Fig. 6.From: Transition in eruption style during the 2011 eruption of Shinmoe-dake, in th Kirishima volcanic group: Implications from a steady conduit flow modelRelation between the magma chamber pressure and volumetric discharge rate in the most likely steady solution for the lava extrusion stage of the 2011 event. Point A corresponds to the initiation of lava effusion at which the discharge rate is 87 m3/s.Back to article page