A Plinian eruption is a kind of volcanic eruption which is similar to that of Mount Vesuvius in the year 79 AD. It is named after Pliny the Younger who wrote the only surviving eyewitness account of the eruption. That eruption of Vesuvius killed Pliny the Elder, the uncle of Pliny the Younger.
Short eruptions can end in less than a day. Longer ones can take several days to months. These eruptions begin with clouds of volcanic ash and occasionally pyroclastic flows. Sometimes the amount of magma erupted is so large that the top of the volcano collapses. This leaves a caldera behind. Fine ash can deposit over large areas. Plinian eruptions often happen with loud noises, such as those created by Krakatoa.
Large Plinian eruptionsEdit
Some examples of large Plinian eruptions that formed calderas include the following:
- the 2022 Hunga Tonga eruption in Tonga;
- the 1991 Mount Pinatubo eruption in Luzon in the Philippines;
- the 1980 eruption of Mount St. Helens in Washington, United States;
- the 1883 eruption of Krakatoa in Indonesia;
- the 1815 eruption of Mount Tambora, also in Indonesia;
- the 1667 and 1739 eruptions of Mount Tarumae in Japan;
- the 1645 BC eruption of Santorini caldera in Greece;
- the 4860 BC eruption forming Crater Lake in Oregon, United States;
- the 11000 BC eruption of the Laacher See in Germany;
- the Long Valley Caldera eruption in eastern California, United States over 760,000 years ago;
- and, of course, the AD 79 eruption of Mount Vesuvius in Italy, which was the prototypical Plinian eruption.
Pliny wrote about what his uncle's did after first seeing the eruption:
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
Pliny the Elder went to rescue some of the victims. He sailed across the Gulf of Naples to Stabiae (near the modern town of Castellammare di Stabia). Pliny the Younger wrote an account of his death, and suggested that he collapsed and died through inhaling poisonous gases emitted by the volcano. His body was found buried under the ashes of the Vesuvius with no apparent injuries on 26 August, after the plume had dispersed. This confirmed the death through asphyxiation or poisoning.
- "The eruption of Mt. Vesuvius - timeline and eyewitness account" (PDF). Melburne Museum. 2009. Archived from the original (pdf) on 2013-08-10. Retrieved 20 September 2009.
- Enlightenment activities for improvement on disasters from Tarumae Volcano, Japan, Cities on Volcanoes 4, 23-27 January 2006
- "C. PLINII CAECILII SECVNDI EPISTVLARVM LIBER SEXTVS" [C. Plinius Caecilius' II Epistle Book VI] (in Latin). Retrieved 20 September 2009.