Plinian eruption

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

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

• The Long Valley Caldera eruption in Eastern California, United States, which happened over 760,000 years ago.
• The Mount Toba 72,000 BC eruption at the site of present-day Lake Toba in Sumatra, Indonesia.
• 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 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
  Washington
  in the western United States.
• The 1982 eruption of
  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 2011–2012 Puyehue-Cordón Caulle eruption in Chile.
• The 2014 eruption of
  Tungurahua volcano in Cordillera Oriental of Ecuador
  .
• The 2020 eruption of Taal Volcano in the Philippines.
• The
  2022 eruption of Hunga Tonga–Hunga Ha'apai in Tonga
  .

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

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

References