thumb|270px|VEI and ejecta volume correlation

The volcanic explosivity index (VEI) is a scale used to measure the size of explosive volcanic eruptions. It was devised by Christopher G. Newhall of the United States Geological Survey and Stephen Self in 1982.

Volume of products, eruption cloud height, and qualitative observations (using terms ranging from "gentle" to "mega-colossal") are used to determine the explosivity value. The scale is open-ended with the largest eruptions in history given a magnitude of 8. A value of 0 is given for non-explosive eruptions, defined as less than of tephra ejected; and 8 representing a supervolcanic eruption that can eject (240 cubic miles) of tephra and have a cloud column height of over . The scale is logarithmic, with each interval on the scale representing a tenfold increase in observed ejecta criteria, with the exception of between VEI-0, VEI-1 and VEI-2.

Classification

With indices running from 0 to 8, the VEI associated with an eruption is dependent on how much volcanic material is thrown out, to what height, and how long the eruption lasts. The scale is logarithmic from VEI-2 and up; an increase of 1 index indicates an eruption that is 10 times as powerful. As such, there is a discontinuity in the definition of the VEI between indices 1 and 2. The lower border of the volume of ejecta jumps by a factor of one hundred, from , while the factor is ten between all higher indices. In the following table, the frequency of each VEI indicates the approximate frequency of new eruptions of that VEI or higher.

<!-- Please note that this is not a database of eruptions and only a small number of examples should be listed here, fitting on one line on PC. Examples used should be eruptions that are significantly noteworthy, more recent examples where appropriate, and not using the same volcano in more than one category. Eruptions must also have a confirmed VEI from the Global Volcanism Program, except for the pre-Holocene VEI 7/8 examples.-->

{| class="wikitable"

! rowspan="2" | VEI

! rowspan="2" | Ejecta<br> volume<br>(bulk)

! style="width: 350px;"| Classification

! style="width: 100px;"| Description

! style="width: 100px;"| Plume

! style="width: 150px;"| Periodicity

! style="width: 100px;"| Tropospheric<br>injection

! style="width: 100px;"| Stratospheric<br>injection

|-

! colspan="7" style="font-size:90%; color:#888;" | Examples

|-

! rowspan="2" style="background-color: white;" | 0

| rowspan="2" | <&nbsp;10<sup>4</sup> m<sup>3</sup> || Hawaiian || Effusive || < 100 m || constant || negligible || none

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Kīlauea, Mawson Peak (current), Fagradalsfjall (2021-2023), Mauna Loa (1975, 1984, 2022), Piton de la Fournaise (current)

|-

! rowspan="2" style="background-color: #FFC;" | <span style="color: black;">1</span>

| rowspan="2" | >&nbsp;10<sup>4</sup> m<sup>3</sup> || Hawaiian / Strombolian || Gentle || || daily || minor || none

|-

| colspan="7" style="font-size:90%; color:#888; background:white;" | Yakedake (1995), Dieng Volcanic Complex (1964, 1979, 2017), Havre Seamount (2012), Sundhnúkur (2023-2024)

|-

! rowspan="2" style="background-color: #FF3;" | <span style="color: black;">2</span>

| rowspan="2" | >&nbsp;10<sup>6</sup> m<sup>3</sup> || Strombolian / Vulcanian || Explosive || 1–5&nbsp;km || 2 weeks || moderate || none

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Mount Etna, Stromboli (since 1934), Unzen (1792), Ritter Island (1888), White Island (2019), Marapi (2023)

|-

! rowspan="2" style="background-color: #FC0;" | <span style="color: black;">3</span>

| rowspan="2" | >&nbsp;10<sup>7</sup> m<sup>3</sup> || Strombolian / Vulcanian / Peléan / Sub-Plinian || Severe || 3–15&nbsp;km || 3 months || substantial || possible

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Surtsey (1963-1967), Nevado del Ruiz (1985), Redoubt (1989-1990), Ontake (2014), Kanlaon (2024)

|-

! rowspan="2" style="background-color: #F90;" | <span style="color: black;">4</span>

| rowspan="2" | >&nbsp;0.1&nbsp;km<sup>3</sup> || Peléan / Plinian / Sub-Plinian|| Catastrophic || > 10&nbsp;km || 18 months || substantial || definite

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Bandai (1888), Pelée (1902), Lamington (1951), Eyjafjallajökull (2010), Merapi (2010), Semeru (2021)

|-

! rowspan="2" style="background-color: #F60;" | <span style="color: black;">5</span>

| rowspan="2" | >&nbsp;1&nbsp;km<sup>3</sup> || Peléan / Plinian || Cataclysmic || > 20&nbsp;km || 12 years || substantial || significant

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Vesuvius (79), Fuji (1707), Tarawera (1886), St. Helens (1980), Puyehue (2011)

|-

! rowspan="2" style="background-color: #F00;" | <span style="color: white;">6</span>

| rowspan="2" | >&nbsp;10&nbsp;km<sup>3</sup> || Plinian / Ultra-Plinian|| Colossal || > 30&nbsp;km || 50–100 years || substantial || substantial

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Lake Ilopango (450), Paektu (946), Huaynaputina (1600), Krakatoa (1883), Santa Maria (1902), Novarupta (1912), Pinatubo (1991), Hunga Tonga–Hunga Haʻapai (2022)

|-

! rowspan="2" style="background-color: #900;" | <span style="color: white;">7</span>

| rowspan="2" | >&nbsp;100&nbsp;km<sup>3</sup> || Ultra-Plinian || Super-colossal || > 40&nbsp;km || 500–1,000 years || substantial || substantial

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | Campi Flegrei (37 kyr), Crater Lake (6000 BC ~ 4000 BC), Kuril Lake (6400 BC), Kikai (4300 BC), Taal Caldera (~4000 BC), Cerro Blanco (2300 BC), Santorini (1600 BC), Taupo (232), Samalas (1257), Tambora (1815)

|-

! rowspan="2" style="background-color: black;" | <span style="color: white;">8</span>

| rowspan="2" | >&nbsp;1,000&nbsp;km<sup>3</sup> || Ultra-Plinian || Mega-colossal || > 50&nbsp;km || > 50,000 years || vast || vast

|-

| colspan="7" style="font-size:90%; color:#888; max-width:1px; background:white;" | 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, 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.

There have been at least 10 eruptions of VEI-7 in the last 11,700 years. There are also 58 Plinian eruptions, and 13 caldera-forming eruptions, of large, but unknown magnitudes. By 2010, the Global Volcanism Program of the Smithsonian Institution had cataloged the assignment of a VEI for 7,742 volcanic eruptions that occurred during the Holocene (the last 11,700 years) which account for about 75% of the total known eruptions during the Holocene. Of these 7,742 eruptions, about 49% have a VEI of 2 or lower, and 90% have a VEI of 3 or lower.

Limitations

Under the VEI, ash, lava, lava bombs, and ignimbrite are all treated alike. Density and vesicularity (gas bubbling) of the volcanic products in question is not taken into account. In contrast, the DRE (dense-rock equivalent) is sometimes calculated to give the actual amount of magma erupted. Another weakness of the VEI is that it does not take into account the power output of an eruption, which makes the VEI extremely difficult to determine with prehistoric or unobserved eruptions.

Although VEI is quite suitable for classifying the explosive magnitude of eruptions, the index is not as significant as sulfur dioxide emissions in quantifying their atmospheric and climatic impact.

Lists of notable eruptions

  • Timeline of volcanism on Earth (mostly VEI-6, within 2 kya)
  • List of volcanic eruptions 1500–2000
  • List of volcanic eruptions in the 21st century
  • List of volcanic eruptions by death toll
  • List of large Holocene volcanic eruptions (VEI-5–7)
  • List of large volcanic eruptions (VEI-5–8, within 450+ Mya)
  • List of largest volcanic eruptions (VEI-7–8, mostly within 500 Mya)

See also

  • Lists of volcanoes
  • List of natural disasters by death toll

References

  • 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