Petrology

1989 Edition

Explosive volcaniceruptions—classification

  • George P. L. Walker
Reference work entry
DOI: https://doi.org/10.1007/0-387-30845-8_67

Most volcanic eruptions are to some extent explosive, and the explosivity index, which is the percentage of pyroclastic material (i.e., volcanic material fragmented and ejected from the vent by volcanic explosions) in the total erupted products is often 100%. The volcanic explosivity index is an informal 0–8 scale of increasing explosivity based on erupted volume, plume height, duration of climactic phase, etc., intended as a useful measure of the likely impact of the eruption on man.

There are several different measures of eruption size: (1) magnitude—the total quantity of pyroclastic products (taken as the equivalent volume of dense rock or magma without voids), for which Tsuya's scale (magnitude 9— ≫100 km3, 8—10 to 100 km3, 7—1 to 10 km3, etc.) is a convenient measure, (2) intensity—the discharge rate of magma plus rock from the vent, and (3) violence—the extent to which dispersal is determined by the translational kinetic energy of the pyroclastic system.

The jet emitted from the...

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Bibliography

  1. Aramaki, S. and M. Yamasaki, 1963, Pyroclastic flows in Japan, Bull. Volcanol. 26, 89–99.Google Scholar
  2. Escher, B. G., 1933, On a classification of central eruptions according to gas pressure of the magma and viscosity of the lavas, Liedse Geol. Meded. 6, 45–49.Google Scholar
  3. Hay, R. L., 1959, Formation of the crystal-rich glowing avalanche deposit of St. Vincent, B.W.I., J. Geol. 67, 540–562.CrossRefGoogle Scholar
  4. Moore, J. G., 1967, Base surge in recent volcanic eruptions, Bull. Volcanol. 30, 337–363.Google Scholar
  5. Newhall, C. G. and S. Self, 1982, The volcanic explosivity index (V.E.I.): an estimate of explosion magnitude from historical volcanism, J. Geophys. Res. 87, 1231–1238.Google Scholar
  6. Pyle, D. M., 1989, The thickness, volume and grainsize of tephra fall deposits, Bull. Volcanol. 51, 1–15.CrossRefGoogle Scholar
  7. Self, S. and R. S. J. Sparks, 1978, Characteristics of widespread pyroclastic deposits formed by the interaction of silicic magma and water, Bull. Volcanol. 41, 196–212.Google Scholar
  8. Smith, R. L., 1960, Ashflows, Bull. Geol. Soc. Am. 71, 795–841.Google Scholar
  9. Sparks, R. S. j., L. Wilson, and G. Hulme, 1978, Theoretical modeling of the generation, movement, and emplacement of pyroclastic flows by column collapse, J. Geophys. Res. 83, 1727–1739.CrossRefGoogle Scholar
  10. Sparks, R. S. J. and J. V. Wright, 1978, Welded air-fall tuffs, Spec. Pap. Geol. Soc. Am. 180, 155–166.Google Scholar
  11. Walker, G. P. L., 1973, Explosive volcanic eruptions—a new classification scheme, Geol. Rundsch. 62, 431–446.CrossRefGoogle Scholar
  12. Walker, G. P. L., 1980, Plinian eruptions and their products, Bull. Volcanol. 44, 223–240.Google Scholar
  13. Wilson, C. J. N. and G. P. L. Walker, 1981, Violence in pyroclastic flow eruptions, in S. Self and R. S. J. Sparks, eds., Tephra Studies. Dordrecht: Reidel, 441–448.Google Scholar
  14. Wilson, L., R. S. J. Sparks, T. C. Huang, and N. D. Watkins, 1978, The control of volcanic column heights by eruption energetics and dynamics, J. Geophys. Res. 83, 1829–1836.Google Scholar

Copyright information

© Van Nostrand Reinhold 1989

Authors and Affiliations

  • George P. L. Walker

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