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 marked 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/Vesuvian eruptions are marked by columns of volcanic debris and hot gases ejected high into the stratosphere, the second layer of Earth's atmosphere. The key characteristics are the ejection of a large amount of pumice and very powerful continuous gas-driven eruptions.

Short eruptions can end in less than a day, but longer events can continue for several 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 noises, such as those generated by the 1883 eruption of Krakatoa. 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]

Pliny's description

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

Pliny described his uncle's involvement from the first observation of the eruption:[5]

On August 24th, 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 interred under the ashes of the eruption with no apparent injuries on 26 August, after the plume had dispersed, confirming asphyxiation or poisoning.

Examples

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

Ultra-Plinian

In 1980, volcanologist George P. L. Walker proposed Hatepe eruption as the representative of a new class called ultra-Plinian deposits, based on its exceptional dispersive power and eruptive column height.[7] A dispersal index of 50,000 square kilometres (19,000 sq mi) has been proposed as a cutoff for an ultra-Plinian eruption.[7] In the criteria of Volcanic Explosivity Index, recognizing an eruption as ultra-Plinian would make it at least VEI-5 or higher.[8]

The threshold for ultra-Plinian eruptions is defined by an eruptive column height of 45 km (28 mi),[9] or 41 km (25 mi) more recently.[10] The few instances of eruptions that lie at the transition between Plinian and ultra-Plinian include the P3 phase of 1257 Samalas eruption,[11] 1991 eruption of Mount Pinatubo,[10] the Plinian phase of the Campanian Ignimbrite,[12] Tsankawi Pumice Bed of Tshirege Member of Bandelier Tuff,[13] and the 1902 eruption of Santa María (volcano).[14]

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.[15][16]

See also

References

  1. ↑ "Pliny Letter 6.16". Retrieved 22 November 2022.
  2. ↑ "Hunga Tonga volcano triggered nearly 400,000 lightning strikes". 17 January 2022.
  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): 106761. doi:10.1016/j.jvolgeores.2019.106761. S2CID 214320363.
  4. ↑ "Okataina Volcanic Centre/ Mt Tarawera Volcano". GNS Science. Retrieved 15 January 2020.
  5. ↑ Pliny's Letters. 1915. pp. 473–481.
  6. ↑ Enlightenment activities for improvement on disasters. From 23–27 January 2006 Tarumae volcano [eruption], Japan, 4 cities near volcanoes.
  7. 1 2 Walker, G. P. L. (1980-08-01). "The Taupo pumice: Product of the most powerful known (ultraplinian) eruption?". Journal of Volcanology and Geothermal Research. 8 (1): 69–94. doi:10.1016/0377-0273(80)90008-6. ISSN 0377-0273.
  8. ↑ Newhall, Christopher G.; Self, Stephen (1982). "The volcanic explosivity index (VEI) an estimate of explosive magnitude for historical volcanism". Journal of Geophysical Research. 87 (C2): 1231. doi:10.1029/JC087iC02p01231. ISSN 0148-0227.
  9. ↑ Pyle, David M. (1989-01-01). "The thickness, volume and grainsize of tephra fall deposits". Bulletin of Volcanology. 51 (1): 1–15. doi:10.1007/BF01086757. ISSN 1432-0819.
  10. 1 2 Bonadonna, Costanza; Costa, Antonio (2013-07-25). "Plume height, volume, and classification of explosive volcanic eruptions based on the Weibull function". Bulletin of Volcanology. 75 (8): 742. doi:10.1007/s00445-013-0742-1. ISSN 1432-0819.
  11. ↑ Vidal, Céline M.; Komorowski, Jean-Christophe; Métrich, Nicole; Pratomo, Indyo; Kartadinata, Nugraha; Prambada, Oktory; Michel, Agnès; Carazzo, Guillaume; Lavigne, Franck; Rodysill, Jessica; Fontijn, Karen; Surono (2015-08-08). "Dynamics of the major plinian eruption of Samalas in 1257 A.D. (Lombok, Indonesia)". Bulletin of Volcanology. 77 (9): 73. doi:10.1007/s00445-015-0960-9. ISSN 1432-0819.
  12. ↑ 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.
  13. ↑ 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.
  14. ↑ Williams, Stanley N.; Self, Stephen (1983-04-01). "The October 1902 plinian eruption of Santa Maria volcano, Guatemala". Journal of Volcanology and Geothermal Research. 16 (1): 33–56. doi:10.1016/0377-0273(83)90083-5. ISSN 0377-0273.
  15. ↑ 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.
  16. ↑ Bonadonna, C.; Cioni, R.; Costa, A.; Druitt, T.; Phillips, J.; Pioli, L.; Andronico, D.; Harris, A.; Scollo, S.; Bachmann, O.; Bagheri, G.; Biass, S.; Brogi, F.; Cashman, K.; Dominguez, L. (2016-10-28). "MeMoVolc report on classification and dynamics of volcanic explosive eruptions". Bulletin of Volcanology. 78 (11): 84. doi:10.1007/s00445-016-1071-y. hdl:11568/903131. ISSN 1432-0819.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.