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 Information about VEI
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The Volcanic Explosivity Index (VEI) was devised by Chris Newhall of the U.S. Geological Survey and Steve Self at the University of Hawaii in 1982 to provide a relative measure of the explosiveness of volcanic eruptions.

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 volcanoes in history given magnitude 8. A value of 0 is given for non-explosive eruptions (less than 104 cubic metres of tephra ejected) with 8 representing a mega-colossal explosive eruption that can eject 1012 cubic metres of tephra and have a cloud column height of over 25 km. Each interval on the scale represents a tenfold increase in observed eruption criteria.


VEI and ejecta volume correlation © USGS

Note that ash, volcanic bombs, and ignimbrite are all treated alike - this is due to taking into account the vesicularity (gas bubbling) of the volcanic products in question and the DRE (Dense-Rock Equivalent) is calculated to give the actual amount of magma erupted. One weakness of the VEI is that it does not take into account the magnitude of power output of an eruption. This, of course, is extremely difficult to detect with prehistoric or unobserved eruptions.

Classification

VEI Classification Description Plume Ejecta volume Frequency Occurrences *
0 Hawaiian Eruption non-explosive < 100 m < 10,000 m³ daily many
1 Strombolian Eruption gentle 100-1000 m > 10,000 m³ daily many
2 Vulcanian Eruption explosive 1-5 km > 1,000,000 m³ weekly 3477
3 Pelean Eruption severe 3-15 km > 10,000,000 m³ yearly 868
4 Plinian cataclysmic 10-25 km > 0.1 km³ ≥ 10 yrs 278
5 Plinian Eruption paroxysmal > 25 km > 1 km³ ≥ 50 yrs 84
6 Ultra-Plinian colossal > 25 km > 10 km³ ≥ 100 yrs 39
7 Ultra-Plinian super-colossal > 25 km > 100 km³ ≥ 1000 yrs 4
8 Ultra-Plinian mega-colossal > 25 km > 1,000 km³ ≥ 10,000 yrs none

*) Count of eruptions in the last 10,000 years based on 1994 figures maintained by the Global Volcanism Program of the Smithsonian Institution.

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