Fig. 7.From: Transition in eruption style during the 2011 eruption of Shinmoe-dake, in th Kirishima volcanic group: Implications from a steady conduit flow modelRepresentative strain rate profile (i) and the profile of the critical value (ii) (right-hand-side of Eq. (11)) versus pressure along the conduit. Discharge rate = 87 m3 /s, R c = 16 m, T = 980°C, n0 = 4.0 wt%, L = 6 km, ω = 3.8, E w = 0.Back to article page