Report on Sinabung (Indonesia) — 28 December-3 January 2017
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
28 December-3 January 2017
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2016. Report on Sinabung (Indonesia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 28 December-3 January 2017. Smithsonian Institution and US Geological Survey.
3.17°N, 98.392°E; summit elev. 2460 m
All times are local (unless otherwise noted)
Based on PVMBG observations, webcam views, satellite images, and wind data the Darwin VAAC reported that during 28 December 2016-1 January 2017 ash plumes from Sinabung rose 3-5.6 km (10,000-18,000 ft) a.s.l. and sometimes drifted SW. A thermal anomaly was detected in satellite images on 30 December.
Geological Summary. Gunung Sinabung is a Pleistocene-to-Holocene stratovolcano with many lava flows on its flanks. The migration of summit vents along a N-S line gives the summit crater complex an elongated form. The youngest crater of this conical andesitic-to-dacitic edifice is at the southern end of the four overlapping summit craters. The youngest deposit is a SE-flank pyroclastic flow 14C dated by Hendrasto et al. (2012) at 740-880 CE. An unconfirmed eruption was noted in 1881, and solfataric activity was seen at the summit and upper flanks in 1912. No confirmed historical eruptions were recorded prior to explosive eruptions during August-September 2010 that produced ash plumes to 5 km above the summit.