18-427: Fournaise (fr. "furnace", "blaze" or "bonfire") may refer to: Piton de la Fournaise , a volcano on the island of Reunion Maison Fournaise , a restaurant and museum near Paris Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Fournaise . If an internal link led you here, you may wish to change
36-532: A view over the northeast part of the caldera. A stairway path descends from the pass to the caldera floor. This path is closed for safety reasons during seismic events that may precede eruptions and during eruptions. White paint marks over rocks delimit a number of footpaths ascending the lava shield inside the caldera. The lower parts of the Grand Brûlé can be visited from the N2 highway. Lava flows that have crossed
54-413: A volume of 120 million cubic metres (4.2 billion cubic feet). The caldera collapse accompanied one of the largest eruptions of lava at the volcano in the past 100 years. An eruption began on 2 July 2023 at 8:30 a.m. local time. Volcanic activity is constantly monitored by geophysical sensors ( tiltmeters , extensometers , differential GPS receivers, etc.). The data from those various sensors
72-519: Is breached to the southeast towards the sea. The eastern flank of the volcano is unstable and is in the initial stages of failure. It will eventually collapse into the Indian Ocean and if it is a cataclysmic debris avalanche, it will generate a megatsunami . There is evidence of earlier failures on the submerged flanks and surrounding abyssal plain. The lower slopes are known as the Grand Brûlé ("Great Burn"). Most volcanic eruptions are confined to
90-644: 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. The uppermost section of the volcano is occupied by the Enclos Fouqué , a caldera 8 kilometres (5.0 mi) wide. High cliffs, known as remparts in French, form the caldera's rim. The caldera
108-468: Is over 530,000 years old, and for most of its history, its flows have intermingled with those from Piton des Neiges , a larger, older and heavily eroded inactive volcano which forms the northwest two-thirds of Réunion Island. There were three episodes of caldera collapses 250,000, 65,000 and 5,000 years ago. The volcano was formed by the Réunion hotspot , which is believed to have been active for
126-974: Is sent to the Piton de la Fournaise Volcano Observatory , located in Bourg-Murat , northwest of the volcano. The observatory, founded in 1978 following the Piton-Sainte-Rose flow, is operated by the Institut de Physique du Globe de Paris (Global Geophysics Institute of Paris), in association with CNRS and the University of Réunion. The OVPF often publishes reports on Piton de la Fournaise's current activity via their website in French. RIGIC (the Réunion Island Geological Information Center) takes this information and translates it into English for distribution to
144-429: The Grand Brûlé occasionally reach the sea. Piton de la Fournaise is one of the most active volcanoes in the world, with more than 150 recorded eruptions since the 17th century. Eruptions within the caldera do not cause much devastation, because the caldera is uninhabited, but little infrastructure exists apart from the highway. Lava flows are generally confined to the caldera. However, lava flows have been known to cross
162-456: The most precipitation produced by a tropical cyclone in a single location . Some beaches in the proximity of the volcano are greenish in color, due to olivine sand derived from picrite basalt lavas. The Grand Brûlé is formed from solidified lava flows accumulated over hundreds of thousands of years; the most recent ones are often the darkest and most vegetation-free, while older ones can be covered by dense natural vegetation. This volcano
180-601: The English-speaking scientific community. Procedures specify several levels of alert, which are decided by the prefect of Réunion on the basis of scientific reports: A forestry road followed by a track connects the highway of the plains in Bourg-Murat to the Pas de Bellecombe (Bellecombe Pass), where a parking lot and a snack bar are located. The Pas de Bellecombe is situated over the caldera rim cliffs and offers
198-1053: 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
SECTION 10
#1732790999281216-433: The N2 highway; areas where the road was destroyed by the eruption are signposted with the year of eruption after the road is rebuilt. In the early 2000s, the highway was destroyed one or more times a year; road engineering services then wait for the lava to cool off and build another stretch of road. For months after an eruption, the core of the lava flows can still be hot enough to steam in rainy weather. Eruptions outside of
234-623: The building. The front entrance was later cleared out, and the church was brought back into service under the name of Notre-Dame des Laves ("Our Lady of the Lavas"). In April 2007, the volcano erupted and produced an estimated 3,000,000 cubic metres (110 million cubic feet) of lava per day. During this eruption of 2007, an incremental caldera collapse of Dolomieu occurred at the volcano over more than nine days. The collapse displaced 0.8 km × 1.1 km (0.50 mi × 0.68 mi) of floor downward by 330 m (1,080 ft), with
252-408: The caldera can pose serious hazards to the population, but are rare. Only six eruptions outside of the caldera have been recorded, most recently in 1986. The village of Piton-Sainte-Rose was evacuated in 1977 before it was inundated by a lava flow which destroyed several buildings. The lava flow crossed the highway and surrounded the local church, entered the front door, then stopped without destroying
270-501: The caldera. Inside the caldera is a 400 metres (1,300 ft) high lava shield named Dolomieu. At the top of this lava shield are Bory Crater ( Cratère Bory ) and Dolomieu Crater ( Cratère Dolomieu ), which is by far the wider of the two and named for French geologist Déodat Gratet de Dolomieu . Many craters and spatter cones can be found inside the caldera and on the higher flanks of the volcano. Lavas with high concentrations of iridium are routinely ejected through these vents. By
288-460: The link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Fournaise&oldid=932829060 " Category : Disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Piton de la Fournaise Piton de la Fournaise ( French: [pitɔ̃ də la fuʁnɛz] ; English: "Peak of
306-557: The past 66 million years. There is evidence for explosive eruptions in the past. One explosive eruption about 4,700 years ago may have had a VEI (Volcanic Explosivity Index) of 5, which is the same as the 18 May 1980 eruption of Mount St. Helens . Most eruptions of Piton de la Fournaise are of the Hawaiian style : fluid basaltic lava flowing out with fire fountaining at the vent. Occasionally, phreatic eruptions (groundwater steam-generated eruptions) occur. Lava flows crossing
324-429: The trailhead of the summit path there lies a small noteworthy crater called Formica Leo , named for its resemblance to the sand pit trap of an antlion . Located outside of the main caldera is Commerson Crater , an inactive caldera notable for receiving intense rainfall, particularly during tropical storms. During Cyclone Hyacinthe in January 1980, it received 6,433 millimetres (253.3 in) of rainfall in 15 days,
#280719