Fig. 6.From: The outline of the 2011 eruption at Shinmoe-dake (Kirishima), JapanTime sequence of subplinian events and height of the eruption column. The height changes estimated with Doppler radars and camera (Shimbori and Fukui, 2012) are shown in gray color and dashed line, respectively. The latter provides the minimum height. Layers of deposits corresponding to individual eruptive events are shown in the top.Back to article page