The name derives from Garumna, a Latinized version of the Aquitanian name meaning "stony river".
Geography
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. 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 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. Surfers and jet skiers could ride the tidal bore at least as far as the village of Cambes, 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. 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.
The European sea sturgeon, also known as the Atlantic sturgeon or common sturgeon, is now a Critically Endangered species status. This species of sturgeon can reach a length of, weigh up to and can reach an age of 100 years. Previously found on most coasts of Europe, it has now become so rare that they only breed in the Garonne river basin in France. 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. .
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. From the ocean, ships pass through the Gironde estuary up to the mouth of the Garonne. Ships continue on the tidal river Garonne up to the Pont de Pierre 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.
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;
Flood of the Garonne from 1930, breaking of the dike in Thivras 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. 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. 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, 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.
