The physical volcanology of the 1600 eruption of Huaynaputina, southern Peru

@article{Adams2001ThePV,
  title={The physical volcanology of the 1600 eruption of Huaynaputina, southern Peru},
  author={Nancy K. Adams and Shanaka L. de Silva and Stephen Self and Guido Salas and Steven Schubring and Jason L. Permenter and Kendra Alice Arbesman},
  journal={Bulletin of Volcanology},
  year={2001},
  volume={62},
  pages={493-518}
}
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 during the period 19 February to 6 March 1600. The main eruptive vents are located at 4200 m within an erosion-modified amphitheater of a significantly older stratovolcano. The eruption proceeded in three stages. Stage I was an ~20-h sustained plinian eruption on 19–20 February that produced an… 
The historical (218 ± 14 aBP) explosive eruption of Tutupaca volcano (Southern Peru)
The little known Tutupaca volcano (17° 01′ S, 70° 21′ W), located at the southern end of the Peruvian arc, is a dacitic dome complex that experienced a large explosive eruption during historical
Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815
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
...
...