Plinian eruption

Short description: Type of volcanic eruption

Plinian eruption: 1: ash plume; 2: magma conduit; 3: volcanic ash fall; 4: layers of lava and ash; 5: stratum; 6: magma chamber 1822 artist's impression of the eruption of Mount Vesuvius in 79, depicting what the AD 79 eruption may have looked like, by the English geologist George Julius Poulett Scrope. Lightning is depicted around the rising column of ash and gas.

Plinian eruptions or Vesuvian eruptions are volcanic eruptions characterized by their similarity to the eruption of Mount Vesuvius in 79 AD, which destroyed the ancient Roman cities of Herculaneum and Pompeii. The eruption was described in a letter[1] written by Pliny the Younger, after the death of his uncle Pliny the Elder.

Plinian eruptions eject columns of volcanic debris and hot gases high into the stratosphere, the second layer of Earth's atmosphere. They eject a large amount of pumice and have powerful, continuous gas-driven eruptions.

Eruptions can end in less than a day, or continue for days or months. The longer eruptions begin with production of clouds of volcanic ash, sometimes with pyroclastic surges. The amount of magma ejected can be so large that it depletes the magma chamber below, causing the top of the volcano to collapse, resulting in a caldera. Fine ash and pulverized pumice can be deposited over large areas. Plinian eruptions are often accompanied by loud sounds. The sudden discharge of electrical charges accumulated in the air around the ascending column of volcanic ashes also often causes lightning strikes, as depicted by the English geologist George Julius Poulett Scrope in his painting of 1822 or observed during 2022 Hunga Tonga–Hunga Ha'apai eruption and tsunami.[2]

The lava is usually dacitic or rhyolitic, rich in silica. Basaltic, low-silica lavas rarely produce Plinian eruptions unless specific conditions are met (low magma water content <2%, moderate temperature, and rapid crystallization);[3] a recent basaltic example is the 1886 eruption of Mount Tarawera on New Zealand's North Island.[4]

## Contents

* 1 Pliny's description
* 2 Examples
* 3 Ultra-Plinian
* 4 See also
* 5 References
* 6 External links

## Pliny's description

A stone pine, the type of tree used by Pliny the Younger to describe the eruption

Pliny the Younger described the initial observations of his uncle, Pliny the Elder, of the 79 AD eruption of Mount Vesuvius:[5]

> On the 24th of August, about one in the afternoon, my mother desired him to observe a cloud which appeared of a very unusual size and shape. He had just taken a turn in the sun and, after bathing himself in cold water, and making a light luncheon, gone back to his books: he immediately arose and went out upon a rising ground from whence he might get a better sight of this very uncommon appearance. A cloud, from which mountain was uncertain, at this distance (but it was found afterwards to come from Mount Vesuvius), was ascending, the appearance of which I cannot give you a more exact description of than by likening it to that of a pine tree, for it shot up to a great height in the form of a very tall trunk, which spread itself out at the top into a sort of branches; occasioned, I imagine, either by a sudden gust of air that impelled it, the force of which decreased as it advanced upwards, or the cloud itself being pressed back again by its own weight, expanded in the manner I have mentioned; it appeared sometimes bright and sometimes dark and spotted, according as it was either more or less impregnated with earth and cinders. This phenomenon seemed to a man of such learning and research as my uncle extraordinary and worth further looking into.

> - Sixth Book of Letters, Letter 16, translation by William Melmoth

Pliny the Elder set out to rescue the victims from their perilous position on the shore of the Bay of Naples, and launched his galleys, crossing the bay to Stabiae (near the modern town of Castellammare di Stabia). Pliny the Younger provided an account of his death, and suggested that he collapsed and died through inhaling poisonous gases emitted from the volcano. His body was found buried under the ashes of the eruption with no apparent injuries on 26 August, after the plume had dispersed, which would be consistent with asphyxiation or poisoning, but also with a heart attack, asthma attack, or stroke.

## Examples

Eruption cloud from Redoubt Volcano on 21 April 1990 as viewed to the west from the Kenai Peninsula, more than 60 km (37 mi) from the volcano's summit April 2015, subplinian eruption of Calbuco

* The Long Valley Caldera eruption in Eastern California, United States, which happened over 760,000 years ago.
* The 10,950 BC eruption of Lake Laach in Rhineland-Palatinate, Germany.
* The 4860 BC eruption forming Crater Lake in Oregon, United States.
* The 1645 BC eruption of Thera in the south Aegean Sea, Greece.
* The 400s BC eruption of the Bridge River Vent in British Columbia, Canada.
* The 79 AD eruption of Mount Vesuvius in Pompeii, Italy. It was the prototypical Plinian eruption.
* The 180 AD Lake Taupo eruption in New Zealand.
* The 946 eruption of Paektu Mountain in China / North Korea.
* The 1257 eruption of Mount Samalas in Lombok, Indonesia.
* The 1600 eruption of Huaynaputina in Peru.
* The 1667 and 1739 eruptions of Mount Tarumae in Hokkaido, Japan.[6]
* The 1707 eruption of Mount Fuji in Japan.
* The 1754 eruption of Taal in the Philippines.
* The 1815 eruption of Mount Tambora in the island of Sumbawa, Indonesia.
* The 1883 eruption of Krakatoa in Sunda Strait, Indonesia.
* The 1886 eruption of Mount Tarawera in New Zealand.
* The 1902 eruption of Santa María in Guatemala.[7]
* The 1912 eruption of Novarupta in Alaska, United States, the largest volcanic eruption of the 20th century.
* The 1929 eruptions of Hokkaido-Komagatake in Japan.
* The 1932 eruption of Cerro Azul\Quizapu in Chile.
* The 1955-1957 eruptions of Bezymianny in Russia.
* The 1980 eruption of Mount St. Helens in Washington State.
* The 1982 eruption of El Chichón in Chiapanecan Volcanic Arc, Chiapas, Mexico.
* The 1991 eruption of Mount Pinatubo in Zambales, Central Luzon, Philippines.
* The June 2009 eruption of Sarychev Peak in Russia.
* The 2011 eruption of Grímsvötn in Iceland
* The 2011–2012 Puyehue-Cordón Caulle eruption in Chile.
* The 2014 eruption of Tungurahua volcano in Cordillera Oriental of Ecuador.
* The 2015 eruption of Calbuco in Chile.
* The 2020 eruption of Taal Volcano in the Philippines.
* The 2021 eruption of Fukutoku-Okanoba in Japan.[8]
* The 2022 eruption of Hunga Tonga–Hunga Ha'apai in Tonga.
* The 2023 eruption of Bezymianny in Russia.
* The 2023 eruption of Shiveluch in Russia.
* The 2024 eruption of Mount Ruang in Indonesia.
* The 2025 eruption of Hayli Gubbi in Ethiopia.

## Ultra-Plinian

In 1980, the volcanologist George P. L. Walker proposed the Hatepe eruption as the representative of a new class called ultra-Plinian deposits, based on its exceptional dispersive power and eruptive column height.[9] A dispersal index of 50,000 square kilometres (19,000 sq mi) has been proposed as a cutoff for an ultra-Plinian eruption.[9] In the criteria of Volcanic Explosivity Index, recognizing an eruption as ultra-Plinian would make it at least VEI-5.[10]

The threshold for ultra-Plinian eruptions is an eruptive column height of 45 km (28 mi),[11] or 41 km (25 mi) more recently.[12] The few instances of eruptions that lie at the transition between Plinian and ultra-Plinian include the P3 phase of 1257 Samalas eruption,[13] 1991 eruption of Mount Pinatubo,[12] the Plinian phase of the Campanian Ignimbrite,[14] Tsankawi Pumice Bed of Tshirege Member of Bandelier Tuff,[15] and the 1902 eruption of Santa María.[16]

The once unequivocal ultra-Plinian classification of the Hatepe eruption has been called into question, with recent evidence showing that it is an artifact of an unrecognized shift in the wind field rather than extreme eruptive vigor.[17][18]

## See also

* Peléan eruption, related to the explosive eruptions of the Mount Pelée
* Types of volcanic eruptions
* List of largest volcanic eruptions
* Ignimbrite

## References

1. ↑ "Pliny Letter 6.16". http://www.yorku.ca/pswarney/2100/pliny-6-16-20.htm.
2. ↑ "Hunga Tonga volcano triggered nearly 400,000 lightning strikes". 17 January 2022. https://wildfiretoday.com/2022/01/17/hunga-tonga-volcano-triggered-nearly-400000-lightning-strikes/.
3. ↑ Bamber, Emily; Arzilli, Fabio (2020). "Pre- and syn-eruptive conditions of a basaltic Plinian eruption at Masaya Volcano, Nicaragua: The Masaya Triple Layer". Journal of Volcanology and Geothermal Research 392 (15 February 2020). doi:10.1016/j.jvolgeores.2019.106761.
4. ↑ "Okataina Volcanic Centre/ Mt Tarawera Volcano". https://www.gns.cri.nz/Home/Learning/Science-Topics/Volcanoes/New-Zealand-Volcanoes/Okataina-Volcanic-Centre-Mt-Tarawera-Volcano.
5. ↑ Pliny's Letters. 1915. pp. 473–481. https://archive.org/stream/letterswithengli01plinuoft/letterswithengli01plinuoft_djvu.txt.
6. ↑ Enlightenment activities for improvement on disasters. "From 23–27 January 2006 Tarumae volcano [eruption], Japan, 4 cities near volcanoes." [full citation needed]
7. ↑ Williams, Stanley N.; Self, Stephen (1983). "The October 1902 plinian eruption of Santa Maria volcano, Guatemala". Journal of Volcanology and Geothermal Research 16 (1–2): 33–56. doi:10.1016/0377-0273(83)90083-5. Bibcode: 1983JVGR...16...33W.
8. ↑ [Authors] (2022). “Title of abstract.” In *AGU 2022 Fall Meeting Abstracts*, V16A..03T. Retrieved from https://ui.adsabs.harvard.edu/abs/2022AGUFM.V16A..03T/abstract
9. ↑ 9.0 9.1 Walker, G. P. L. (1980-08-01). "The Taupo pumice: Product of the most powerful known (ultraplinian) eruption?" (in en). Journal of Volcanology and Geothermal Research 8 (1): 69–94. doi:10.1016/0377-0273(80)90008-6. ISSN 0377-0273. Bibcode: 1980JVGR....8...69W.
10. ↑ Newhall, Christopher G.; Self, Stephen (1982). "The volcanic explosivity index (VEI) an estimate of explosive magnitude for historical volcanism" (in en). Journal of Geophysical Research 87 (C2): 1231. doi:10.1029/JC087iC02p01231. ISSN 0148-0227. Bibcode: 1982JGR....87.1231N. http://doi.wiley.com/10.1029/JC087iC02p01231.
11. ↑ Pyle, David M. (1989-01-01). "The thickness, volume and grainsize of tephra fall deposits" (in en). Bulletin of Volcanology 51 (1): 1–15. doi:10.1007/BF01086757. ISSN 1432-0819. Bibcode: 1989BVol...51....1P.
12. ↑ 12.0 12.1 Bonadonna, Costanza; Costa, Antonio (2013-07-25). "Plume height, volume, and classification of explosive volcanic eruptions based on the Weibull function" (in en). Bulletin of Volcanology 75 (8): 742. doi:10.1007/s00445-013-0742-1. ISSN 1432-0819. Bibcode: 2013BVol...75..742B.
13. ↑ Vidal, Céline M.; Komorowski, Jean-Christophe; Métrich, Nicole; Pratomo, Indyo; Kartadinata, Nugraha; Prambada, Oktory; Michel, Agnès; Carazzo, Guillaume et al. (2015-08-08). "Dynamics of the major plinian eruption of Samalas in 1257 A.D. (Lombok, Indonesia)" (in en). Bulletin of Volcanology 77 (9): 73. doi:10.1007/s00445-015-0960-9. ISSN 1432-0819. Bibcode: 2015BVol...77...73V.
14. ↑ Scarpati, Claudio; Perrotta, Annamaria (2016-03-09). "Stratigraphy and physical parameters of the Plinian phase of the Campanian Ignimbrite eruption". Geological Society of America Bulletin 128 (7–8): 1147–1159. doi:10.1130/b31331.1. ISSN 0016-7606. Bibcode: 2016GSAB..128.1147S.
15. ↑ Self, Stephen; Wolff, John ; Wright, John (2021-12). Tsankawi Pumice Fall Unit B, a Very Widespread and Powerfully Emplaced Plinian Deposit. AGU Fall Meeting 2021.
16. ↑ Williams, Stanley N.; Self, Stephen (1983-04-01). "The October 1902 plinian eruption of Santa Maria volcano, Guatemala" (in en). Journal of Volcanology and Geothermal Research 16 (1): 33–56. doi:10.1016/0377-0273(83)90083-5. ISSN 0377-0273. Bibcode: 1983JVGR...16...33W.
17. ↑ Houghton, B.F.; Carey, R.J.; Rosenberg, M.D. (2014-05-01). "The 1800a Taupo eruption: "III wind" blows the ultraplinian type event down to Plinian". Geology 42 (5): 459–461. doi:10.1130/g35400.1. ISSN 1943-2682. Bibcode: 2014Geo....42..459H.
18. ↑ Bonadonna, C.; Cioni, R.; Costa, A.; Druitt, T.; Phillips, J.; Pioli, L.; Andronico, D.; Harris, A. et al. (2016-10-28). "MeMoVolc report on classification and dynamics of volcanic explosive eruptions" (in en). Bulletin of Volcanology 78 (11): 84. doi:10.1007/s00445-016-1071-y. ISSN 1432-0819. Bibcode: 2016BVol...78...84B.

## External links

* USGS Photo Glossary Entry for Plinian Eruptions
* Volcanic mesocyclones

Template:Types of volcanic eruptions

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