Ardèche (river)


The Ardèche is a long river in south-central France, a right-bank tributary of the River Rhône. Its source is in the Massif Central, near the village of Astet. It flows into the Rhône near Pont-Saint-Esprit, north-west of Orange. The river gives its name to the French department of Ardèche.
The valley of the Ardèche is very scenic, in particular a section known as the Ardèche Gorges. The walls of the river here are limestone cliffs up to high. A kayak and camping trip down the gorge is not technically difficult and is very popular in the summer. The most famous feature is a natural stone arch spanning the river known as the Pont d'Arc.

Geography

The source of the river lies at above sea level in the Vivarais, near the Col de la Chavade, in the forest of Mazan in the commune of Astet. After the towns of Aubenas and Ruoms, it collects the Chassezac and the Beaume and plunges into its famous gorge below Vallon-Pont-d'Arc. It flows into the Rhône at Pont-Saint-Esprit.

Departments and communes

The Ardèche flows through the following departments and communes:
The most important tributaries and subtributaries to the Ardèche River include:

Hydrology

The river has an average discharge of but experiences severe floods, called "coups de l'Ardèche", in spring and autumn and periods of very low water in summer. During flood events in 1827, 1890, and 1924, it reached and the water level rose to a record in the gorge.
Despite the Ardèche's short length, the flow of the river at is relatively high—higher than the Gardon at, the Cèze, the Hérault, or the Agout —major rivers south of the Massif Central but much longer.

Rates of flow at Saint-Martin d'Ardèche

The inter-annual average flow of the Ardèche was observed and calculated over a period of 26 years at Saint-Martin d'Ardèche. It amounted to for a surface basin of —i.e. the vast majority of its watershed of. The river has seasonal fluctuations: a typical flow around the Cevennes, with high water in autumn and winter being double the normal, brings the average monthly flow at the first peak of in October then, after falling to in December, a new peak occurs from in January–March. A rapid decline in flow rate follows ending in a dry period in July–August resulting in a decrease of the average monthly rate to the level of in July.
The VCN3 can drop to in a dry year.
Floods can be extremely important. The Qix 2 and Qix 5 are respectively which is high. QIX 10 is while QIX 20 and QIX 50 respectively rise to.
The maximum instantaneous flow recorded in Saint-Martin d'Ardèche has been , while the maximum recorded daily rate was.
The runoff curve number flowing into the catchment of the river is annually, which is very high. The specific flow reaches 28.3 litres per second per square kilometre of the catchment.

Flows of waterways in the Ardèche catchment

Voice server

The prefecture of Ardèche has provided a voice server since June 2005 whose objective is to regularly disseminate information messages to allow monitoring of any significant event that might trigger a civil security crisis or standby alert. Precise information on the evolution of any flood is provided.

Peculiarity

The Ardèche receives water from the Loire river via the "La Palisse" flood barrier and the Lake d'Issarlès. Effectively, the water is collected to feed the EDF hydroelectric plant at Montpezat-sous-Bauzon and is subsequently piped into the Fontaulière river, a tributary of the Ardèche, near the town of Aubenas.

Hydronymy

Several ancient inscriptions about a college of nautes in associated rivers have been discovered in the Gard. It is possible that the two rivers concerned are the Ardèche and the Ouvèze.
The identification of these two rivers is still pending. However, if it does involve the Ardèche river, the spellings Hentica, then Ardesca have been attested.

Protected areas

The Ardèche is protected along almost all of its course. These protected areas are: