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마지막 업데이트: 3월 6, 2026
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The Tchier de Borée is a contemporary artwork situated in the heart of the volcanic landscapes of the Boutières region. Created in 2008 by Fabienne Versé and Serge Boyer, this megalithic installation comprises 70 standing stones arranged in a circle 80 meters in diameter. Each stone bears a symbol or message: runes, astrological signs, natural elements (air, water, fire, earth), winds, mythology… The word “Tchier” (from the local dialect) means “pile of stones”: a tribute to stone, time, and the memory of the land. https://www.montagnedardeche.com/patrimoine-culturel/tchier-de-boree-2634/
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One of the most beautiful viewpoints in the region with the village of Borée, at the foot of the Sucs and Mont Mézenc
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Mont Gerbier-de-Jonc is one of the highest peaks of the Monts d'Ardèche in the south-eastern Massif Central. The mountain itself is a striking, extinct volcanic cone with a good view over the Massif Central. The ascent and descent require some fitness and good footwear. There are a few short climbing rocks that cannot be avoided. But the view is worth it.
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Contemporary work by Fabienne and Serge Boÿer: Glypheins sculptors. 70 stones engraved with symbols, myths of the country of Boutières, allegory. The cultural history of the high country of Boutières is told through nine themes: memory, reflection and philosophers, secrets and desires, travelers and pilgrims, astronomers and cartographers.
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La Volane is one of the prettiest rivers in the Ardèche. Here, you can take a short break, lying by the water, and cool off in the clear water.
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The Suc de Sara is a summit of volcanic origin located at 1,521 m. No surface volcanic activity has taken place on this peak, but it was created as a result of an underground magma chamber 6-8 million years ago. Fragments of concentric rings are all that remain to suggest its existence. From this summit, the view is magnificent.
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The Suc de Sara is a summit of volcanic origin located at 1,521 m. No surface volcanic activity has taken place on this peak, but it was created as a result of an underground magma chamber 6-8 million years ago. Fragments of concentric rings are all that remain to suggest its existence. From this summit, the view is magnificent.
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