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Piton de la Fournaise ( Peak of the Furnace ). By Joseph Barnes and Papa Moda Loum . Dept. of Geology, Colby College. Geographic and tectonic setting. Sits on a mantle plume (hot spot) Western Indian Ocean Latitude: 21.231°S 21°13'51"S Longitude: 55.713°E 55°42'45"E.
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Piton de la Fournaise (Peak of the Furnace) By Joseph Barnes and Papa ModaLoum. Dept. of Geology, Colby College
Geographic and tectonic setting • Sits on a mantle plume (hot spot) • Western IndianOcean • Latitude:21.231°S 21°13'51"S Longitude:55.713°E 55°42'45"E
Dimensions • 530,000 yearoldshieldvolcano • Base: 135 miles (220 km) in diameter • 21,600 feettall (6600 meters) • The base of the volcanois 24 times largerthan the one in Mount St.Helens
Eruptive history • One of the most active volcanoes in the world (lava eruptions) • Recordederuptions: • First : 1640 • Last: 2010
Eruptive style • Hawaiian style : pahoehoe and aaflows. Pahoehoe AA
Volcanicdeposits • Depositsfrom lava flows: • Pahoehoe and AA • Pyroclasticflows Piton de la Fournaise 2010 eruption
Positivecontributions • Power source • Tourism In the 1977 eruption, the local people cried miracle because the lava spared the church. Sincethen, the entrance has been cleared and the churchrepainted and renamed "Notre Dame des Laves" (litterally: "Our Lady of the Lavas").
Volcanichazards • Small population , verylittle danger and damage • 1977 : village of Piton-Sainte-Rose wasinundated by lava flows.
On 6 July 2001, police and security personnel watch as molten lava from Piton de la Fournaise blocks the main national RN 2 road, which connects Réunion island from E to S.
Observederuption • April 2007 : • 3,000,000 cubicmeters of lava • caldera collapse • One of the largesteruptions of lava in the past 100 years
Caldera’s collapse consequences • The 6 April collapse affected the Dolomieu's Northern part. • SO₂ release • Decreasedgas content of unerupted magma
Hydrothermal activity • No major hydrothermal activity • Potential hydrothermal system from the summit area to the magma reservoir
Petrology and volcanicdeposits Basalt rock Olivine based, plagioclase-phyricbasedbasalt
Monitoring of the volcano Tiltmeters Differential GPS receivers Extensometers
Monitoring (continued) Figure A: Daily earthquakes at Piton de la Fournaise during 1 March to 1 July 2006. Courtesy of OVPF. Seismicitywaslowfrommid-Januarythrough March. From March untilmid-July, seismicitygraduallyincreased.
Tourism • 1990 – 2005 : the golden era • 2001: • 424,000 tourists • 271.5 million € revenue B. 2005 – 2006: the crisis • 27 and 60% drops in 2005 and 2006, respectively
Bibliography • Works cited http://volcano.oregonstate.edu/book/export/html/139http://www.volcanolive.com/piton.htmlhttp://www.alaingerente.com/ehistoire.htmlhttp://www.volcano.si.edu/world/volcano.cfm?vnum=0303-02=&volpage=weeklyhttp://en.wikipedia.org/wiki/Piton_de_la_Fournaisehttp://onlinelibrary.wiley.com/doi/10.1029/2010GL046183/fullhttp://en.wikipedia.org/wiki/Tourism_in_R%C3%A9unionhttp://publishing.cdlib.org/ucpressebooks/view?docId=ft6v19p151&chunk.id=d0e13525&toc.id=d0e12419&brand=ucpress
https://www.google.com/search?q=piton+de+la+fournaise+caldera&hl=en&client=firefox-a&hs=sft&tbo=u&rls=org.mozilla:en-US:official&channel=fflb&biw=1440&bih=679&tbm=isch&source=univ&sa=X&ei=_9gBUevjC5Lh0AHCxYGgDw&ved=0CC0QsAQhttps://www.google.com/search?q=piton+de+la+fournaise+craters&hl=en&client=firefox-a&hs=pKE&tbo=u&rls=org.mozilla:en-US:official&channel=fflb&biw=1440&bih=679&tbm=isch&source=univ&sa=X&ei=5NgBUaCaO8a60AH6w4DICA&ved=0CD4QsAQhttp://volcano.oregonstate.edu/oldroot/volcanoes/piton/index.html http://www.gsi.ie/Education/Geology+for+Everyone/Volcanoes.html • http://www.picstropical.com/reunion/index_files/index_reunion_map.gif • http://farm5.staticflickr.com/4082/4770746257_158e07d3a5.jpg • http://www.alaingerente.com/ehistoire.html • http://www.sainte-rose-reunion.org/images/stories/coulee1977.jpg • http://geology.com/rocks/pictures/basalt-380.jpg • http://jfmoyen.free.fr/IMG/jpg/bplagio.jpghttp://tanoutout.com/sites/default/files/images/8.gif