Experimental studies have been performed to evaluate pre-explosive wat
er-melt mixes with respect to explosive volcanic molten-fuel-coolant i
nteraction (MFCI), i.e., phreatomagmatic explosion. Re-molten ultrabas
ic volcanic rock was used as a magma simulant. Measurement of the expl
osion intensity was used to determine optimal premixing conditions. A
well-defined optimal range was found for the hydrodynamic mixing energ
y (differential flow speed of 4.2 m/s), as well as for the water/melt
mass ratio (0.03 to 0.04) under experimental conditions. The mass flux
of water had a minor influence on the explosion intensity. Additional
ly, transparent mixing experiments with silicon oil and inked water we
re carried out. They indicate a direct dependence of the pre-explosive
water-melt interface area on the explosion intensity. The experimenta
l results show that the contact conditions of water and melt required
for explosive MFCI may easily be established in natural volcanic syste
ms. Thus, explosive MFCI is a probable mechanism of explosive volcanis
m.