Piton de la Fournaise

From Wikipedia, the free encyclopedia

Piton de la Fournaise
Piton de la Fournaise, Réunion Island (High Resolution).jpg
Piton de la Fournaise is a shield volcano
Highest point
Elevation2,632 m (8,635 ft)
Prominence1,021 m (3,350 ft) Edit this on Wikidata
Isolation26.98 km (16.76 mi) Edit this on Wikidata
Coordinates21°14′33″S 55°42′32″E / 21.24250°S 55.70889°E / -21.24250; 55.70889Coordinates: 21°14′33″S 55°42′32″E / 21.24250°S 55.70889°E / -21.24250; 55.70889
English translationPeak of the Furnace
Language of nameFrench
Piton de la Fournaise is located in Réunion
Piton de la Fournaise
Piton de la Fournaise
Age of rock530,000 year
Mountain typeShield volcano
Last eruptionDecember 2020 [1]
First ascent21 September 1751 [2]

Piton de la Fournaise (French: [pitɔ̃ də 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,[3] and on 1 August 2015.[4] The most recent eruption began on 7 December 2020.[1] 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 on Réunion island.


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 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, but whether or not it will generate a "megatsunami" is controversial.[citation needed] 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 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.

Topographic map showing the volcano and surrounding terrain

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 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, the most precipitation produced by a tropical cyclone in a single location.[5]

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 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 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.[1]


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. Occasionally, phreatic eruptions (groundwater steam-generated eruptions) occur. Lava flows crossing 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 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 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 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 of lava per day. During this eruption of 2007 an incremental caldera collapse of Dolomieu occurred at the volcano over more than nine days.[6] The collapse displacing 0.8 x 1.1 km floor downward by 330 m, with a volume of 120 million cubic metres. The caldera collapse accompanied one of the largest eruptions of lava at the volcano in the past 100 years.


Volcanic activity is constantly monitored by geophysical sensors (tiltmeters, extensometers, differential GPS receivers, etc.). The data from those various sensors 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 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:

  • Pre-alert: Warnings about possible eruptions; hikers accessing the caldera are warned about possible developments.
  • Level 1: An eruption will occur soon; the public may not access the caldera until specialists have examined the situation and set pathways for those willing to admire the eruption.
  • Level 2: An eruption is occurring inside the caldera. Access to the caldera is restricted to authorized personnel only.
  • Level 3: An eruption is occurring or will occur soon outside of the caldera; some villages may have to be evacuated for safety.


The gate for the visitors who want to climb the volcano

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 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 the road are indicated by signs. Completely free access during eruptions was permitted until 1998; access has been limited since that date, being virtually banned at present.[citation needed]

A panoramic view on the top of the volcano

See also[edit]


  1. ^ a b c "Piton de la Fournaise". Global Volcanism Program. Smithsonian Institution.
  2. ^ Active Volcanoes of the Southwest Indian Ocean: Piton de la Fournaise and Karthala, Patrick Bachelery, Springer, 2016 OCLC 928762285
  3. ^ "Le Piton de la Fournaise en direct (9 December 2010 – 9 April 2011)" (in French). Observatoire volcanologique du Piton de la Fournaise, Institut de Physique du Globe de Paris. Archived from the original on 27 April 2011.
  4. ^ Klemetti, Erik (2014). "New Eruption at Piton de la Fournaise on Reunion Island". Wired. Archived from the original on 22 June 2014.
  5. ^ Landsea, Christopher W; Hurricane Research Division (12 March 2007). "Subject: E4) What are the largest rainfalls associated with tropical cyclones?". Tropical Cyclone Frequently Asked Questions. Archived from the original on 3 December 2013. Retrieved 12 April 2013.
  6. ^ Fontaine, F. R.; Roult, G.; Hejrani, B.; Michon, L.; Ferrazzini, V.; Barruol, G.; Tkalčić, H.; Di Muro, A.; Peltier, A.; Reymond, D.; Staudacher, T.; Massin, F. (30 May 2019). "Very- and ultra-long-period seismic signals prior to and during caldera formation on La Réunion Island". Scientific Reports. 9 (1): 8068. Bibcode:2019NatSR...9.8068F. doi:10.1038/s41598-019-44439-1. ISSN 2045-2322. PMC 6543087. PMID 31147579.

External links[edit]