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                                                        ERUPTION STYLES, SCALES, AND FREQUENCIES  155


                 Table 10.3 The Volcanic Explosivity Index (VEI) classification scheme.

                 Volcanic Explosivity  General eruption   Qualitative eruption   Erupted volume   Eruption column
                                                                            3
                 Index               description       description         (m )            height (km)
                 0                   Nonexplosive      “Gentle, effusive”  < 10 4          < 0.1
                  1                  Small             “Gentle, effusive”   10 6           0.1–1
                 2                   Moderate          “Explosive”          10 7             1–5
                 3                   Moderate/large    “Explosive”          10 8             3–15
                 4                   Large             “Explosive”          10 9            10–25
                 5                   Very large        “Cataclysmic,        10 10          > 25
                  6                  Very large        paroxysmal,          10 11          up
                 7                   Very large        or                   10 12          to
                 8                   Very large        colossal”           > 10 12           ∼55



                 Table 10.4 The magnitude, intensity and Volcanic Explosivity Index (VEI) of a number of historical eruptions: M is the total
                                                                                              e
                 erupted mass and M the peak mass flux.
                               f
                                                                   −1
                 Eruption                Erupted     M (kg)   M (kg s )  Column   VEI  Magnitude  Intensity
                                                      e         f
                                                 3
                                         volume (km )                   height (km)
                 Etna (Italy) 1991–1993    0.25       5 × 10 11  6 × 10 4  ∼1     2    4.7       7.8
                  Pinatubo (Philippines) 1991  7.5   1.1 × 10 13  4 × 10 8  35    6    6         11.6
                 Mount St Helens (USA) 1980  1.2     1.3 × 10 12  2 × 10 7  19    5    4.8      10.3
                 Soufriere (St Vincent) 1979  0.05       10 11  3 × 10 7  18      3    4         10.5
                 Kilauea (USA) 1959        0.03      6.6 × 10 10  1.5 × 10 5  > 0.6  2  3.8      8.2
                  Bezymianny (Russia) 1956  ∼2           10 12  2.2 × 10 8  36    5    5.3      11.3
                 Mauna Loa (USA) 1950      0.39          10 12  7 × 10 6  ?       0    5         9.8
                 Novarupta (Alaska) 1912  15          3 × 10 13  1 × 10 8  25     6    6.5      11.0
                 Santa Maria (Guatemala) 1902  12     2 × 10 13  1.7 × 10 8  34   6    6.3      11.2
                 Tarawera (New Zealand) 1886  2       2 × 10 12  2.2 × 10 8  34   5    5.3      11.3
                 Krakatau (Indonesia) 1883  > 10      3 × 10 13  ∼5 × 10 7  25    6    6.5      10.7
                 Askja (Iceland) 1875      0.17         ∼10 11  8 × 10 7  26      4    4.0      10.9
                 Tambora (Indonesia) 1815  > 50       2 × 10 14  2.8 × 10 8  43   7    7.3      11.4
                 Laki (Iceland) 1783      15          3 × 10 13  2.4 × 10 7  12   4    6.5      10.4
                 Taupo (New Zealand) ∼ AD 180  35     8 × 10 13  1.1 × 10 9  51   6+   6.9       12.0
                 Vesuvius (Italy) AD 79    6          6 × 10 12  1.5 × 10 8  32   6    5.8      11.2

                 Data taken from Richter, D.H., Eaton, J.P., Murata, K.J., Ault, W.U. and Krivoy, H.L. (1970) Chronological narrative of the
                 1959–60 eruption of Kilauea Volcano, Hawai’I. U.S. Geol. Surv. Prof. Pap., 537-E, 73 pp.; Sparks, R.S.J., Wilson, L. and
                 Sigurdsson, H. (1981) The pyroclastic deposits of the 1875 eruption of Askja, Iceland. Philos. Trans. Roy. Soc. London Ser. A,
                 299, 241–273; Wadge, G. (1981) The variation of magma discharge during basaltic eruptions. J. Volcanol. Geotherm. Res., 11,
                  139–168; Newhall & Self (1982); Sparks, R.S.J. and Wilson, L. (1982) Explosive volcanic eruptions – V. Observations of plume
                  dynamics during the 1979 Soufriere eruption, St Vincent. Geophys. J. Roy. Astron. Soc., 69, 551–570; Walker, G.P.L., Self, S.
                 and Wilson, L. (1984) Tarawera 1886, New Zealand – a basaltic plinian fissure eruption. J. Volcanol. Geotherm. Res., 21,
                 61–78; Cas, R.A.F. and Wright, J.V. (1987) Volcanic Successions – Modern and Ancient. Chapman and Hall, London, 528 pp.;
                 Wilson, L. and Walker, G.P.L. (1987) Explosive volcanic eruptions – VI. Ejecta dispersal in Plinian eruptions – the control of
                 eruption conditions and atmospheric properties. Geophys. J. Roy. Astron. Soc., 89, 657–679; Pyle, D.M. (1989) The thickness,
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                 World. Geoscience Press, 349 pp.; Parfitt, E.A. (1998) A study of clast size distribution, ash deposition and fragmentation in a
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