Ardèche (French pronunciation:[aʁdɛʃ]; Occitan: Ardecha, pronounced[aɾˈdet͡ʃɔ]; Arpitan: Ardecha) is a department in Auvergne-Rhône-Alpes, Southeastern France. It is named after the river Ardèche and had a population of 328,278 as of 2019. Its prefecture is in Privas, but its largest city is Annonay.
The Montgolfier brothers – Joseph-Michel Montgolfier (French:[ʒozɛfmiʃɛlmɔ̃ɡɔlfje]; 26 August 1740 – 26 June 1810) and Jacques-Étienne Montgolfier ([ʒaketjɛnmɔ̃ɡɔlfje]; 6 January 1745 – 2 August 1799) – were aviation pioneers, balloonists and paper manufacturers from the communeAnnonay in Ardèche, France. They invented the Montgolfière-style hot air balloon, globe aérostatique, which launched the first confirmed piloted ascent by humans in 1783, carrying Jacques-Étienne.
Joseph-Michel also invented the self-acting hydraulic ram (1796) and Jacques-Étienne founded the first paper-making vocational school. Together, the brothers invented a process to manufacture transparent paper.
The Loire (/lwɑːr/LWAR, US also /luˈɑːr/loo-AR, French:[lwaʁ]; Occitan: Léger[ˈledʒe]; Arpitan: Lêre; Breton: Liger[ˈliːɡɛr]; Latin: Liger) is the longest river in France and the 171st longest in the world. With a length of 1,006 kilometres (625 mi), it drains 117,054 km (45,195 sq mi), more than a fifth of France's land, while its average discharge is only half that of the Rhône.
The name Cévennes comes from the GaulishCebenna. As of 1999, there were 165,707 inhabitants in the region, with 20,847 living inside the UNESCO protected zone. Inhabitants of the region are known as Cévenols, from the adjective Cévenol (fem. Cévenole).
Mont Gerbier de Jonc is a mountain of volcanic origin located in the Massif Central in France. It is made of a type of rock called phonolite. It rises to an altitude of 1,551 m (5,089 ft), and its base contains three springs that are the source of the Loire, France's longest river. It is the second most-visited site in the département of Ardèche, after the Ardèche Gorges.
Mont Gerbier de Jonc was formed 8 million years ago when a volcano erupted molten phonolite lava. The lava was too viscous to flow far and it cooled to form a lava dome of phonolite rock in the crater of the volcano. The lava dome has columnar jointing, which formed during cooling of the lava. The volcanic cone containing the lava dome was later eroded away, exposing the lava dome.