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Continuing generally westward, the Rhône then receives the waters of the Valserine, enters the reservoir created by the Génissiat Dam, and is then joined by the Ain. Mouth of the Rhône Reaching Lyon , the most populous city on its course, the Rhône receives its biggest tributary, the Saône , with an average flow of 473 m 3 /s (16,700 cu ft ...
Rhone Glacier at Gletsch in 1900. Rhone watershed upstream from Lake Geneva. The Rhône rises in the St. Gotthard massif in the Swiss Alps. [1] It is formed by the melting of the Rhône glacier, and flows through the long valley of the same name through the canton of Valais, marking the border with the canton of Vaud in the Chablais region before joining Lake Geneva in the commune of Port ...
Old European hydronymic map for the root *al-, *alm-Old European (German: Alteuropäisch) is the term used by Hans Krahe (1964) for the language of the oldest reconstructed stratum of European hydronymy (river names) in Central and Western Europe. [1] [note 1]
Klepáč – one of six places in Europe where three watersheds meet Rhine–Danube watershed marker near Weitnau, Germany European watershed marker (Lviv Oblast, 2009). The divide continues northwards along the Albula Alps to Julier Pass, Albula Pass and Flüela Pass south of Davos, between the catchment area of the Rhine, which empties into the North Sea via the Netherlands, and the Danube ...
In French, rivers are traditionally classified either as fleuves when they flow into the sea (or into a desert or lake), or as rivières when they flow into another river. The fleuves are shown in bold. For an alphabetical overview of rivers of France, see the category Rivers of France.
The bridge had great strategic importance as when first built it was the only fixed river crossing between Lyon and the Mediterranean Sea. It was also the only river crossing between the Comtat Venaissin, an enclave controlled by the Pope, and France proper under the authority of the kings of France. As such, it was closely guarded on both ...
The river Rhône forks into two branches just upstream of Arles, forming the Camargue delta. Because the Camargue is for a large part administratively part of Arles, the commune as a whole is the largest commune in Metropolitan France in terms of territory. But its population numbers only slightly more than 50,000.
The Massif Central is an old massif, formed during the Variscan orogeny, consisting mostly of granitic and metamorphic rocks.It was powerfully raised and made to look geologically younger in the eastern section by the uplift of the Alps during the Paleogene period and in the southern section by the uplift of the Pyrenees.