Piton de la Fournaise in the context of Déodat Gratet de Dolomieu


Piton de la Fournaise in the context of Déodat Gratet de Dolomieu

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⭐ Core Definition: Piton de la Fournaise

Piton de la Fournaise (French: [pitɔ̃ la fuʁnɛz]; English: "Peak of the Furnace") is a shield volcano on the eastern side of Réunion island, a French overseas department and region, in the Indian Ocean. It is currently one of the most active volcanoes in the world, along with Kīlauea in the Hawaiian Islands, Stromboli and Etna in Italy and Mount Erebus in Antarctica. A previous eruption began in August 2006 and ended in January 2007. The volcano erupted again in February 2007, on 21 September 2008, on 9 December 2010, which lasted for two days, and on 1 August 2015. The most recent eruption began on 15 September 2022. The volcano is located within Réunion National Park, a World Heritage Site.

Residents of Réunion sometimes refer to Piton de la Fournaise simply as le Volcan ("the Volcano"). It is a major tourist attraction.

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👉 Piton de la Fournaise in the context of Déodat Gratet de Dolomieu

Dieudonné Sylvain Guy Tancrède de Gratet de Dolomieu usually known as Déodat de Dolomieu (French pronunciation: [deɔda dɔlɔmjø]; 23 June 1750 – 28 November 1801) was a French geologist. The mineral and the rock dolomite and the largest summital crater on the Piton de la Fournaise volcano were named after him.

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Piton de la Fournaise in the context of Satellite cone

A parasitic cone (also adventive cone, satellite cone, satellitic cone or lateral cone) is the cone-shaped accumulation of volcanic material not part of the central vent of a volcano. It forms from eruptions from fractures on the flank of the volcano. These fractures occur because the flank of the volcano is unstable. Eventually, the fractures reach the magma chamber and generate eruptions called flank eruptions, which, in turn, produce a parasitic cone.

A parasitic cone can also be formed from a dike or sill cutting up to the surface from the central magma chamber in an area different from the central vent.

View the full Wikipedia page for Satellite cone
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