Environmental Geology

, Volume 30, Issue 1, pp 59–61

The global impact of the Minoan eruption of Santorini, Greece

  • D. M. Pyle
Research article

DOI: 10.1007/s002540050132

Cite this article as:
Pyle, D. Environmental Geology (1997) 30: 59. doi:10.1007/s002540050132

Abstract

 The Minoan eruption of Santorini was a large-magnitude natural event. However, in terms of scale it ranks smaller in erupted volume and eruptive intensity than the historical eruption of Tambora in 1815 AD, and smaller in sulphur emission and, by inference, climatic effects than both the Tambora and Mt. Pinatubo, 1991, eruptions. Eruption statistics for the past 2000 years indicate that Minoan-size eruptions typically occur at a rate of several per thousand years. Eruptions resulting in a Minoan-scale injection of sulphur to the stratosphere occur far more frequently – at a rate of one or two per century. Inferences of massive sociological, religious and political impacts from such eruptions owe more to mythology than reality.

Key words Explosive volcanic eruptionsVolcano-climate interactionTheraGreece

Copyright information

© Springer-Verlag Berlin Heidelberg 1997

Authors and Affiliations

  • D. M. Pyle
    • 1
  1. 1.Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UKGB