Transition in eruption style during the 2011 eruption of Shinmoe-dake, in th Kirishima volcanic group: Implications from a steady conduit flow model

Earth, Planets and Space

Table 1. Parameters for Shinmoe-dake 2011 eruption.

Parameters	Value range	References
Lava discharge rate	70–87 m³/s	Kozono et al. (2013)
Magma Temperature	960–980°C	Suzuki et al. (2013)
Initial H₂O content	4 wt%	Suzuki et al. (2013)
Volume fraction of phenocrysts	30%	Suzuki et al. (2013)
Magma chamber depth	6.2 km	GSI (2012)