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The erupting lava met the water of the Indian Ocean during the August 2004 eruption. Video of a lava flow in August 2019 2004 eruption Animated map of eruptions between 1972 and 2000. Most eruptions of Piton de la Fournaise are of the Hawaiian style : fluid basaltic lava flowing out with fire fountaining at the vent.
The Réunion hotspot is a volcanic hotspot which currently lies under the island of Réunion in the Indian Ocean. The Chagos-Laccadive Ridge and the southern part of the Mascarene Plateau are volcanic traces of the Réunion hotspot. [1] The hotspot is believed to have been active for over 65 million years.
It has erupted more than 100 times since 1640, and is under constant monitoring, most recently erupting on 2 July 2023. [40] During another eruption in April 2007, the lava flow was estimated at 3,000,000 m 3 (3,900,000 cu yd) per day. [41] The hotspot that fuels Piton de la Fournaise also created the islands of Mauritius and Rodrigues.
Commerson Crater is a caldera in the mountains of Réunion, an overseas department of France.Located in the municipal territory of Saint-Joseph, it is part of the Piton de la Fournaise, a shield volcano on the eastern end of Réunion Island, but is located outside of the Enclos Fouqué, the volcano's most recent caldera.
Mandatory evacuation orders were issued on St. Vincent on Friday after a hurricane erupted.
High 3 He/ 4 He ratios of the main pulse of the eruption are often seen in magmas with mantle plume origin. [31] The area of long-term eruption (the hotspot), known as the Réunion hotspot, is suspected of both causing the Deccan Traps eruption and opening the rift that separated the Mascarene Plateau from India.
Kilauea, one of the world's most active volcanoes, began erupting around 2:30 a.m. local time, according to the U.S. Geological Survey.
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