Puy De Pariou
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Puy De Pariou
The Puy de Pariou, also known as Puy Pariou or Le Pariou, is a volcano located in the Chaîne des Puys, in the Massif Central region. It is formed by the overlay of two strombolian cones and a tuff ring; it produced three lava flows during its eruptive history. Geography The Puy de Pariou is located about 10 km at the west of Clermont-Ferrand and a little more than 2 km from Orcines, at the south of the road that crosses the Col des Goules. The Puy des Goules is less than 400 meters north; the Cliersou, the Grand Suchet and the Petit Suchet are situated a few hundred meters west and south-west, and the Puy de Dôme lies about 1.5 km south. Topography Its highest point reaches 1,209 meters, 250 meters above the crystalline basement that forms the surrounding plain. It has a typical volcano shape of strombolian type, and its crater is formed by two craters, one nested in the other. The central crater, which is the highest and most recent, has an almost pe ...
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Puy De Pariou 2001-07-30
Puy () is a geology, geological term used locally in the Auvergne (région), Auvergne, France for a volcano, volcanic hill. The word derives from the Franco-Provençal language, Provençal ''puech'', meaning an isolated hill, coming from Latin ''podium'', which has given also ''puig'' in Catalan, ''poggio'' in Italian, ''poio'' in Galician and Portuguese. Most of the puys of central France are small cinder cones, with or without associated lava, whilst others are domes of trachyte, trachytic rock, like the of the Puy-de-Dôme (mountain), Puy-de-Dôme. The puys may be scattered as isolated hills, or, as is more usual, clustered together, sometimes in lines. The chain of puys in central France probably became extinct in late prehistoric time. Other volcanic hills more or less like those of Auvergne are also known to geologists as puys; examples may be found in the Eifel and in the small cones on the Bay of Naples, whilst the relics of puys denuded by erosion are numerous in the S ...
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