Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815

@article{Oppenheimer2003ClimaticEA,
  title={Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815},
  author={Clive Oppenheimer},
  journal={Progress in Physical Geography},
  year={2003},
  volume={27},
  pages={230 - 259}
}
The 1815 eruption of Tambora volcano (Sumbawa island, Indonesia) expelled around 140 gt of magma (equivalent to ≈50 km3 of dense rock), making it the largest known historic eruption. More than 95% by mass of the ejecta was erupted as pyroclastic flows, but 40% by mass of the material in these flows ended up as ash fallout from the ‘phoenix’ clouds that lofted above the flows during their emplacement. Although they made only a minor contribution to the total magnitude of the eruption, the short… Expand
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References

SHOWING 1-10 OF 59 REFERENCES
Volcanological study of the great Tambora eruption of 1815
The 1815 eruption of Tambora is one of the largest explosive volcanic events of the past 10 000 yr. By a conservative estimate, 175 km3 of nepheline-normative trachyandesitic pyroclastic materialExpand
The physical volcanology of the 1600 eruption of Huaynaputina, southern Peru
Abstract. Volcán Huaynaputina is a group of four vents located at 16°36'S, 70°51'W in southern Peru that produced one of the largest eruptions of historical times when ~11 km3 of magma was eruptedExpand
Global influence of the AD 1600 eruption of Huaynaputina, Peru
It has long been estabished that gas and fine ash from large equatorial explosive eruptions can spread globally, and that the sulphuric acid that is consequently produced in the stratosphere canExpand
Climatic and Demographic Consequences of the Massive Volcanic Eruption of 1258
Somewhere in the tropics, a volcanoexploded violently during the year 1258, producing amassive stratospheric aerosol veil that eventuallyblanketed the globe. Arctic and Antarctic ice coressuggestExpand
Dimensions and dynamics of co-ignimbrite eruption columns
VERY powerful volcanic eruptions cannot always form classical Plinian eruption columns1–4. Instead, collapsing fountains may develop above the vent and shed pyroclastic flows which spread laterallyExpand
Ice core and palaeoclimatic evidence for the timing and nature of the great mid-13th century volcanic eruption
Ice cores from both the Arctic and Antarctic record a massive volcanic eruption in around AD 1258. The inter-hemispheric transport of ash and sulphate aerosol suggests a low-latitude explosiveExpand
Ice core evidence for an explosive tropical volcanic eruption 6 years preceding Tambora
High-resolution analyses of ice cores from Antarctica and Greenland reveal an explosive volcanic eruption in the tropics in A.D. 1809 which is not reflected in the historical record. A comparison inExpand
Volatile emission during the eruption of Baitoushan Volcano (China/North Korea) ca. 969 AD
3 [magma volume (DRE): 24 ± 5 km3]. The main phase (ca. 95 vol.%) is represented by comenditic tephra deposited dominantly as widespread fallout blankets and proximal ignimbrites. The eruption columnExpand
A 110,000-yr record of explosive volcanism from the GISP2 (Greenland) ice core
The time series of volcanically produced sulfate from the GISP2 ice core is used to develop a continuous record of explosive volcanism over the past 110,000 yr. We identified ∼850 volcanic signalsExpand
Kuwae (≈ 1425 A.D.): the forgotten caldera
In Vanuatu, Tongoa and Epi islands once formed part of a larger landmass, Kuwae, which was partly destroyed during a cataclysmic seismo-volcanic event that is recorded in local folklore. It led toExpand
...
1
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3
4
5
...