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List of largest volcanic eruptions

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A tower of grey ash erupts above a mountain
The 1991 eruption of Mount Pinatubo, the largest eruption since 1912, is dwarfed by the eruptions in this list.

In a volcanic eruption, lava, volcanic bombs, ash, and various gases are expelled from a volcanic vent and fissure. While many eruptions only pose dangers to the immediately surrounding area, Earth's largest eruptions can have a major regional or even global impact, with some affecting the climate and contributing to mass extinctions.[1][2] Volcanic eruptions can generally be characterized as either explosive eruptions, sudden ejections of rock and ash, or effusive eruptions, relatively gentle outpourings of lava.[3] A separate list is given below for each type.

There have probably been many such eruptions during Earth's history beyond those shown in these lists. However erosion and plate tectonics have taken their toll, and many eruptions have not left enough evidence for geologists to establish their size. Even for the eruptions listed here, estimates of the volume erupted can be subject to considerable uncertainty.[4]

Explosive eruptions

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Further information: Supervolcano § Massive explosive eruptions

In explosive eruptions, the eruption of magma is driven by the rapid release of pressure, often involving the explosion of gas previously dissolved within the material. The most famous and destructive historical eruptions are mainly of this type. An eruptive phase can consist of a single eruption, or a sequence of several eruptions spread over several days, weeks or months. Explosive eruptions usually involve thick, highly viscous, silicic or felsic magma, high in volatiles like water vapor and carbon dioxide. Pyroclastic materials are the primary product, typically in the form of tuff. Eruptions the size of that at Lake Toba 74,000 years ago, at least 2,800 cubic kilometres (670 cu mi), or the Yellowstone eruption 620,000 years ago, around 1,000 cubic kilometres (240 cu mi), occur worldwide every 50,000 to 100,000 years.[1][n 1]

Volcano—eruption[5] Age (millions of years)[n 2] Location Volume (km3)[n 3] Notes Ref.
Guarapuava —Tamarana—Sarusas 132  Paraná and Etendeka traps 8,600 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Santa Maria—Fria ~132  Paraná and Etendeka traps 7,800 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Lake Toba Caldera—Youngest Toba Tuff 0.073 Sunda Arc, Indonesia 2,000–13,200 Largest known eruption on earth in at least the last million years, possibly responsible for a population bottleneck of the human species (see Toba catastrophe theory) [8][9][10]

[11][12][13]

Guarapuava —Ventura ~132  Paraná and Etendeka traps 7,600 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Flat Landing Brook Eruption 466  Flat Landing Brook Formation 2,000–12,000 One of the largest and oldest supereruptions. Existence as a single eruption is controversial. Possibly a multiple 2,000+ km3 event under a million years. [14][15]
Sam Ignimbrite and Green Tuff 29.5  Yemen 6,797–6,803 Volume includes 5550 km3 of distal tuffs. This estimate is uncertain to a factor of 2 or 3. [16]
Goboboseb–Messum volcanic centre—Springbok quartz latite unit 132  Paraná and Etendeka traps, Brazil and Namibia 6,340 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [17]
Wah Wah Springs Tuff 30.06  Indian Peak-Caliente Caldera Complex 5,500–5,900 The largest of the Indian Peak-Caliente Caldera Complex, and includes flows over 4,000 meters thick at the most. [18][10]
Caxias do Sul—Grootberg ~132  Paraná and Etendeka traps 5,650 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
La Garita Caldera—Fish Canyon Tuff 27.8  San Juan volcanic field, Colorado 5,000 Part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma. [19][20]
Lund Tuff 29.2  Indian Peak-Caliente Caldera Complex 4,400 Formed the White Rock Caldera, one of the largest eruptions of the Mid-Tertiary Ignimbrite flareup. [18]
Jacui—Goboboseb II ~132  Paraná and Etendeka traps 4,350 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Ourinhos—Khoraseb ~132  Paraná and Etendeka traps 3,900 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Jabal Kura'a Ignimbrite 29.6  Yemen 3,797–3,803 Volume estimate is uncertain to a factor of 2 or 3. [16]
Windows Butte tuff 31.4  William's Ridge, central Nevada 3,500 Part of the Mid-Tertiary ignimbrite flare-up [21][22]
Anita Garibaldi—Beacon ~132  Paraná and Etendeka traps 3,450 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Oxaya ignimbrites 19  Chile 3,000 Really a regional correlation of many ignimbrites originally thought to be distinct [23]
Gakkel Ridge Caldera 1.1  Gakkel Ridge 3,000 It is the only known supervolcano located directly on the mid-ocean ridge.
Grey's Landing Supereruption 8.72  Located in southern Idaho >2,800 One of 2 previously unknown Yellowstone hotspot Supereruptions; Largest Yellowstone eruption. [24]
Pacana Caldera—Atana ignimbrite 4  Chile 2,800 Forms a resurgent caldera. [25]
Mangakino Caldera—Kidnappers ignimbrite 1.01  Taupō Volcanic Zone, New Zealand 2,760 [26]
Iftar Alkalb—Tephra 4 W 29.5  Afro-Arabian 2,700 [4]
Yellowstone Caldera—Huckleberry Ridge Tuff 2.059 Yellowstone hotspot 2,450–2,500 One of the largest Yellowstone eruptions on record [27][9]
Nohi Rhyolite—Gero Ash-Flow Sheet 70  Honshū, Japan 2,200 Nohi Rhyolite total volume over 7,000 km3 in 70 to 72 Ma, Gero Ash-Flow Sheet being the largest [28]
Whakamaru 0.254 Taupō Volcanic Zone, New Zealand 2,000 Largest in the Southern Hemisphere in the Late Quaternary [29]
Palmas BRA-21—Wereldsend 29.5  Paraná and Etendeka traps 1,900 The nature of eruption is disputed. Paraná Province suggests an effusive origin from local sources.[6][7] No ashfall deposits have been found, and the erupted volume could be 2-3 times larger than listed if any ashfall deposits are found.[4] [4]
Kilgore tuff 4.3  Near Kilgore, Idaho 1,800 Last of the eruptions from the Heise volcanic field [30]
McMullen Supereruption 8.99  Located in southern Idaho >1,700 One of 2 previously unknown Yellowstone hotspot eruptions. [24]
Sana'a Ignimbrite—Tephra 2W63 29.5  Afro-Arabian 1,600 [4]
Deicke and Millbrig 454  England, exposed in Northern Europe and Eastern US 1,509[n 4] One of the oldest large eruptions preserved [5][31][32]
Blacktail tuff 6.5  Blacktail, Idaho 1,500 First of several eruptions from the Heise volcanic field [30]
Mangakino Caldera—Rocky Hill 1  Taupō Volcanic Zone, New Zealand 1,495 [26]
Aso Caldera 0.087 Kyushu, Japan 930–1,860 Aso-4 ignimbrite [13]
Emory Caldera—Kneeling Nun tuff 33  Mogollon-Datil volcanic field 1,310 [33]
Omine-Odai Caldera—Murou pyroclastic flow 13.7  Honshū, Japan 1,260 A part of the large eruptions that occurred in southwest Japan to 13 to 15 Ma. [34]
Timber Mountain tuff 11.6  Southwestern Nevada 1,200 Also includes a 900 cubic km tuff as a second member in the tuff [35]
Paintbrush tuff (Tonopah Spring Member) 12.8  Southwestern Nevada 1,200 Related to a 1000 cubic km tuff (Tiva Canyon Member) as another member in the Paintbrush tuff [35]
Bachelor—Carpenter Ridge tuff 28  San Juan volcanic field 1,200 Part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma [20]
Bursum—Apache Springs Tuff 28.5  Mogollon-Datil volcanic field 1,200 Related to a 1050 cubic km tuff, the Bloodgood Canyon tuff [36]
Taupō Volcano—Oruanui eruption 0.027 Taupō Volcanic Zone, New Zealand 1,170 Most recent VEI 8 eruption [37]
Mangakino Caldera—Ongatiti–Mangatewaiiti 1.21  Taupō Volcanic Zone, New Zealand 1,150 [26]
Huaylillas Ignimbrite 15  Bolivia 1,100 Predates half of the uplift of the central Andes [38]
Bursum—Bloodgood Canyon Tuff 28.5  Mogollon-Datil volcanic field 1,050 Related to a 1200 cubic km tuff, the Apache Springs tuff [36]
Okueyama Caldera 13.7  Kyūshū, Japan 1,030 A part of the large eruptions that occurred in southwest Japan to 13 to 15 Ma. [34]
Yellowstone Caldera—Lava Creek Tuff 0.639 Yellowstone hotspot 1,000 Last large eruption in the Yellowstone National Park area [39][9][10]
Awasa Caldera 1.09  Main Ethiopian Rift 1,000 [40]
Cerro Galán 2.2  Catamarca Province, Argentina 1,000 Elliptical caldera is ~35 km wide [41]
Paintbrush tuff (Tiva Canyon Member) 12.7  Southwestern Nevada 1,000 Related to a 1200 cubic km tuff (Topopah Spring Member) as another member in the Paintbrush tuff [35]
San Juan—Sapinero Mesa Tuff 28  San Juan volcanic field 1,000 Part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma [20]
Uncompahgre—Dillon & Sapinero Mesa Tuffs 28.1  San Juan volcanic field 1,000 Part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma [20]
Platoro—Chiquito Peak tuff 28.2  San Juan volcanic field 1,000 Part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma [20]
Mount Princeton—Wall Mountain tuff 35.3  Thirtynine Mile volcanic area, Colorado 1,000 Helped cause the exceptional preservation at Florissant Fossil Beds National Monument [42]
Aira Caldera 0.03  Kyushu, Japan 940–1,040 Osumi pumice fall deposit, Ito ignimbrite, and Aira-Tanzawa ash fall deposit [13]

Effusive eruptions

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A red-hot lava flow streams out of a fuming vent, meandering past the viewer under a low cloudy sky.
Effusive eruption of lava from Krafla, Iceland

Effusive eruptions involve a relatively gentle, steady outpouring of lava rather than large explosions. They can continue for years or decades, producing extensive fluid mafic lava flows.[43] For example, Kīlauea on Hawaiʻi continuously erupted from 1983 to 2018, producing 2.7 km3 (1 cu mi) of lava covering more than 100 km2 (40 sq mi).[44] Despite their ostensibly benign appearance, effusive eruptions can be as dangerous as explosive ones: one of the largest effusive eruptions in history occurred in Iceland during the 1783–1784 eruption of Laki, which produced about 15 km3 (4 cu mi) of lava and killed one fifth of Iceland's population.[43] The ensuing disruptions to the climate may also have killed millions elsewhere.[45] Still larger were the Icelandic eruptions of Katla (the Eldgjá eruption) circa 934, with 18 km3 (4 cu mi) of erupted lava, and the Þjórsárhraun eruption of Bárðarbunga circa 6700 BCE, with 25 km3 (6 cu mi) lava erupted, the latter being the largest effusive eruption in the last 10,000 years.[46] The lava fields of these eruptions measure 565 km2 (Laki), 700 km2 (Eldgjá) and 950 km2 (Þjórsárhraun).

Eruption Age (Millions of years) Location Volume
(km3) 		Notes Refs
Mahabaleshwar–Rajahmundry Traps (Upper) 64.8 Deccan Traps, India 9,300 [4]
Wapshilla Ridge flows ~15.5 Columbia River Basalt Group, United States 5,000–10,000 Member comprises 8–10 flows with a total volume of ~50,000 km3 [47]
McCoy Canyon flow 15.6 Columbia River Basalt Group, United States 4,300 [47]
Umtanum flows ~15.6 Columbia River Basalt Group, United States 2,750 Two flows with a total volume of 5,500 km3 [4]
Sand Hollow flow 15.3 Columbia River Basalt Group, United States 2,660 [4]
Pruitt Draw flow 16.5 Columbia River Basalt Group, United States 2,350 [47]
Museum flow 15.6 Columbia River Basalt Group, United States 2,350 [47]
Moonaree Dacite 1591   Gawler Range Volcanics, Australia 2,050 One of the oldest large eruptions preserved [4]
Rosalia flow 14.5 Columbia River Basalt Group, United States 1,900 [4]
Joseph Creek flow 16.5 Columbia River Basalt Group, United States 1,850 [47]
Ginkgo Basalt 15.3 Columbia River Basalt Group, United States 1,600 [4]
California Creek–Airway Heights flow 15.6 Columbia River Basalt Group, United States 1,500 [47]
Stember Creek flow 15.6 Columbia River Basalt Group, United States 1,200 [47]

Large igneous provinces

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Main article: Large igneous province
The Siberian Traps underlie much of Russia, from the Lena River west to the Ural Mountains (around 3,000 km), and stretching south from the Arctic coast almost to Lake Baikal (around 2,000 km).
Extent of the Siberian Traps large igneous province (map in German)

Highly active periods of volcanism in what are called large igneous provinces have produced huge oceanic plateaus and flood basalts in the past. These can comprise hundreds of large eruptions, producing millions of cubic kilometers of lava in total. No large eruptions of flood basalts have occurred in human history, the most recent having occurred over 10 million years ago. They are often associated with breakup of supercontinents such as Pangea in the geologic record,[48] and may have contributed to a number of mass extinctions. Most large igneous provinces have either not been studied thoroughly enough to establish the size of their component eruptions, or are not preserved well enough to make this possible. Many of the eruptions listed above thus come from just two large igneous provinces: the Paraná and Etendeka traps and the Columbia River Basalt Group. The latter is the most recent large igneous province, and also one of the smallest.[45] A list of large igneous provinces follows to provide some indication of how many large eruptions may be missing from the lists given here.

Igneous province Age (Millions of years) Location Volume (millions of km3) Notes Refs
Ontong Java–Manihiki–Hikurangi Plateau 121  Southwest Pacific Ocean 59–77[n 5] Largest igneous body on Earth, later split into three widely separated oceanic plateaus, with a fourth component perhaps now accreted onto South America. Possibly linked to the Louisville hotspot. [49][50][51]
Kerguelen Plateau–Broken Ridge 112  South Indian Ocean, Kerguelen Islands 17[n 5] Linked to the Kerguelen hotspot. Volume includes Broken Ridge and the Southern and Central Kerguelen Plateau (produced 120–95 Ma), but not the Northern Kerguelen Plateau (produced after 40 Ma). [52][53]
North Atlantic Igneous Province 55.5 North Atlantic Ocean 6.6[n 6] Linked to the Iceland hotspot. [5][54]
Mid-Tertiary ignimbrite flare-up 32.5 Southwest United States: mainly in Colorado, Nevada, Utah, and New Mexico 5.5 Mostly andesite to rhyolite explosive (.5 million km3) to effusive (5 million km3) eruptions, 25–40 Ma. Includes many volcanic centers, including the San Juan volcanic field. [55]
Caribbean large igneous province 88  Caribbean–Colombian oceanic plateau 4 Linked to the Galápagos hotspot. [56]
Siberian Traps 249.4 Siberia, Russia 1–4 A large outpouring of lava on land, believed to have caused the Permian–Triassic extinction event, the largest mass extinction ever. [57]
Karoo-Ferrar 183  Mainly Southern Africa and Antarctica. Also South America, India, Australia and New Zealand 2.5 Formed as Gondwana broke up [58]
Paraná and Etendeka traps 133  Brazil/Angola and Namibia 2.3 Linked to the Tristan hotspot [59][60]
Central Atlantic magmatic province 200  Laurasia continents 2 Believed to be the cause of the Triassic–Jurassic extinction event. Formed as Pangaea broke up [61]
Deccan Traps 66  Deccan Plateau, India 1.5 A large igneous province of west-central India, believed to have been one of the causes of the Cretaceous–Paleogene extinction event. Linked to the Réunion hotspot. [62][63]
Emeishan Traps 256.5 Southwestern China 1 Along with Siberian Traps, may have contributed to the Permian–Triassic extinction event. [64]
Coppermine River Group 1267  Mackenzie Large Igneous Province/Canadian Shield 0.65 Consists of at least 150 individual flows. [65]
Ethiopia-Yemen Continental Flood Basalts 28.5 Ethiopia/Yemen/Afar, Arabian-Nubian Shield 0.35 Associated with silicic, explosive tuffs [66][67]
Columbia River Basalt Group 16  Pacific Northwest, United States 0.18 Well exposed by Missoula Floods in the Channeled Scablands. [68]

See also

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Notes

[edit]
  1. ^ Certain felsic provinces, such as the Chon Aike province in Argentina and the Whitsunday igneous province of Australia, are not included in this list because they are composed of many separate eruptions that have not been distinguished.
  2. ^ Dates are an average of the range of dates of volcanics.
  3. ^ These volumes are estimated total volumes of tephra ejected. If the available sources only report a dense rock equivalent volume, the number is italicized but not converted into a tephra volume.
  4. ^ Also the site of 972 and 943 km3 (233 and 226 cu mi) eruptions.
  5. ^ a b This is the volume of crustal thickening, so the figure includes intrusive as well as extrusive deposits.
  6. ^ Actually several provinces, ranging in size from 1.5 to 6.6 million km3

References

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  1. ^ a b Roy Britt, Robert (8 March 2005). "Super Volcano Will Challenge Civilization, Geologists Warn". LiveScience. Archived from the original on 23 March 2012. Retrieved 27 August 2010.
  2. ^ Self, Steve. "Flood basalts, mantle plumes and mass extinctions". Geological Society of London. Archived from the original on 29 February 2012. Retrieved 27 August 2010.
  3. ^ "Effusive & Explosive Eruptions". Geological Society of London. Archived from the original on 11 October 2013. Retrieved 28 August 2010.
  4. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z Scott E. Bryan; Ingrid Ukstins Peate; David W. Peate; Stephen Self; Dougal A. Jerram; Michael R. Mawby; J.S. Marsh; Jodie A. Miller (2010). "The largest volcanic eruptions on Earth" (PDF). Earth-Science Reviews. 102 (3–4): 207. Bibcode:2010ESRv..102..207B. doi:10.1016/j.earscirev.2010.07.001. Archived (PDF) from the original on 2020-08-07. Retrieved 2020-03-11.
  5. ^ a b c (Data in this table are from Ward (2009) unless noted otherwise) Ward, Peter L. (2 April 2009). "Sulfur Dioxide Initiates Global Climate Change in Four Ways" (PDF). Thin Solid Films. 517 (11). Elsevier B. V.: 3188–3203. Bibcode:2009TSF...517.3188W. doi:10.1016/j.tsf.2009.01.005. Archived from the original (PDF) on 20 January 2010. Retrieved 2010-03-19. Supplementary Table I: "Supplementary Table to P.L. Ward, Thin Solid Films (2009) Major volcanic eruptions and provinces" (PDF). Teton Tectonics. Archived from the original (PDF) on 20 January 2010. Retrieved 8 September 2010. Supplementary Table II: "Supplementary References to P.L. Ward, Thin Solid Films (2009)" (PDF). Teton Tectonics. Archived from the original (PDF) on 20 January 2010. Retrieved 8 September 2010.
  6. ^ a b c d e f g h i Rossetti, Lucas; Lima, Evandro F.; Waichel, Breno L.; Hole, Malcolm J.; Simões, Matheus S.; Scherer, Claiton M.S. (2018-04-15). "Lithostratigraphy and volcanology of the Serra Geral Group, Paraná-Etendeka Igneous Province in Southern Brazil: Towards a formal stratigraphical framework". Journal of Volcanology and Geothermal Research. 355: 98–114. Bibcode:2018JVGR..355...98R. doi:10.1016/j.jvolgeores.2017.05.008. ISSN 0377-0273. Archived from the original on 2021-10-24. Retrieved 2021-06-15.
  7. ^ a b c d e f g h i BENITES, SUSANA; SOMMER, CARLOS A.; LIMA, EVANDRO F. DE; SAVIAN, JAIRO F.; HAAG, MAURICIO B.; MONCINHATTO, THIAGO R.; TRINDADE, RICARDO I.F. DA (2020). "Characterization of volcanic structures associated to the silicic magmatism of the Paraná-Etendeka Province, in the Aparados da Serra region, southern Brazil". Anais da Academia Brasileira de Ciências. 92 (2): e20180981. doi:10.1590/0001-3765202020180981. hdl:10183/220249. ISSN 1678-2690. PMID 32187251. S2CID 214583807. Archived from the original on 2021-10-24. Retrieved 2021-06-15.
  8. ^ Ambrose, Stanley H. (June 1998). "Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans" (PDF). Journal of Human Evolution. 34 (6). Elsevier B. V.: 623–651. Bibcode:1998JHumE..34..623A. doi:10.1006/jhev.1998.0219. PMID 9650103. Archived from the original (PDF) on 28 September 2010. Retrieved 5 August 2010.
  9. ^ a b c "What is a supervolcano? What is a supereruption?". www.usgs.gov. Archived from the original on 2019-09-25. Retrieved 2019-09-12.
  10. ^ a b c "Volcanic Explosivity Index: Measuring the size of an eruption". geology.com. Archived from the original on 2019-06-01. Retrieved 2019-09-12.
  11. ^ Antonio Costa; Victoria C. Smith; Giovanni Macedonio; Naomi E. Matthews (2014). "The magnitude and impact of the Youngest Toba Tuff super-eruption". Frontiers in Earth Science. 2: 16. Bibcode:2014FrEaS...2...16C. doi:10.3389/feart.2014.00016.
  12. ^ "VOGRIPA". www2.bgs.ac.uk. Archived from the original on 2021-04-23. Retrieved 2021-04-23.
  13. ^ a b c Takarada, Shinji; Hoshizumi, Hideo (2020-06-23). "Distribution and Eruptive Volume of Aso-4 Pyroclastic Density Current and Tephra Fall Deposits, Japan: A M8 Super-Eruption". Frontiers in Earth Science. 8: 170. Bibcode:2020FrEaS...8..170T. doi:10.3389/feart.2020.00170. ISSN 2296-6463.
  14. ^ "Lexique du substrat rocheux". dnr-mrn.gnb.ca. Archived from the original on 2019-12-22. Retrieved 2019-12-22.
  15. ^ "Archived copy" (PDF). Archived from the original (PDF) on 2019-12-12. Retrieved 2019-09-11.{{cite web}}: CS1 maint: archived copy as title (link)
  16. ^ a b Ingrid Ukstins Peate; Joel A. Baker; Mohamed Al-Kadasi; Abdulkarim Al-Subbary; Kim B. Knight; Peter Riisager; Matthew F. Thirlwall; David W. Peate; Paul R. Renne; Martin A. Menzies (2005). "Volcanic stratigraphy of large-volume silicic pyroclastic eruptions during Oligocene Afro-Arabian flood volcanism in Yemen". Bulletin of Volcanology. 68 (2). Springer: 135–156. Bibcode:2005BVol...68..135P. doi:10.1007/s00445-005-0428-4. S2CID 140160158.
  17. ^ Ewart, A.; Milner, S.C.; Armstrong, R.A.; Duncan, A.R. (1998). "Etendeka Volcanism of the Goboboseb Mountains and Messum Igneous Complex, Namibia. Part II: Voluminous Quartz Latite Volcanism of the Awahab Magma System". Journal of Petrology. 39 (2): 227–253. Bibcode:1998JPet...39..227E. doi:10.1093/petrology/39.2.227.
  18. ^ a b Tingey, David G.; Hart, Garret L.; Gromme, Sherman; Deino, Alan L.; Christiansen, Eric H.; Best, Myron G. (2013-08-01). "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.
  19. ^ Ort, Michael (22 September 1997). "La Garita Caldera". Northern Arizona University. Archived from the original on 19 May 2011. Retrieved 5 August 2010.
  20. ^ a b c d e Lipman, Peter W. (2007-11-02). "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}}: Cite journal requires |journal= (help)
  21. ^ Cannon, Eric. "4. Petrology – The Mid-Tertiary Ignimbrite Flare-Up". University of Colorado at Boulder. Archived from the original on 2012-10-13. Retrieved 5 August 2010.
  22. ^ Best, Myron G.; Scott R. B.; Rowley P. D.; Swadley W. C.; Anderson R. E.; Grommé C. S.; Harding A. E.; Deino A. L.; Christiansen E. H.; Tingey D. G.; Sullivan K. R. (1993). "Oligocene–Miocene caldera complexes, ash-flow sheets, and tectonism in the central and southeastern Great Basin". Field Trip Guidebook for Cordilleran/Rocky Mountain Sections of the Geological Society of America. Crustal Evolution of the Great Basin and the Sierra Nevada: 285–312.
  23. ^ Wörner, Gerhard; Konrad Hammerschmidt; Friedhelm Henjes-Kunst; Judith Lezaun; Hans Wilke (2000). "Geochronology (40Ar/39Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from Northern Chile (18–22°S): implications for magmatism and tectonic evolution of the central Andes". Revista Geológica de Chile. 27 (2). Archived from the original on 7 July 2011. Retrieved 5 August 2010.
  24. ^ a b Knott, Thomas; Branney, M.; Reichow, Marc; Finn, David; Tapster, Simon; Coe, Robert (June 2020). "Discovery of two new super-eruptions from the Yellowstone hotspot track (USA): Is the Yellowstone hotspot waning?". Geology. 48 (9): 934–938. Bibcode:2020Geo....48..934K. doi:10.1130/G47384.1. Retrieved 21 June 2022.
  25. ^ Lindsay, J. M.; S. de Silva; R. Trumbull; R. Emmermann; K. Wemmer (April 2001). "La Pacana caldera, N. Chile: a re-evaluation of the stratigraphy and volcanology of one of the world's largest resurgent calderas". Journal of Volcanology and Geothermal Research. 106 (1–2). Elsevier B. V.: 145–173. Bibcode:2001JVGR..106..145L. doi:10.1016/S0377-0273(00)00270-5.
  26. ^ a b c "Mangakino". VOGRIPA. Archived from the original on 9 December 2018. Retrieved 9 December 2018.
  27. ^ Topinka, Lyn (25 June 2009). "Description: Yellowstone Caldera, Wyoming". USGS. Archived from the original on 4 February 2012. Retrieved 6 August 2010.
  28. ^ Takahiro, Sonehara; Satoru, Harayama (1 November 2007). "Petrology of the Nohi Rhyolite and its related granitoids: A Late Cretaceous large silicic igneous field in central Japan". Journal of Volcanology and Geothermal Research. 167 (1–4): 57–80. Bibcode:2007JVGR..167...57S. doi:10.1016/j.jvolgeores.2007.05.012.
  29. ^ 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.
  30. ^ a b Morgan, Lisa A.; McIntosh, William C. (March 2005). "Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA". GSA Bulletin. 117 (3–4). Geological Society of America: 288–306. Bibcode:2005GSAB..117..288M. doi:10.1130/B25519.1.
  31. ^ Stetten, Nancy. "Plate Tectonics from the Middle of the Plate". Archived from the original on 10 March 2012. Retrieved 5 August 2010.
  32. ^ Huff, W.D.; Bergstrom, S.M.; Kolata, D.R. (October 1992). "Gigantic Ordovician volcanic ash fall in North America and Europe: Biological, tectonomagmatic, and event-stratigraphy significance". Geology. 20 (10). Geological Society of America: 875–878. Bibcode:1992Geo....20..875H. doi:10.1130/0091-7613(1992)020<0875:GOVAFI>2.3.CO;2.
  33. ^ Mason, Ben G.; Pyle, David M.; Oppenheimer, Clive (2004). "The size and frequency of the largest explosive eruptions on Earth". Bulletin of Volcanology. 66 (8): 735–748. Bibcode:2004BVol...66..735M. doi:10.1007/s00445-004-0355-9. S2CID 129680497.
  34. ^ a b Daisuke, Miura; Yutaka, Wada (2007). "Middle Miocene ash-flow calderas at the compressive margin of southwest Japan arc: Review and synthesis". The Journal of the Geological Society of Japan. 113 (7): 283–295. doi:10.5575/geosoc.113.283. Archived from the original on 6 December 2018. Retrieved 6 December 2018.
  35. ^ a b c Bindeman, Ilya N.; John W. Valley (May 2003). "Rapid generation of both high- and low-δ18O, large-volume silicic magmas at the Timber Mountain/Oasis Valley caldera complex, Nevada". GSA Bulletin. 115 (5). Geological Society of America: 581–595. Bibcode:2003GSAB..115..581B. doi:10.1130/0016-7606(2003)115<0581:RGOBHA>2.0.CO;2.
  36. ^ a b Ratté, J. C.; R. F. Marvin; C. W. Naeser; M. Bikerman (27 January 1984). "Calderas and Ash Flow Tuffs of the Mogollon Mountains, Southwestern New Mexico". Journal of Geophysical Research. 89 (B10). American Geophysical Union: 8713–8732. Bibcode:1984JGR....89.8713R. doi:10.1029/JB089iB10p08713. Archived from the original on 24 October 2021. Retrieved 18 August 2010.
  37. ^ Wilson, Colin J. N.; Blake, S.; Charlier, B. L. A.; Sutton, A. N. (2006). "The 26.5 ka Oruanui Eruption, Taupo Volcano, New Zealand: Development, Characteristics and Evacuation of a Large Rhyolitic Magma Body". Journal of Petrology. 47 (1): 35–69. Bibcode:2005JPet...47...35W. doi:10.1093/petrology/egi066.
  38. ^ Thouret, J. C.; Wörner, G.; Singer, B.; Finizola, A. (April 6, 2003). "EGS-AGU-EUG Joint Assembly, held in Nice, France; chapter: Valley Evolution, Uplift, Volcanism, and Related Hazards in the Central Andes of Peru" (PDF): 641–644. Archived from the original (PDF) on 21 July 2011. Retrieved 5 August 2010. {{cite journal}}: Cite journal requires |journal= (help)
  39. ^ Morgan, Lisa (30 March 2004). "The floor of Yellowstone Lake is anything but quiet: Volcanic and hydrothermal processes in a large lake above a magma chamber". National Park Service and United States Geological Survey. Archived from the original on 30 May 2010. Retrieved 5 August 2010.
  40. ^ "Corbetti Caldera". VOGRIPA. Archived from the original on 2018-12-09. Retrieved 9 December 2018.
  41. ^ "How Volcanos Work: Cerro Galan". San Diego State University. Archived from the original on 6 February 2012. Retrieved 5 August 2010.
  42. ^ "Wall Mountain Tuff". National Park Service. Archived from the original on 14 February 2012. Retrieved 5 August 2010.
  43. ^ a b "VHP Photo Glossary: Effusive Eruption". USGS. 29 December 2009. Archived from the original on 27 May 2010. Retrieved 25 August 2010.
  44. ^ Ruben, Ken (6 January 2008). "A Brief History of the Pu'u 'O'o Eruption of Kilauea". School of Ocean and Earth Science and Technology. Archived from the original on 7 February 2012. Retrieved 27 August 2010.
  45. ^ a b Frank Press & Raymond Siever (1978). "Volcanism". Earth (2nd ed.). San Francisco: W. F. Freeman and Company. pp. 348–378. ISBN 0-7167-0289-4.
  46. ^ "Smithsonian Institution – Global Volcanism Program: Worldwide Holocene Volcano and Eruption Information". Volcano.si.edu. Archived from the original on 2012-10-24. Retrieved 2015-12-16.
  47. ^ a b c d e f g Martin, B. S.; Petcovic, H. L.; Reidel, S. P. (May 2005). "Goldschmidt Conference 2005: Field Trip Guide to the Columbia River Basalt Group" (PDF). doi:10.2172/15016367. Archived (PDF) from the original on 3 October 2012. Retrieved 1 September 2010. {{cite journal}}: Cite journal requires |journal= (help)
  48. ^ Coffin, Millard F.; Millard F. Coffin; Olav Eldholm (1994). "Large igneous provinces: Crustal structure, dimensions, and external consequences". Reviews of Geophysics. 32 (1): 1–36. Bibcode:1994RvGeo..32....1C. doi:10.1029/93RG02508. Archived from the original on 28 October 2011. Retrieved 27 August 2010.
  49. ^ T. Worthington; Tim J. Worthington; Roger Hekinian; Peter Stoffers; Thomas Kuhn; Folkmar Hauff (30 May 2006). "Osbourn Trough: Structure, geochemistry and implications of a mid-Cretaceous paleospreading ridge in the South Pacific". Earth and Planetary Science Letters. 245 (3–4). Elsevier B. V.: 685–701. Bibcode:2006E&PSL.245..685W. doi:10.1016/j.epsl.2006.03.018.
  50. ^ Taylor, Brian (31 January 2006). "The single largest oceanic plateau: Ontong Java-Manihiki-Hikurangi" (PDF). Earth and Planetary Science Letters. 241 (3–4). Elsevier B. V.: 372–380. Bibcode:2006E&PSL.241..372T. doi:10.1016/j.epsl.2005.11.049. Archived from the original (PDF) on 20 November 2008. Retrieved 20 September 2010.
  51. ^ Kerr, Andrew C.; Mahoney, John J. (2007). "Oceanic plateaus: Problematic plumes, potential paradigms". Chemical Geology. 241 (3–4): 332–353. Bibcode:2007ChGeo.241..332K. doi:10.1016/j.chemgeo.2007.01.019.
  52. ^ Weis, D.; Frey, F. A. "Kerguelen Plateau—Broken Ridge: A Major Lip Related to the Kerguelen Plume" (PDF). Seventh Annual V. M. Goldschmidt Conference. Archived (PDF) from the original on 5 June 2011. Retrieved 5 August 2010.
  53. ^ Coffin, M.F.; Pringle, M.S.; Duncan, R.A.; Gladczenko, T.P.; Storey, M.; Müller, R.D.; Gahagan, L.A. (2002). "Kerguelen Hotspot Magma Output since 130 Ma". Journal of Petrology. 43 (7): 1121–1137. Bibcode:2002JPet...43.1121C. doi:10.1093/petrology/43.7.1121.
  54. ^ D. W. Jolley; B. R. Bell, eds. (2002). The North Atlantic Igneous Province: Stratigraphy, Tectonic, Volcanic and Magmatic Processes. Special Publication No. 197. Geological Society of London. ISBN 1-86239-108-4. ISSN 0305-8719.
  55. ^ Cannon, Eric. "Introduction – The Mid-Tertiary Ignimbrite Flare-Up". Archived from the original on 2008-12-02. Retrieved 9 September 2010.
  56. ^ Hoernle, Kaj; Folkmar Hauff; Paul van den Bogaard (August 2004). "70 m.y. history (139–69 Ma) for the Caribbean large igneous province". Geology. 32 (8). Geological Society of America: 697–700. Bibcode:2004Geo....32..697H. doi:10.1130/G20574.1.
  57. ^ Goodwin, Anna; Wyles, Jon & Morley, Alex (2001). "The Siberian Traps". Palaeobiology and Biodiversity Research Group, Department of Earth Sciences, University of Bristol. Archived from the original on 11 August 2010. Retrieved 5 August 2010.
  58. ^ Segev, A. (4 March 2002). "Flood basalts, continental breakup and the dispersal of Gondwana: evidence for periodic migration of upwelling mantle flows (plumes)" (PDF). European Geosciences Union Special Publication Series. 2: 171–191. Bibcode:2002SMSPS...2..171S. doi:10.5194/smsps-2-171-2002. Archived (PDF) from the original on 24 July 2011. Retrieved 5 August 2010.
  59. ^ O'Neill, C.; Müller, R. D.; Steinberger, B. (2003). "Revised Indian plate rotations based on the motion of Indian Ocean hotspots" (PDF). Earth and Planetary Science Letters. 215 (1–2). Elsevier B. V.: 151–168. Bibcode:2003E&PSL.215..151O. CiteSeerX 10.1.1.716.4910. doi:10.1016/S0012-821X(03)00368-6. Archived from the original (PDF) on 26 July 2011. Retrieved 20 September 2010.
  60. ^ O'Connor, J. M.; le Roex, A. P. (1992). "South Atlantic hot spot-plume systems. 1: Distribution of volcanism in time and spac". Earth and Planetary Science Letters. 113 (3). Elsevier B. V.: 343–364. Bibcode:1992E&PSL.113..343O. doi:10.1016/0012-821X(92)90138-L.
  61. ^ McHone, Greg. "CAMP site introduction". Auburn University. Archived from the original on 8 December 2011. Retrieved 5 August 2010.
  62. ^ "India's Smoking Gun: Dino-Killing Eruptions". Science Daily. 10 August 2005. Archived from the original on 29 March 2010. Retrieved 5 August 2010.
  63. ^ Chatterjee, Sankar; Mehrotra, Naresh M. (2009). "The Significance of the Contemporaneous Shiva Impact Structure and Deccan Volcanism at the KT Boundary". Abstracts with Programs. 2009 Annual Meeting of the Geological Society of America. Vol. 41. Portland. p. 160. Archived from the original on 6 April 2010. Retrieved 22 September 2010.
  64. ^ Lo, Ching-Hua; Sun-Lin Chung; Tung-Yi Lee; Genyao Wu (2002). "Age of the Emeishan Flood magmatism and relations to Permian-Triassic boundary events" (PDF). Earth and Planetary Science Letters. 198 (3–4). Elsevier: 449–458. Bibcode:2002E&PSL.198..449L. doi:10.1016/S0012-821X(02)00535-6. Archived (PDF) from the original on 25 July 2011. Retrieved 5 August 2010.
  65. ^ Gittings, Fred W. (October 2008). Geological Report on the Muskox Property: Coppermine River Area, Nunavut (PDF). Vol. NTS 86 O/6. Archived from the original (PDF) on 15 July 2011. Retrieved 20 September 2010.
  66. ^ Peate, Ingrid Ukstins; et al. (2005). "Volcanic stratigraphy of large-volume silicic pyroclastic eruptions during Oligocene Afro-Arabian flood volcanism in Yemen". Bulletin of Volcanology. 68 (2). Springer: 135–156. Bibcode:2005BVol...68..135P. doi:10.1007/s00445-005-0428-4. S2CID 140160158.
  67. ^ Peate, Ingrid Ukstins; et al. (30 June 2003). "Correlation of Indian Ocean tephra to individual Oligocene silicic eruptions from Afro-Arabian flood volcanism" (PDF). Earth and Planetary Science Letters. 211 (3–4). Elsevier B. V.: 311–327. Bibcode:2003E&PSL.211..311U. doi:10.1016/S0012-821X(03)00192-4. Archived from the original (PDF) on 20 November 2008. Retrieved 5 August 2010.
  68. ^ Topinka, Lyn (27 August 2002). "Columbia Plateau, Columbia River Basin, Columbia River Flood Basalts". USGS. Archived from the original on 7 February 2012. Retrieved 5 August 2010.

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