The ash emissions are fueled by a cycle of lava dome growth and collapse. In this process, thick lava is extruded from the erupting vent near the volcano’s summit. As the dome grows the outside of the lava cools, forming a solid shell, while more lava oozes up from below. Eventually, the sides of the lava dome become too steep to be stabilized by the weak rock, and it collapses. The rock, often red-hot and riddled with gas-filled holes, disintegrates as it flows down the mountainside, creating a pyroclastic flow and ash cloud.
The following video shows a dome collapse and pyroclastic flow that occurred on Sinabung during January 2014.
References
- Financial Times (2014, January 23) Sinabung devastation highlights Indonesia volcano risk. Accessed January 29, 2014.
- Klemetti, Erik (2014, January 28) Eruption Update for January 28, 2014: Etna and Sinabung. Accessed January 29, 2014.
- Roscoe, Richard (2014, January) Sinabung Volcano (Gunung Sinabung). Accessed January 29, 2014.
NASA Earth Observatory image by Jesse Allen and Robert Simmon, using EO-1 ALI data from the NASA EO-1 team. Photograph & video ©2014, Richard Roscoe, Photovolcanica. Caption by Robert Simmon.
- Instrument:
- EO-1 - ALI