Probability of a VEI 5+ volcanic eruption within 5 years is over 95%

It has been 24 years since the last VEI 5+ (Mount Pinatubo, 1991, VEI 6) occurred and the probability that a VEI 5+ volcanic eruption will occur within the next 5 years is now over 95%. There are around 10 – 14 VEI 5+ eruptions every hundred years and for the the last 300 years the time between eruptions has been as short as 1 year and as long as 23 years. The current gap could be the longest recorded in three centuries. There are, on average, 2 eruptions of intensity 6 every hundred years and so the probability that an eruption of VEI 6 could occur within 5 years is about 50% (current gap 24 years, average gap 50 years). That a supervolcanic eruption of VEI 7 or greater could occur within the next 5 years is less than 1%.

The next VEI 5+ volcanic eruption is overdue During the 19th century VEI eruptions of 5 or greater occurred every 11 years on average with the Krakatoa eruption being the greatest at VEI 6 in 1883. Through the 20th century, an eruption of intensity 5 or greater came at intervals varying from 1 year upto 23 years with an average interval of just under 7 years. The Novarupta (1912) and Mount Pinatubo (1991) eruptions were the two classified at VEI6. 

  • 1902 Santa Maria
  • 1907 Kudach
  • 1912 Novarupta
  • 1913 Colima
  • 1918 Katla
  • 1932 Cerro Azul
  • 1933 Kharimkotan
  • 1956 Bezymianny
  • 1963 Mount Agung
  • 1980 Mount St. Helens
  • 1982 El Chichón
  • 1991 Mount Pinatubo
  • 1991 Mount Hudson
vei eruption balls image

vei eruption balls image

So far in this century the 2010 Eyjafjallajökull eruption in Iceland “only” reached a VEI intensity of 4. The Puyehue-Cordón Caulle eruption in 2011 was judged – by some – to be of intensity 5 was really just a VEI 4. The 2012 Mt. Etna eruption was rated a 3+.

Classification of eruptions

Classification of eruptions

The impact of the next eruption has to be assessed in a short and a long-term perspective. Immediate loss of life and property is primarily a function of population in the area of the eruption and the time available for evacuation. Populations are higher now than ever in the past but warnings come earlier and possibilities for evacuation are better than ever before.  The population directly at risk from volcanoes in the year 2000 has been estimated at 500 million or more, The long-term impacts could be much more profound and independent of the location of the eruption. We are already into an ocean- current led global cooling cycle. We could well have another year or two without a summer after the next VEI 5+ eruption. The key will be the extent of the dust cloud, the altitude it reaches and for how long it persists. It will not be a Toba like cataclysm which affected the evolution of humans, but it may well be the impulse which drives the earth into an Ice Age. It could even be the start of a 1000 years of transition back into a Glacial Age since the current Interglacial has been around for some 15,000 years.

Extreme Geohazards: Reducing the Disaster Risk and Increasing Resilience VEI values have been determined for more than 5,000 eruptions in the Holocene…. None of these reached the maximum VEI of 8. Several of the most devastating eruptions during the last 2,000 years had VEI values lower than 6. For example, the VEI 5 eruption of Vesuvius in 79 AD destroyed Pompeii and Herculaneum. Since 1500, more than 20 eruptions of VEI 5 or more occurred, with only the Tambora eruption in 1815 reaching VEI 7. It is worth noting that the extremely disruptive eruption of Eyjafjallajökull only reached an estimated VEI of between 3 and 4. …… The size and magnitude of …. the eruption, is only loosely related to the resulting damage. For example, mudflows triggered by the VEI 3 eruption of Nevado del Ruiz (Colombia) in 1985 caused one of the worst volcanic disaster in the 20th century. …… of the nine greatest volcanic disasters in terms of casualties since 1500, only three (Tambora, Krakatau and Laki) qualify as ‘very large’ eruptions with a VEI of greater than 5. ….. during the past 36 Ma, 42 VEI 8 eruptions have been identified. The authors indicate that these eruptions are not evenly distributed in time but seem to cluster in two pulses over the past 36 Ma. Periods with as many as 22 events/Ma and down to 1.4 event/Ma have been identified. More recent examples are the eruptions of Taupo (around 24,000 BC), Toba (around 74,000 BC), and Yellowstone (around 640,000 BC), for which the impacts have been studied in detail. More recent large eruptions with a VEI of 5, 6 or 7 include Thera (≈1630 BC), Vesuvius (79 AD), Laki (1783), Tambora (1815), Krakatau (1883), Novarupta (1912) and Pinatubo (1991). Each of these eruptions (except Novarupta, due to the remoteness of the area) generated immediate loss of life and structures at local distances (through the generation of pyroclastic flows, ash and gas emissions, tsunamis) as well as long-term losses at regional and global distances. These eruptions impacted the climate for long periods by injecting ash in the stratosphere at high altitudes (Tambora’s ash column height reached 43 km) and triggering temperature changes which heavily impacted the harvest and led to famine and epidemics in several areas of the planet: the year 1816, following Tambora’s eruption, is recalled as ‘the year without summer’, and generated abnormal temperatures in China, Europe and North America. 

The hypotheses about man made global warming are neither predictable or measurable and are just fancies. But volcanic eruptions are neither fanciful nor amenable to prediction. They will occur and we have no means of preventing them. Within 5 years it is close to a certainty (> 95%) that a VEI 5+ volcanic eruption will occur. With global mobilisation loss of life can be minimised but the effects of the eruption on climate will just have to be endured.


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