Get our newsletter!
Check out our volcano tours on!
Volcanoes & Earthquakes - new app for Android
Volcanoes & Earthquakes - app for iPhone & iPad

Guaranteed tours:
2-18 Nov 2019: Volcanoes and Spices - N-Sulawesi + Halmahera (Indonesia)
17-21 Nov 2019: Krakatau Volcano Special - Krakatau volcano (Indonesia)
17-30 Nov 2019: Desert, salt and volcanoes - Danakil desert (Ethiopia)
9-17 May 2020: From Stromboli to Etna - Eolian Islands + Etna volcano (Italy)
11-29 Aug 2020: Kamchatka - Land of Colors - Kamchatka (Russia)
: spaces available / : guaranteed / : few spaces left / : booked out
Random pictures
Sinabung volcano
Stratovolcano 2460 m (8,071 ft)
Sumatra, Indonesia, 3.17°N / 98.39°E
Current status: restless (2 out of 5)
Sinabung webcams / live data | Reports
Sinabung volcano videos
Sinabung volcano books | Tours
| Places to stay
Sinabung volcano eruptions:
2013-ongoing, 2010
Typical eruption style:
Last earthquakes nearby
Latest satellite images

Sentinel hub | Landsat 8

Sinabung volcano (Sumatra): eruption news and activity updates

Sinabung volcano (Sumatra) - continuing lava effusion forms large lava lobe and pyroclastic flows

Thursday Jan 30, 2014 11:23 AM | BY: T

The lava flow from Sinabung has reached the base of the mountain
The lava flow from Sinabung has reached the base of the mountain
Pyroclastic flow this morning
Pyroclastic flow this morning
Zoom onto the upper part of the lava lobe originating at the dome
Zoom onto the upper part of the lava lobe originating at the dome
The new lava lobe descending the SE flank of Sinabung
The new lava lobe descending the SE flank of Sinabung
Ash landscape
Ash landscape
The unstable front of the lava lobe (26 Jan)
The unstable front of the lava lobe (26 Jan)
Lava effusion continues at the volcano and pyroclastic flows occurred this morning. During the past 7-10 days, the growing lava dome has effused an impressive thick extrusion lobe that managed to form a massive, approx. 800 m long coherent lava flow reaching the base of the mountain.
The sticky lava flow followed and almost completely filled the deep ravine on the SE side of the volcano which before channeled the rockfalls and pyroclastic flows.
However, this steep, blocky lava flow is highly unstable. Collapsing material from the flow still generates frequent rock avalanches and sometimes pyroclastic flows, although the latter ones have been significantly smaller in size than those during late Dec until mid January.

This suggests that the arriving magma is already more degassed and less prone to fragmentation, i.e. explosive activity and pyroclastic flows.
Another significant difference is the changed geometry of the crater and the lava dome. Until 10-11 January, the dome had been confined inside a circular crater with steep outer slopes, which forced all overspilling lava to break apart from the main mass to disintegrate (and partially explode due to gas contained in the lava) into the frequent pyroclastic flows (as opposed to a coherent lobe as now).
This changed probably during the night of 10-11 January, when a major collapse or a sequence of collapse events occurred. It resulted in the formation of the large V-shaped crater breach and the removal of much of the lava dome. A deep canyon starting at the breached crater channeled from then on all rockfalls and pyroclastic flows. The formation of this lower-lying and increasingly eroded "outlet" for the sticky lava also made for an overall less steep path.
Blog Culture Volcan has posted a beautiful description with comparative photos illustrating this evolution of the crater geometry during January.
In combination with a currently less gas-rich (and less prone to explode) magma, the changed geometry allowed the viscous lava from the dome to remain coherent and flow out as a lobe. For the time being, this means that the eruption is in a more stable phase and less dangerous (as pyroclastic flows although they still occurring are less likely).

It is impossible to predict how the eruption will continue. It could come to an gradual end with slowly decreasing lava effusion, but it could also enter a new phase of more explosive activity, if new batches of fresh, gas-rich magma arrive at the summit. As it continues to grow, the risk of a major collapse of the dome and even the lava lobe remains as well.

The situation of the evacuees (about 30,000 according to official numbers) remains difficult. The Indonesian president visited the site last week and promised help and announced that the area in a 3 km radius around the volcano should remain as a permanently depopulated area.
Previous news
Pyroclastic flow from Sinabung yesterday (photo: Aris)
Tuesday, Jan 28, 2014
The volcano's lava dome continues to grow. Following a quieter interval, a new series of pyroclastic flows occurred yesterday. ... [more]
Steam / ash plume rising fro Sinabung this morning
Friday, Jan 24, 2014
A tall steam and ash plume rises from the summit crater, reaching altitudes of up to estimated 4-5 km at times. ... [more]
Wednesday, Jan 22, 2014
Activity at the volcano continues at reduced rate. The lava dome continues to be active with intense degassing and ash venting, and has produced a series of sporadic smaller pyroclastic flows over the past days. [more]

Monday, Jan 20, 2014
Aris Yanto (NdesoAdventures) who is currently on location sent us some impressions from the activity at Sinabung volcanotaken during 16-20 Jan 2014. ... [more]
Visual and seismic data ("Letusan"=explosions, "Guguran"= pyroclastic flows) for the past weeks (VSI)
Sunday, Jan 19, 2014
Activity at the volcano has been a bit lower during the past days, especially when compared to the first half of the past week. It is certainly too early to say whether this is a sign of a possible approaching end of the of the eruption or just a temporary or perhapy only apparent decrease. ... [more]

More on VolcanoDiscovery:

Copyrights: VolcanoDiscovery and other sources as noted.
Use of material: Most texts and images, in particular photographs, on this website are protected by copyright. Further reproduction and use of without authorization is usually not consented. If you are not sure or need licensing rights for photographs, for example for publications and commercial use, please contact us.