The global impact of the Minoan eruption of Santorini, Greece

@article{Pyle1997TheGI,
  title={The global impact of the Minoan eruption of Santorini, Greece},
  author={David M. Pyle},
  journal={Environmental Geology},
  year={1997},
  volume={30},
  pages={59-61}
}
  • D. Pyle
  • Published 24 March 1997
  • Geology
  • Environmental Geology
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… 

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References

SHOWING 1-10 OF 23 REFERENCES
Lessons from a major eruption: Mt. Pinatubo, Philippines
Small phreatic explosions on April 2, 1991, ended more than 400 years of quiescence at Mount Pinatubo. A joint Philippine-United States team worked quickly to understand the unrest and the eruptive
Caldera Development During the Minoan Eruption, Thira, Cyclades, Greece
The well-known caldera of Thira (Santorini), Greece, was not formed during a single eruption but is composed of two overlapping calderas superimposed upon a complex volcanic field that developed
Worldwide environmental impacts from the eruption of Thera
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
Irish tree rings, Santorini and volcanic dust veils
There has recently been renewed interest in the dating of the violent eruption of the Aegean island of Santorini in the second millennium BC, both by its possible effects on tree-ring growth in the
The role of microphysical and chemical processes in prolonging the climate forcing of the Toba Eruption
The mega-eruption of Toba, Sumatra, occurred around 73 Ka ago, during the onset of a glaciation of the Late Quaternary. This coincidence combined with the unprecedented amount of sulphur released by
Explosive volcanism on Santorini, Greece
Santorini volcanic field has had 12 major (1–10 km 3 or more of magma), and numerous minor, explosive eruptions over the last ~ 200 ka. Deposits from these eruptions (Thera Pyroclastic Formation) are
ICE‐CORE ACIDITY PEAKS, RETARDED TREE GROWTH AND PUTATIVE ERUPTIONS
The timings of many historic volcanic eruptions coincide with sulphuric acid maxima in polar ice cores and transient cooling events. Similar effects are recorded in ancient ice cores and tree-ring
Historic eruptions of Tambora (1815), Krakatau (1883), and Agung (1963), their stratospheric aerosols, and climatic impact
Abstract Decreases in surface temperatures after the eruptions of Tambora (1815), Krakatau (1883), and Agung (1963) were of similar magnitude, even though the amount of material (dust and volatiles)
Plinian and co-ignimbrite tephra fall from the
A study of pyroclastic deposits from the 1815 Tambora eruption reveals two distinct phases of activity, i.e., four initial tephra falls followed by generation of pyroclastic flows and the production
Sulphur emissions to the stratosphere from explosive volcanic eruptions
Abstract Two methods were used to quantify the flux of volcanic sulphur (as the equivalent mass of SO2) to the stratosphere over different timescales during the Holocene. A combination of
...
1
2
3
...