Bordeaux port de la lune 01.jpg
The Garonne (French: Garonne, IPA: ; in Occitan, Catalan, and Spanish: Garona; Latin: Garumna or Garunna) is a river in southwest France and northern Spain, with a length of 602 kilometres (374 mi). It flows into the Atlantic Ocean at Bordeaux.

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

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 / 42.709494°N 0.945398°E / 42.709494; 0.945398), the Ratera-Saboredo cirque 42°36′26″N 0°57′56″E / 42.607295°N 0.965424°E / 42.607295; 0.965424), or the slopes of Pic Aneto (Salterillo-Barrancs ravine 42°38′59″N 0°40′06″E / 42.6498°N 0.6683°E / 42.6498; 0.6683 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. The Ratera-Saboredo cirque has been pointed by many researchers as the origin of the Garonne.

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 / 42.6666°N 0.6669°E / 42.6666; 0.6669) 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. 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 / 42.68092°N 0.7077°E / 42.68092; 0.7077) in the Artiga de Lin on the other side of the mountain. 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).

This page was last edited on 30 January 2018, at 03:17.
Reference: under CC BY-SA license.

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