Chaîne des Puys

Chaîne des Puys
View of the Chaîne des Puys from Puy de Dôme
Highest point
Elevation	max. 1,464 m (4,803 ft) at Puy de Dôme
Coordinates	45°30′N 2°48′E / 45.5°N 2.8°E / 45.5; 2.8
Geography
Chaîne des Puys Location of Chaîne des Puys
Location	Auvergne-Rhône-Alpes, France
Parent range	Massif Central
Geology
Age of rock	From 7,000 to 95,000 years
Mountain type	cinder cones, lava domes, and maars
Last eruption	4040 BCE ± 150 years
UNESCO World Heritage Site
Official name	Chaîne des Puys - Limagne fault tectonic arena
Type	Natural
Criteria	(viii)
Designated	2018
Reference no.	1434
State Party	France
Region	Western Europe

The Chaîne des Puys (French: [ʃɛn de pɥi]) is a north-south oriented chain of cinder cones, lava domes, and maars in the Massif Central of France. The chain is about 40 km (25 mi) long, and the identified volcanic features include 48 cinder cones, eight lava domes, and 15 maars and explosion craters.^[1] Its highest point is the lava dome of Puy de Dôme, located near the middle of the chain, which is 1,465 m (4,806 ft) high.^[1] The name of the range comes from a French term, puy, that refers to a volcanic mountain with a rounded profile. A date of 4040 BCE is usually given for the last eruption of a Chaîne des Puys volcano.^[2]

The location became a World Heritage site in 2018.^[3]

Formation[]

The chain began to form approximately 95,000 years ago, and the volcanic activity that formed the range stopped about 10,000 years ago.^[1] The majority of the cones were formed by Strombolian eruptions, and these cones usually have well-defined summit craters. Some have nested craters, and others show broken rims where lava poured through.^[1]

In contrast, Puy de Dôme was created by a Peléan eruption; this type of eruption is characterized by long dormant periods periodically interrupted by sudden, extremely violent eruptions.^[1]

Future eruptions at the Chaîne des Puys are possible and would result in the formation of new mountains.^[4]

Research[]

Before 1750 and the chain's identification as volcanic, the Puys were rumored to be man-made mounds of mining waste or Roman forge furnaces.^[5]

The chain was the subject of the pioneering research of English geologist George Julius Poulett Scrope, starting in the 1820s. In 1827 he published his Memoir on the Geology of Central France, including the Volcanic formations of Auvergne, the Velay and the Vivarais, which was later re-published in a revised and somewhat more popular form in The Geology and extinct Volcanos of Central France in 1858. These books were the first widely published descriptions of the Chaîne des Puys, and the analysis therein laid the foundation for many of the basic principles of volcanology.^{[citation needed]}

References[]

Bibliography[]

Wikimedia Commons has media related to Chaîne des Puys.

• Scrope, George Poulett (1858). The Geology and extinct Volcanos of Central France. J. Murray, London. pp. 258. ISBN 0-405-10459-6. (reprinted in 1978 by Arno Press)
• Scarth, Alwyn; Tanguy, Jean-Claude (2001). Volcanoes of Europe. Oxford University Press. pp. 243 pp. ISBN 0-19-521754-3.
• Cattermole, Peter (2001). Auvergne (Classic Geology in Europe 2). Terra Publishing. pp. 176 pp. ISBN 1-903544-05-X.
• "Chaîne des Puys". Global Volcanism Program. Smithsonian Institution.
• Boivin Pierre; et al. (2004). Volcanologie de la Chaîne des Puys, Massif Central Français. Clermont-Ferrand: Parc Naturel Régional des Volcans d'Auvergne. OCLC 634970268.