Fig. 10From: Relating gas ascent to eruption triggering for the April 27, 2016, White Island (Whakaari), New Zealand eruption sequenceCO2 travel-times plotted as functions of permeability. The gas pulse originates at 800 m depth which marks the VLP source location which is inferred to be the boundary between the magma supply zone and the hydrothermal systemBack to article page