Supervolcano

A supervolcano is a large volcano that has had an eruption with a Volcanic Explosivity Index (VEI) of 8, the largest recorded value on the index. This means the volume of deposits for that eruption is greater than 1,000 cubic kilometers (240 cubic miles).[1]

Location of Yellowstone hotspot over time (numbers indicate millions of years before the present).
Satellite image of Lake Toba, the site of a VEI 8 eruption c. 75,000 years ago.
Cross-section through Long Valley Caldera.
For the 2005 disaster television film, see Supervolcano (film).

Map of known VEI 7 and VEI 8 volcanoes around the world:
  Volcanic Explosivity Index (VEI) 8 (Supervolcanoes)
  Volcanic Explosivity Index (VEI) 7

Supervolcanoes occur when magma in the mantle rises into the crust but is unable to break through it and pressure builds in a large and growing magma pool until the crust is unable to contain the pressure. This can occur at hotspots (for example, Yellowstone Caldera) or at subduction zones (for example, Toba).[2][3]

Large-volume supervolcanic eruptions are also often associated with large igneous provinces, which can cover huge areas with lava and volcanic ash. These can cause long-lasting climate change (such as the triggering of a small ice age) and threaten species with extinction. The Oruanui eruption of New Zealand's Taupo Volcano (about 26,500 years ago)[4] was the world's most recent VEI-8 eruption.

Terminology

The term "supervolcano" was first used in a volcanic context in 1949.[note 1]

Its origins lie in an early 20th-century scientific debate about the geological history and features of the Three Sisters volcanic region of Oregon in the United States. In 1925, Edwin T. Hodge suggested that a very large volcano, which he named Mount Multnomah, had existed in that region.[note 2] He believed that several peaks in the Three Sisters area were the remnants of Mount Multnomah after it had been largely destroyed by violent volcanic explosions, similar to Mount Mazama.[5] In 1948, the possible existence of Mount Multnomah was ignored by volcanologist Howel Williams in his book The Ancient Volcanoes of Oregon. This book was reviewed in 1949 by another volcanologist, F. M. Byers Jr.[6] In the review, Byers refers to Mount Multnomah as a supervolcano.[7]

More than fifty years after Byers' review was published, the term supervolcano was popularised by the BBC popular science television program Horizon in 2000, referring to eruptions that produce extremely large amounts of ejecta.[8][9]

The term megacaldera is sometimes used for caldera supervolcanoes, such as the Blake River Megacaldera Complex in the Abitibi greenstone belt of Ontario and Quebec, Canada.

Eruptions that rate VEI 8 are termed "super eruptions".[10] Though there is no well-defined minimum explosive size for a "supervolcano", there are at least two types of volcanic eruptions that have been identified as supervolcanoes: large igneous provinces and massive eruptions.[11]

Large igneous provinces
Map of large Flood Basalt igneous provinces worldwide
Main article: Large igneous province

Large igneous provinces, such as Iceland, the Siberian Traps, Deccan Traps, and the Ontong Java Plateau, are extensive regions of basalts on a continental scale resulting from flood basalt eruptions. When created, these regions often occupy several thousand square kilometres and have volumes on the order of millions of cubic kilometers. In most cases, the lavas are normally laid down over several million years. They release large amounts of gases.

The Réunion hotspot produced the Deccan Traps about 66 million years ago, coincident with the Cretaceous–Paleogene extinction event. The scientific consensus is that a meteor impact was the cause of the extinction event, but the volcanic activity may have caused environmental stresses on extant species up to the Cretaceous–Paleogene boundary.[12] Additionally, the largest flood basalt event (the Siberian Traps) occurred around 250 million years ago and was coincident with the largest mass extinction in history, the Permian–Triassic extinction event, although it is unknown whether it was solely responsible for the extinction event.

Such outpourings are not explosive, though lava fountains may occur. Many volcanologists consider Iceland to be a large igneous province that is currently being formed. The last major outpouring occurred in 1783–84 from the Laki fissure, which is approximately 40 km (25 mi) long. An estimated 14 km3 (3.4 cu mi) of basaltic lava was poured out during the eruption (VEI 4).

The Ontong Java Plateau has an area of about 2,000,000 km2 (770,000 sq mi), and the province was at least 50% larger before the Manihiki and Hikurangi Plateaus broke away.

Massive explosive eruptions
See also: List of largest volcanic eruptions

Volcanic eruptions are classified using the Volcanic Explosivity Index, or VEI. It is a logarithmic scale, which means that an increase of one in VEI number is equivalent to a tenfold increase in volume of erupted material. VEI 7 or VEI 8 eruptions are so powerful that they often form circular calderas rather than cones because the downward withdrawal of magma causes the overlying rock mass to collapse into the empty magma chamber beneath it.

Known super eruptions

Based on incomplete statistics, at least 60 VEI 8 eruptions have been identified.[11][13] Below is a list of well-known super-eruptions.

VEI 8 eruptions have happened in the following locations.
Name Zone Location Notes Years ago (approx.) Ejecta bulk volume (approx.) Reference
Wah Wah Springs Indian Peak–Caliente Caldera Complex Utah, United States The largest of the Indian Peak-Caliente Caldera Complex eruptions, preserved as the Wah Wah Springs Tuff; includes pyroclastic flows more than 4,000 metres (13,000 ft) thick 30,600,000 5,500–5,900 km3 [14][15]
La Garita Caldera San Juan volcanic field Colorado, United States Fish Canyon eruption 27,800,000 5,000 km3 [16][17]
Youngest Toba Eruption Lake Toba, North Sumatra Sumatra, Indonesia Produced 2200–4400 million tons of H2SO4 74,000 2,800 km3 [18][19][20]

[21][22] [23][15]

La Pacana Andes Central Volcanic Zone Chile Responsible for the Antana Ignimbrite 4,000,000 2500 km3 [24]
Huckleberry Ridge eruption Yellowstone hotspot Idaho, United States Huckleberry Ridge Tuff; consisted of three distinct eruptions separated by years to decades 2,100,000 2,450–2,500 km3 [25][23]
Taupo Nui a tia Taupo Volcanic Zone North Island, New Zealand Whakamaru Ignimbrite/Mount Curl Tephra 340,000 2,000 km3 [26]
Heise Volcanic Field Yellowstone hotspot Idaho, United States Kilgore Tuff 4,500,000 1,800 km3 [27]
Heise Volcanic Field Yellowstone hotspot Idaho, United States Blacktail Tuff 6,000,000 1,500 km3 [27]
Cerro Guacha Altiplano-Puna volcanic complex Sur Lípez, Bolivia Guacha ignimbrite, two smaller eruptions identified 5,700,000 1,300 km3 [28]
Mangakino Caldera Taupo Volcanic Zone North Island, New Zealand Kidnappers eruption 1,080,000 1,200 km3 [29]
Oruanui eruption Taupo Volcanic Zone North Island, New Zealand Taupo Volcano (Lake Taupo) 26,500 1,170 km3 [30]
Cerro Galán Andes Central Volcanic Zone Catamarca, Argentina Consisted of three distinct eruptions, separated by 30-40 thousands of years 2,500,000 1,050 km3 [31]
Lava Creek eruption Yellowstone hotspot Idaho, Montana, and Wyoming, United States Lava Creek Tuff; consisted of two distinct eruptions separated by years 640,000 1,000 km3 [25][23][15]
Bishop Tuff Long Valley Caldera California, United States A single eruption completed within 6 days; volume in dense rock equivalent 760,000 600 km3 [32]

Media portrayal
  • Nova featured an episode "Mystery of the Megavolcano" in September 2006 examining such eruptions in the last 100,000 years.[33]
  • Volcano, lake, and caldera locations in the Taupo Volcanic Zone

See also

References
  1. The term entered the English language already in a 1925 book, Conquering the World by Helen Bridgeman, about Indonesia to refer to an Indian Ocean sunset.
  2. Subsequent research proved that each peak of the Three Sisters was formed independently, and that Mount Multnomah never existed.
  1. "Questions About Supervolcanoes". Volcanic Hazards Program. USGS Yellowstone Volcano Observatory. 21 August 2015. Archived from the original on 3 July 2017. Retrieved 22 August 2017.
  2. Wotzlaw, Jörn-Frederik; Bindeman, Ilya N.; Watts, Kathryn E.; Schmitt, Axel K.; Caricchi, Luca; Schaltegger, Urs (September 2014). "Linking rapid magma reservoir assembly and eruption trigger mechanisms at evolved Yellowstone-type supervolcanoes". Geology. 42 (9): 807–810. doi:10.1130/g35979.1. ISSN 1943-2682.
  3. Budd, David A.; Troll, Valentin R.; Deegan, Frances M.; Jolis, Ester M.; Smith, Victoria C.; Whitehouse, Martin J.; Harris, Chris; Freda, Carmela; Hilton, David R.; Halldórsson, Sæmundur A.; Bindeman, Ilya N. (25 January 2017). "Magma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz". Scientific Reports. 7 (1): 40624. doi:10.1038/srep40624. ISSN 2045-2322. PMC 5264179. PMID 28120860.
  4. Wilson, C. J. N. (2001). "The 26.5ka Oruanui eruption, New Zealand: An introduction and overview". Journal of Volcanology and Geothermal Research. 112 (1–4): 133–174. Bibcode:2001JVGR..112..133W. doi:10.1016/S0377-0273(01)00239-6.
  5. Harris, Stephen (1988) Fire Mountains of the West: The Cascade and Mono Lake Volcanoes, Missoula, Mountain Press.
  6. Byers Jr., F. M. (1949) Reviews: The Ancient Volcanoes of Oregon by Howel Williams Archived 8 March 2016 at the Wayback Machine, The Journal of Geology, volume 57, number 3, May 1949, page 324. Retrieved 2012-08-17.
  7. supervolcano, n. Oxford English Dictionary, third edition, online version June 2012. Retrieved on 2012-08-17.
  8. Supervolcanoes Archived 1 August 2003 at the Wayback Machine. Bbc.co.uk (2000-02-03). Retrieved on 2011-11-18.
  9. USGS Cascades Volcano Observatory Archived 4 February 2012 at the Wayback Machine. Vulcan.wr.usgs.gov. Retrieved on 2011-11-18.
  10. de Silva, Shanaka (2008). "Arc magmatism, calderas, and supervolcanos". Geology. 36 (8): 671–672. Bibcode:2008Geo....36..671D. doi:10.1130/focus082008.1.
  11. Bryan, S.E. (2010). "The largest volcanic eruptions on Earth" (PDF). Earth-Science Reviews. 102 (3–4): 207–229. Bibcode:2010ESRv..102..207B. doi:10.1016/j.earscirev.2010.07.001.
  12. Keller, G (2014). "Deccan volcanism, the Chicxulub impact, and the end-Cretaceous mass extinction: Coincidence? Cause and effect?". Geological Society of America Special Papers. 505: 57–89. doi:10.1130/2014.2505(03). ISBN 9780813725055.
  13. BG, Mason (2004). "The size and frequency of the largest explosive eruptions on Earth". Bull Volcanol. 66 (8): 735–748. Bibcode:2004BVol...66..735M. doi:10.1007/s00445-004-0355-9. S2CID 129680497.
  14. Tingey, David G.; Hart, Garret L.; Gromme, Sherman; Deino, Alan L.; Christiansen, Eric H.; Best, Myron G. (1 August 2013). "The 36–18 Ma Indian Peak–Caliente ignimbrite field and calderas, southeastern Great Basin, USA: Multicyclic super-eruptions". Geosphere. 9 (4): 864–950. Bibcode:2013Geosp...9..864B. doi:10.1130/GES00902.1.
  15. https://geology.com/stories/13/volcanic-explosivity-index/
  16. Ort, Michael (22 September 1997). "La Garita Caldera". Northern Arizona University. Archived from the original on 19 May 2011. Retrieved 5 August 2010.
  17. Lipman, Peter W. (2 November 2007). "Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado". USGS Investigations Series I-2799. Archived from the original on 31 August 2010. Retrieved 6 August 2010. Cite journal requires |journal= (help)
  18. Petraglia, M.; Korisettar, R.; Boivin, N.; Clarkson, C.; Ditchfield, P.; Jones, S.; Koshy, J.; Lahr, M. M.; et al. (2007). "Middle Paleolithic Assemblages from the Indian Subcontinent Before and After the Toba Super-Eruption". Science. 317 (5834): 114–116. Bibcode:2007Sci...317..114P. doi:10.1126/science.1141564. PMID 17615356. S2CID 20380351.
  19. Knight, M.D., Walker, G.P.L., Ellwood, B.B., and Diehl, J.F. (1986). "Stratigraphy, paleomagnetism, and magnetic fabric of the Toba Tuffs: Constraints on their sources and eruptive styles". Journal of Geophysical Research. 91 (B10): 10355–10382. Bibcode:1986JGR....9110355K. doi:10.1029/JB091iB10p10355.CS1 maint: multiple names: authors list (link)
  20. Ninkovich, D., Sparks, R.S.J., and Ledbetter, M.T. (1978). "The exceptional magnitude and intensity of the Toba eruption, Sumatra: An example of using deep-sea tephra layers as a geological tool". Bulletin Volcanologique. 41 (3): 286–298. Bibcode:1978BVol...41..286N. doi:10.1007/BF02597228. S2CID 128626019.CS1 maint: multiple names: authors list (link)
  21. Rose, W.I. & Chesner, C.A. (1987). "Dispersal of ash in the great Toba eruption, 75 ka" (PDF). Geology. 15 (10): 913–917. Bibcode:1987Geo....15..913R. doi:10.1130/0091-7613(1987)15<913:DOAITG>2.0.CO;2. ISSN 0091-7613. Archived (PDF) from the original on 17 June 2010.
  22. Williams, M.A.J. & Royce, K. (1982). "Quaternary geology of the middle son valley, North Central India: Implications for prehistoric archaeology". Palaeogeography, Palaeoclimatology, Palaeoecology. 38 (3–4): 139. Bibcode:1982PPP....38..139W. doi:10.1016/0031-0182(82)90001-3.
  23. https://www.usgs.gov/faqs/what-a-supervolcano?qt-news_science_products=0#qt-news_science_products
  24. Lindsay, J. M. (1 March 2001). "Magmatic Evolution of the La Pacana Caldera System, Central Andes, Chile: Compositional Variation of Two Cogenetic, Large-Volume Felsic Ignimbrites". Journal of Petrology. 42 (3): 459–486. Bibcode:2001JPet...42..459L. doi:10.1093/petrology/42.3.459. ISSN 0022-3530.
  25. Global Volcanism Program | Volcanoes of the World | Large Holocene Eruptions Archived 13 February 2010 at the Wayback Machine. Volcano.si.edu. Retrieved on 2011-11-18.
  26. Froggatt, P. C.; Nelson, C. S.; Carter, L.; Griggs, G.; Black, K. P. (13 February 1986). "An exceptionally large late Quaternary eruption from New Zealand". Nature. 319 (6054): 578–582. Bibcode:1986Natur.319..578F. doi:10.1038/319578a0. S2CID 4332421. The minimum total volume of tephra is 1,200 km3 but probably nearer 2,000 km3, ...
  27. Lisa A. Morgan & William C. McIntosh (2005). "Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA". GSA Bulletin. 117 (3–4): 288–306. Bibcode:2005GSAB..117..288M. doi:10.1130/B25519.1. S2CID 53648675.
  28. Salisbury, M. J.; Jicha, B. R.; de Silva, S. L.; Singer, B. S.; Jimenez, N. C.; Ort, M. H. (21 December 2010). "40Ar/39Ar chronostratigraphy of Altiplano-Puna volcanic complex ignimbrites reveals the development of a major magmatic province". Geological Society of America Bulletin. 123 (5–6): 821–840. Bibcode:2011GSAB..123..821S. doi:10.1130/B30280.1.
  29. Rejuvenation and Repeated Eruption of a 1.0 Ma Supervolcanic System at Mangakino Caldera, Taupo Volcanic Zone, New Zealand American Geophysical Union, Fall Meeting 2012, abstract #V31C-2797. Retrieved 10 September 2017.
  30. Wilson, C. J. N (1 December 2001). "The 26.5ka Oruanui eruption, New Zealand: an introduction and overview". Journal of Volcanology and Geothermal Research. 112 (1): 133–174. Bibcode:2001JVGR..112..133W. doi:10.1016/S0377-0273(01)00239-6. ISSN 0377-0273.
  31. Kay, Suzanne Mahlburg; Coira, Beatriz; Wörner, Gerhard; Kay, Robert W.; Singer, Bradley S. (1 December 2011). "Geochemical, isotopic and single crystal 40Ar/39Ar age constraints on the evolution of the Cerro Galán ignimbrites". Bulletin of Volcanology. 73 (10): 1487–1511. Bibcode:2011BVol...73.1487K. doi:10.1007/s00445-010-0410-7. ISSN 1432-0819.
  32. Hildreth, Wes; Wilson, Colin J. N. (1 May 2007). "Compositional Zoning of the Bishop Tuff". Journal of Petrology. 48 (5): 951–999. Bibcode:2007JPet...48..951H. doi:10.1093/petrology/egm007. ISSN 0022-3530.
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Further reading
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