Somme (river)(Redirected from Somme River)
|Somme (La Somme)|
|- elevation||85 m (279 ft)|
|Length||245 km (152 mi)|
|Basin||6,550 km2 (2,529 sq mi)|
|- average||35 m3/s (1,236 cu ft/s)|
Course in Northern France
Topographic map of the Somme basin
The river is 245 km (152 mi) long, from its source in the high ground of the former Forest of Arrouaise at Fonsommes near Saint-Quentin, to the Bay of the Somme, in the English Channel. It lies in the geological syncline which also forms the Solent. This gives it a fairly constant and gentle gradient where several fluvial terraces have been identified.
The river gave its name to the infamous Battle of the Somme during World War I, lasting from July to November 1916, resulting in more than a million casualties. The Somme also featured prominently in other historical campaigns. In 1066, the invasion fleet of William the Conqueror assembled in the Bay of the Somme at Saint-Valery-sur-Somme. The river featured in the 1346 withdrawal of Edward III of England's army, which forded the river at the battle of Blanchetaque during the campaign which culminated in the Battle of Crécy. Crossing the river also featured prominently in the campaign which led to the Battle of Agincourt in 1415. The great battles which finally stopped the German advance in the Spring Offensive of 1918 were fought around the valley of the Somme in places like Villers Bretonneux, which marked the beginning of the end of the war.
Départements and towns along the riverEdit
The river is characterized by a very gentle gradient and a steady flow. The valley is more or less steep-sided but its bottom is flat with fens and pools. These characteristics of steady flow and flooded valley bottom arise from the river's being fed by the ground water in the chalk basin in which it lies. At earlier, colder times, from the Günz to the Würm (Beestonian or Nebraskan to Devensian or Wisconsinian) the river has cut down into the Cretaceous geology to a level below the modern water table. The valley bottom has now therefore, filled with water which, in turn, has filled with fen. This picture, of the source of the Somme in 1986, shows it when the water table had fallen below the surface of the chalk in which the aquifer lies. Here, the flow of water had been sufficient to keep fen from forming.
One of the fens, the Marais de l'Île is a nature reserve in the town of St.Quentin. The traditional market gardens of Amiens, the Hortillonages are on this sort of land but drained. Once exploited for peat cutting, the fen is now used for fishing and shooting
The construction of the Canal de la Somme began in 1770 and reached completion in 1843. It is 156 km (97 mi) long, beginning at St.Simon and opening into the Bay of the Somme. From St.Simon to Froissy (near Bray sur Somme, south of Albert), the canal is alongside the river. Thence to the sea, the river is partly river and partly navigation. From Abbeville, it is diverted through the silted, former estuary, to Saint-Valery-sur-Somme, where the maritime canal, once called the canal du Duc d'Angoulême enters the English Channel.
The St Quentin Canal, famous for the 1918 battle, links the Somme to northern France and Belgium and southward to the Oise. The Canal du Nord also links the Somme to the Oise, at Noyon, thence to Paris.
In 2001, the Somme valley was affected by particularly high floods, which were in large part due to a rise in the water table of the surrounding land.
Monthly flow rates (mean over 43 years)Edit
Catchment area 5,560 km2 (2,150 sq mi).
Flow rates at Hangest-sur-SommeEdit
Daily flow rates compared with mean rates for the time of year at Hangest-sur-Somme (m³/s). Catchment area 4,835 km2 (1,867 sq mi).
- for the year -
Flow rates at PéronneEdit
Mean flow rates monthly and daily at Péronne (m³/s). Catchment area 1,294 km2 (500 sq mi).
- for the year -
- Gargani J.; Stab O; Cojan I.n Brulhet J. (2006). "Modelling the long-term fluvial erosion of the river Somme during the last million years.". Terra Nova. 18 (2): 118–129. doi:10.1111/j.1365-3121.2006.00671.x.
- Delattre, Ch., Mériaux, E. and Waterlot, M. Guides Géologiques Régionaux: Région du Nord, Flandre Artois Boulonnais Picardie (1973)