-Neuf

Flood of the Garonne in 1855: 7.25 m at Toulouse Pont-Neuf

Flood of the Garonne in 1875: 9,70 m to Toulouse Pont-Neuf (or 8m32 according to vigicrue).

Flood of the Garonne in 1879: 4,87 m at Toulouse Pont-Neuf

Flood of the Garonne in 1890: 3.30 m at Toulouse Pont-Neuf

Flood of the Garonne in 1900: 4,00 m in Toulouse Pont-Neuf

Flood of the Garonne in 1905: 4.24 m at Toulouse Pont-Neuf

Crete of 1927 in Aquitaine, particularly imposing after the confluence of the Garonne with the Lot (of which it remained raw reference), insignificant upstream18.

Flood of the Garonne in 1952: 4,57 m at Toulouse Pont-Neuf

Flood of the Garonne in 1977: 4,31 m in Toulouse Pont-Neuf

Flood of the Garonne in 2000: 4.38 m at Toulouse Pont-Neuf

Flood of the Garonne in 2004: 3,52 m at Toulouse Pont-Neuf

In 1777, the Garonne suffered an extraordinary flood to the point that the priest of Bourdelles took the trouble to retranscribe the event, at the end of the acts of the year, in the parish register of baptisms, marriages and deaths.

See also

References
  1. Smith, William (1850). A new classical dictionary of Greek and Roman biography, mythology, and geography. London: John Murray. p. 492. OCLC 223027795.
  2. Smith, William (1862). "GARUMNA". In Anthon, Charles (ed.). A New Classical Dictionary of Greek and Roman Biography, Mythology and Geography, partly based upon the Dictionary of Greek and Roman Biography and Mythology by William Smith [...]. Revised by Charles Anthon (revised ed.). New York: Harper (published 1895). p. 322. Retrieved 14 December 2019. GARUMNA (now Garonne), one of the chief rivers of Gaul, rises in the Pyrenees, flows northwest through Aquitania, and becomes a bay of the sea below Burdigala (now Bordeaux).
  3. Sandre. "Fiche cours d'eau - La Garonne (O---0000)".
  4. Le bassin versant de la Garonne, Syndicat Mixte d'Études & d'Aménagement de la Garonne
  5. "3". oph.chebro.es. Archived from the original on 2012-03-14.
  7. Salvador Rivas-Martínez (member of the Spanish Royal Academy of Sciences); Manuel Costa (Professor of the Universitat de Valencia) (1998). "Datos sobre la vegetación y bioclima del Valle de Arán". Acta Bot. Barcinon. 45: 473–499.
  8. Soler i Santaló; La Vall d'Aran. Guía monográfica de la comarca; pág. 12. Barcelona, 1916.
  9. Faura i Sans (M.); Sobre hidrología subterránea en los Pirineos Centrales de Aragón y Cataluña. Bol. de la Real Soc. de Hist. Nat, vom. XVI, pgs. 353-354. Madrid, 1916.
  10. Boletín del Centro Excursionista de Cataluña
  11. Reynolds, Kev (2001). Walks and Climbs in the Pyrenees. Milnthorpe, England: Cicerone Press. p. 208. ISBN 978-1-85284-328-1.
  12. Casteret, Norbert (1939). Ten Years Under the Earth. Mussey, Barrows (trans). London: J. M. Dent.
  13. Mapa topogràfic de Catalunya 1:100 000 (Map) (1st ed.). Institut Cartogràfic de Catalunya. § 1: Pirineu occidental.
  14. Lambert, Roger (1996). "A propos de la Garonne Supérieure". Géographie du cycle de l'eau (in French). Toulouse: Presses Universitaires du Mirail. p. 351. ISBN 978-2-85816-273-4. prouvant péremptoirement que la Garonne a sa vrai source et la plus importante dans les Monts Maudits, sur le versant Sud des Pyrénées ('proving conclusively that the Garonne has its true source, and the most important, in the Monts Maudits, on the southern slopes of the Pyrenees')
  15. "Archived copy". Archived from the original on 2010-11-17. Retrieved 2011-01-11.CS1 maint: archived copy as title (link)
  16. "Largest Rivers in the United States" (PDF). United States Geological Survey. Retrieved 24 October 2009.
  17. National Geographic News @ nationalgeographic.com
  18. The True Utmost Reaches of the Missouri
  19. "IBGE - Instituto Brasileiro de Geografia e Estatística". Archived from the original on 2008-09-28. Retrieved 2019-12-24.
  20. "Quest for the Missouri River Source, John LaRandeau, U.S. Army Corps of Engineers" (PDF). Archived from the original (PDF) on 2013-06-02. Retrieved 2011-01-11.
  21. Instituto Geográfico Nacional; Ministerio de FOmento. "Visor cartográfico del Instituto Geográfico Nacional". Instituto Geográfico Nacional de España. Retrieved 10 November 2012.
  22. s - Géoportail, le portail des territoires et des citoyens. "IGN France Cartes Topographie". Retrieved 10 November 2012.
  23. Chanson, H., Lubin, P., Simon, B., and Reungoat, D. (2010). Turbulence and Sediment Processes in the Tidal Bore of the Garonne River: First Observations. Hydraulic Model Report No. CH79/10, School of Civil Engineering, The University of Queensland, Brisbane, Australia, 97 pages. ISBN 978-1-74272-010-4.CS1 maint: multiple names: authors list (link)
  24. Simon, B., Lubin, P., Reungoat, D., Chanson, H. (2011). Turbulence Measurements in the Garonne River Tidal Bore: First Observations. Proc. 34th IAHR World Congress, Brisbane, Australia, 26 June-1 July, Engineers Australia Publication, Eric Valentine, Colin Apelt, James Ball, Hubert Chanson, Ron Cox, Rob Ettema, George Kuczera, Martin Lambert, Bruce Melville and Jane Sargison Editors. pp. 1141–1148. ISBN 978-0-85825-868-6.CS1 maint: multiple names: authors list (link)
  25. Chanson, Hubert; Reungoat, David; Simon, Bruno; Lubin, Pierre (December 2011). "High-frequency turbulence and suspended sediment concentration measurements in the Garonne River tidal bore". Estuarine, Coastal and Shelf Science. 95 (2–3): 298–306. Bibcode:2011ECSS...95..298C. CiteSeerX 10.1.1.692.2537. doi:10.1016/j.ecss.2011.09.012.
  26. Reungoat, D., Chanson, H., Caplain, B. (2012). Field Measurements in the Tidal Bore of the Garonne River at Arcins (June 2012). Hydraulic Model Report No. CH89/12, School of Civil Engineering, the University of Queensland, Brisbane, Australia, 121 Pages. ISBN 9781742720616.CS1 maint: multiple names: authors list (link)
  27. Gesner, J.; Williot, P.; Rochard, E.; Freyhof, J.; Kottelat, M. (2010). "Acipenser sturio". IUCN Red List of Threatened Species. 2010: e.T230A13040963. doi:10.2305/IUCN.UK.2010-1.RLTS.T230A13040963.en.
  28. Froese, Rainer and Pauly, Daniel, eds. (2005). "Acipenser sturio" in FishBase. 10 2005 version.
  29. Rolt, L. T. C. (1973). From Sea to Sea: An Illustrated History of the Canal du Midi. Grenoble, France: Euromapping. pp. 19–40. ISBN 978-2-910185-02-2.
  30. "Garonne Irrigation channels". Archived from the original on 2008-12-04. Retrieved 2018-08-13.
  31. Astrié, Théophile (1875). Les drames de l'inondation à Toulouse / Théophile Astrié Éditeur : Éditeur : Librairie centrale (Toulouse) Date d'édition : 1875 gallica.bnf.fr/ark:/12148/bpt6k5778575j. Librairie centrale (Toulouse): Arnaud et Labat (Paris).
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