New insights into eruption source parameters of the 1600 CE Huaynaputina Plinian eruption, Peru

@article{Prival2019NewII,
  title={New insights into eruption source parameters of the 1600 CE Huaynaputina Plinian eruption, Peru},
  author={Jean-Marie Prival and Jean-Claude Thouret and Saida Japura and Lucia Gurioli and Costanza Bonadonna and Jersy Mari{\~n}o and K. Cueva},
  journal={Bulletin of Volcanology},
  year={2019},
  volume={82}
}
In the Central Andes, large Plinian eruptions (Volcanic Explosivity Index ≥ 5) occur at a relatively high frequency, i.e. average one every 2000 to 4000 years over the past 50,000 years in Peru. Such recurring explosive activity represents a significant challenge for regions typically hosting several million people (e.g. Southern Peru, Western Bolivia and Northern Chile). With VEI 6, the 1600 CE Huaynaputina eruption is considered the largest historical eruption in South America. We have re… 
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References

SHOWING 1-10 OF 67 REFERENCES
Largest explosive eruption in historical times in the Andes at Huaynaputina volcano, a.d. 1600, southern Peru
The largest explosive eruption (volcanic explosivity index of 6) in historical times in the Andes took place in a.d. 1600 at Huaynaputina volcano in southern Peru. According to chronicles, the
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 erupted
Global Impacts of the 1600 Eruption of Peru's Huaynaputina Volcano
The human impacts of the 1815 eruption of Tambora volcano in eastern Indonesia are well known. The sulfur injected into the stratosphere by that eruption produced a veil of sunlight-reflecting
Explosive volcanism (VEI 6) without caldera formation: insight from Huaynaputina volcano, southern Peru
Through examination of the vent region of Volcán Huaynaputina, Peru, we address why some major explosive eruptions do not produce an equivalent caldera at the eruption site. Here, in 1600, more than
Determination of the largest clast sizes of tephra deposits for the characterization of explosive eruptions: a study of the IAVCEI commission on tephra hazard modelling
The distribution of clasts deposited around a volcano during an explosive eruption typically contoured by isopleth maps provides important insights into the associated plume height, wind speed and
MeMoVolc report on classification and dynamics of volcanic explosive eruptions
Classifications of volcanic eruptions were first introduced in the early twentieth century mostly based on qualitative observations of eruptive activity, and over time, they have gradually been
Constraining explosive volcanism: subjective choices during estimates of eruption magnitude
When estimating the magnitude of explosive eruptions from their deposits, individuals make three sets of critical choices with respect to input data: the spacing of sampling sites, the selection of
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