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Geological Formation

Chaine des Puys

Volcanic Formations

The Chaine des Puys is a volcanic field about 40 kilometers long running north to south through France's Massif Central, made up of 48 cinder cones, eight lava domes and 15 maars and explosion craters. Its highest point, Puy de Dome, reaches 1,465 meters, and the chain's name comes from a regional French word for a rounded volcanic hill. The field was active from roughly 95,000 years ago until about 10,000 years ago, with its most recent eruption dated to around 4040 BC. In 2018 UNESCO recognized the Chaine des Puys, together with the Limagne fault, as a World Heritage Site for its clear evidence of continental rifting and plate tectonics, and although quiet for millennia, future volcanic activity there remains theoretically possible.

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Protected Status
UNESCO World Heritage Site 1
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Volcanism, Processes
Source Chaîne des Puys (Wikipedia)

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Source Chaîne des Puys (Wikipedia)
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Sources
1. Wikidata: Chaine des Puys
  • Wikidata Q1068630, class allow-list match (w-wdresolver-0926)
  • became a UNESCO World Heritage Site in 2018
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Chaîne des Puys (Wikipedia)
  • In Discipline: Volcanology, Lead section (in-discipline Volcanology)
    The Chaîne des Puys (French: [ʃɛːn de pɥi]; lit. 'Chain of the Puys') is a north-south oriented volcanic field, about 40 kilometres (25 mi) long, comprising 48 cinder cones, eight lava domes, and 15 maars and explosion craters, in the Massif Central of France.
  • Caused By: Volcanism, Lead section (caused-by Volcanism)
    The Chaîne des Puys (French: [ʃɛːn de pɥi]; lit. 'Chain of the Puys') is a north-south oriented volcanic field, about 40 kilometres (25 mi) long, comprising 48 cinder cones, eight lava domes, and 15 maars and explosion craters, in the Massif Central of France.
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