Skip to main content
Log in

Worldwide environmental impacts from the eruption of Thera

  • Original Articles
  • Published:
Environmental Geology

Abstract

The eruptions of Thera (Santorini) between 1628 and 1450 BC constituted a natural catastrophe unparalleled in all of history. The last major eruption in 1450 BC destroyed the entire Minoan Fleet at Crete at a time when the Minoans dominated the Mediterranean world. In addition, there had to be massive loss of life from ejecta gases, volcanic ash, bombs, and flows. The collapse of a majestic mountain into a caldera 15 km in diameter caused a giant ocean wave, a tsunami, that at its source was estimated in excess of 46 m high. The tsunami destroyed ships as far away as Crete (105 km) and killed thousands of people along the shorelines in the eastern Mediterranean area. At distant points in Asia Minor and Africa, there was darkness from ash fallout, lightning, and destructive earthquakes. Earthquake waves emanating from the epicenter near the ancient volcano were felt as far away as the Norwegian countries. These disturbances caused great physical damage in the eastern Mediterranean and along the rift valley system from Turkey to the south into central Africa. They caused major damage and fires in north Africa from Sinai to Alexandria, Egypt. Volcanic ash spread upward as a pillar of fire and clouds into the atmosphere and blocked out the sun for many days. The ash reached the stratosphere and moved around the world where the associated gases and fine particulate matter impacted the atmosphere, soils, and waters. Ground-hugging, billowing gases moved along the water surface and destroyed all life downwind, probably killing those who attempted to flee from Thera. The deadly gases probably reached the shores of north Africa. Climatic changes were the aftermath of the eruption and the atmospheric plume was to eventually affect the bristlecone pine of California; the bog oaks of Ireland, England, and Germany, and the grain crops of China. Historical eruptions at Krakatau, Tambora, Vesuvius, and, more currently, eruptions at Nevado del Ruiz, Pinatubo, and Mount Saint Helens, have done massive environmental damage but none can compare with the sociological, religious, economic, agricultural, and political impacts from Thera (Santorini). Major natural catastrophes that have occurred over historical time illustrate the force of nature and the impact on civilizations. Some examples of these are rains that flooded the Euphrates Valley during the time of Noah, and floods, earthquakes, and hurricanes in recent years, such as earthquakes in California and Hurricane Hugo on the east coast of the United States.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References

  • Baillie MGL (1989) Irish tree-rings and an event in 1628 BC. In: Proceedings of the Third International Congress, Thera and the Aegean World, Santorini, Greece, 3–9 September, 1989. Santorini, Greece: The Thera Foundation, pp. 160–166.

    Google Scholar 

  • Boettcher A (Ed) (undated) Portrait of an island-Santorini. Aachen, Germany: P. Laufen KG. 72 pp

  • Davis EN (1990) A storm in Egypt during the reign of Ahmose. In: Proceedings of the Third International Congress, Thera and the Aegean World, Santorini, Greece, 3–9 September, 1989. Santorini, Greece: The Thera Foundation, pp 232–235

    Google Scholar 

  • Friedman GM (1992) Geology illuminates biblical events. Geotimes 37(3):18–20

    Google Scholar 

  • Galanopoulos AG (1963) How Moses crossed sea-quake and tidal wave provided a dry gap? San Francisco Examiner, San Francisco, California, Sunday, August 25, Sec. 1. p 17

  • Goedicke H (1986) The end of the Hyksos in Egypt. In: Lesko L. (Ed), Egyptological studies in honor of Richard A. Parker: Hannover: Verlag Heinz Heise pp 37–47

    Google Scholar 

  • Huntington E (1911) Palestine and its transformation. Boston: Houghton Mifflin. 443 pp

    Google Scholar 

  • Issar AS (1990) Water shall flow from the rock. Heidelberg: Springer-Verlag. 213 pp

    Google Scholar 

  • Marinatos S (1939) The volcanic destruction of Minoan Crete. Antiquity 13:425–439

    Google Scholar 

  • McClelland L and Simkin T (1986) Volcanic events reviewed. Geotimes 31(4):14–17

    Google Scholar 

  • McCoy FW and Haiken G (1990) Anatomy of an eruption, how a terrifying series of explosions reshaped the Minoan island of Thera. Archaeology, 43(3):42–49

    Google Scholar 

  • McCredie S (1994) When nightmare waves appear out of nowhere to smash the land. Smithsonian 24(12):28–38

    Google Scholar 

  • National Research Council (1989) Reducing disasters' toll. Washington, DC: National Academy Press. 40 pp

    Google Scholar 

  • Oeschger H and Eddy JA (Eds) (1989) Global changes of the pastreport no. 6: Report of meeting of the IGBP working group on techniques extracting environmental data from the past. University of Bern, Switzerland, pp 1–8

    Google Scholar 

  • Perevolotsky A and Finkelstein I (1985) The southern Sinai exodus route in ecological perspective. Biblical Archaeol Rev 9(4):27–41

    Google Scholar 

  • Pichler H and Friedrich WL (1972) Mechanism of the Minoan eruption of Santorini. Doumas (supra note 2 and 3), Vol II(19), 135 p

  • Puchelt H (undated) Geology. In: Boettcher A (Ed), Portrait of an Island-Santorini. Aachen, Germany: P. Laufen KG. pp 22–47

  • Pyles DM (1989) The application of tree-ring and ice-core studies to the dating of the Minoan eruption. In: Proceedings of the Third International Congress, Thera and the Aegean World, Santorini, Greece, 3–9 September 1989. Santorini, Greece: The Thera Foundation, pp 167–173

    Google Scholar 

  • Ressmeyer RH and Pasachoff JM (1992) The great eclipse. Natl Geogr, 181(5):30–42

    Google Scholar 

  • Shiklomanov IA (1993) Climate of uncertainty (climatic changes and global water supply). Paris: UNESCO, pp 29–32

    Google Scholar 

  • Stiebing WH Jr (1985) Should the exodus and the Israelite settlement be redated? Biblical Archaeol Rev 9(4):58–69

    Google Scholar 

  • Stiebing WH Jr (1987) Greenland ice study puts Thera destruction at 1645 BC. The Tuscaloosa News, Tuscaloosa, Alabama, August 7. p 19

    Google Scholar 

  • United States Geological Survey (1982) The Mediterranean seafloor (map). Washington, DC

  • Wilford JN (1985) New evidence could link volcano to biblical exodus. New York Times News Service, New York, December 24

    Google Scholar 

  • Yokoyama I (1980) The tsunami caused by the prehistoric eruption of Thera. In: roceedings of the international symposium on engineering geology and protection of ancient works, monuments and historical sites, Athens, Greece. London: International Association on Engineering Geology.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

LaMoreaux, P.E. Worldwide environmental impacts from the eruption of Thera. Geo 26, 172–181 (1995). https://doi.org/10.1007/BF00768739

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00768739

Key words

Navigation