Volcanic Explosivity Index

In volcanology, the Volcanic Explosivity Index (VEI) is the way to measure the strength of a volcanic eruption. The Volcanic Explosivity Index measures how large or strong volcanic eruptions are. The index is a scale of 0 to 8. 0 is very small, and 8 is huge and very rare.

The largest eruption in modern times, the 1980 eruption of Mount St. Helens, was a 5 on the index. The Oruanui eruption of the Taupo Volcano in New Zealand was the world’s largest known eruption in the past 70,000 years was an 8. Another eruption of the Taupo volcano happened about 1,800 years ago. It was the most violent eruption in the world in the last 5,000 years. Mt Tambora was a 7 on the Volcanic Explosivity Index. Supervolcanoes have a Volcanic Explosivity Index of 8; and if the definition is expanded, also include volcanoes with a Volcanic Explosivity Index of 7.

 VEI Ejecta volume(bulk) Classification Description Plume Periodicity Troposphericinjection Stratosphericinjection Examples 0 < 104 m3  Hawaiian  Effusive  < 100 m  constant  negligible  none Kīlauea (current), Mawson Peak (current), Dallol (2011), Holuhraun (2014-2015), Fagradalsfjall (2021-2023), Mauna Loa (1975, 1984, 2022)  1 > 104 m3  Hawaiian / Strombolian  Gentle    daily  minor  none Yakedake (1995), Raoul Island (2006), Havre Seamount (2012), Dieng Volcanic Complex (1964, 1979, 2017), Nyiragongo (1977, 2002, 2021) 2 > 106 m3  Strombolian / Vulcanian  Explosive  1–5 km  2 weeks  moderate  none Stromboli (since 1934), Etna (current), Unzen (1792), Ruang (1871), Ritter Island (1888), Galeras (1993), Whakaari / White Island (2019) 3 > 107 m3  Strombolian / Vulcanian / Peléan / Sub-Plinian  Severe  3–15 km  3 months  substantial  possible Surtsey (1963-1967), Nevado del Ruiz (1985), Redoubt (1989-1990), Soufrière Hills (1997), Ontake (2014), Fuego (2018), Cumbre Vieja (2021) 4 > 0.1 km3  Peléan / Plinian / Sub-Plinian Catastrophic  > 10 km  18 months  substantial  definite Laki (1783), Bandai (1888), Pelée (1902), Lamington (1951), Eyjafjallajökull (2010), Merapi (2010), Taal (2020), Semeru (2021) 5 > 1 km3  Peléan / Plinian  Cataclysmic  > 10 km  12 years  substantial  significant Vesuvius (79), Fuji (1707), Tarawera (1886), St. Helens (1980), El Chichón (1982), Puyehue (2011), Hunga Tonga–Hunga Haʻapai (2022) 6 > 10 km3  Plinian / Ultra-Plinian Colossal  > 20 km  50–100 years  substantial  substantial Santorini (1620 BC), Lake Ilopango (450), Huaynaputina (1600), Krakatoa (1883), Santa Maria (1902), Novarupta (1912), Pinatubo (1991) 7 > 100 km3  Ultra-Plinian  Super-colossal  > 20 km  500–1,000 years  substantial  substantial Long Valley (760 kyr), Campi Flegrei (37 kyr), Aira (22 kyr), Mazama (5700 BC), Kikai (4300 BC), Samalas (1257), Tambora (1815) 8 > 1,000 km3  Ultra-Plinian  Mega-colossal  > 20 km  > 50,000 years  vast  vast Flat Landing Brook (Ordovician), Wah Wah Springs (30 Mya), La Garita (26.3 Mya), Yellowstone (2.1 Mya, 640 kyr), Toba (74 kyr), Taupō (26.5 kyr)

About 40 eruptions of VEI-8 magnitude within the last 132 million years (Mya) have been identified, of which 30 occurred in the past 36 million years. Considering the estimated frequency is on the order of once in 50,000 years, there are likely many such eruptions in the last 132 Mya that are not yet known. Based on incomplete statistics, other authors assume that at least 60 VEI-8 eruptions have been identified. The most recent is Lake Taupō's Oruanui eruption, more than 27,000 years ago, which means that there have not been any Holocene eruptions with a VEI of 8.

References

 Further reading 



 Other websites 
 VEI glossary entry  from a USGS website
 How to measure the size of a volcanic eruption , from The Guardian
 The size and frequency of the largest explosive eruptions on Earth, a 2004 article from the Bulletin of Volcanology
 List of Large Holocene Eruptions (VEI > 4) from the Smithsonian Global Volcanism Program 

Category:Volcanology

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