Phreatic eruptions at Whakaari volcano are influenced by subsurface pressurisation magnitudes and timescales, which are significantly influenced by hydrothermal mineralisation and magmatic gas input rates, according to 3-dimensional numerical modelling of volcanic hydrothermal systems.

Abstract. Heterogeneous structures and diverse volcanic, hydrothermal, and geomorphological processes hinder characterisation of the mechanical properties of volcanic rock masses. Laboratory experimen...

Abstract. Heterogeneous structures and diverse volcanic, hydrothermal, and geomorphological processes hinder the characterisation of the mechanical properties of volcanic rock masses. Laboratory exper...