Logo link to homepage

Report on Karangetang (Indonesia) — 15 February-21 February 2023


Karangetang

Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 15 February-21 February 2023
Managing Editor: Sally Sennert.

Please cite this report as:

Global Volcanism Program, 2023. Report on Karangetang (Indonesia) (Sennert, S, ed.). Weekly Volcanic Activity Report, 15 February-21 February 2023. Smithsonian Institution and US Geological Survey.

Weekly Report (15 February-21 February 2023)

Karangetang

Indonesia

2.781°N, 125.407°E; summit elev. 1797 m

All times are local (unless otherwise noted)


According to PVMBG the eruption at Karangetang’s Main Crater (S crater) continued during 14-21 February. Multiple nighttime webcam images posted with daily reports showed three main incandescent lava flows of different lengths descending the S, SW, and W flanks; a webcam image from 2156 on 17 February possibly showed incandescent material descending the SE flank. Incandescent rocks dotted the upper flanks, possibly from ejected or collapsed material from the crater; the incandescence was often most intense at the summit. Based on analyses of satellite imagery and weather models, the Darwin VAAC reported that during 16-20 February daily ash plume rose to an altitude of 2.1-3 km (7,000-10,000 ft) a.s.l. and drifted NNE, E, and SE. BNPB reported that as of 16 February there were as many as 77 people that had been displaced by the eruption and were in the East Siau Museum which was designated as a temporary evacuation shelter. The Alert Level remained at 3 (on a scale of 1-4) and the public were advised to stay 2.5 km away from Main Crater with an extension to 3.5 km on the S and SE flanks.

Geological Summary. Karangetang (Api Siau) volcano lies at the northern end of the island of Siau, about 125 km NNE of the NE-most point of Sulawesi. The stratovolcano contains five summit craters along a N-S line. It is one of Indonesia's most active volcanoes, with more than 40 eruptions recorded since 1675 and many additional small eruptions that were not documented (Neumann van Padang, 1951). Twentieth-century eruptions have included frequent explosive activity sometimes accompanied by pyroclastic flows and lahars. Lava dome growth has occurred in the summit craters; collapse of lava flow fronts have produced pyroclastic flows.

Sources: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM), Badan Nacional Penanggulangan Bencana (BNPB), Darwin Volcanic Ash Advisory Centre (VAAC)