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Report on Gamalama (Indonesia) — 3 January-9 January 2024


Gamalama

Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 3 January-9 January 2024
Managing Editor: Sally Sennert.

Please cite this report as:

Global Volcanism Program, 2024. Report on Gamalama (Indonesia) (Sennert, S, ed.). Weekly Volcanic Activity Report, 3 January-9 January 2024. Smithsonian Institution and US Geological Survey.

Weekly Report (3 January-9 January 2024)

Gamalama

Indonesia

0.81°N, 127.3322°E; summit elev. 1714 m

All times are local (unless otherwise noted)


Although there was no eruptive activity reported at Gamalama, in a 4 January press release PVMBG noted that the number of daily deep volcanic earthquakes had significantly increased. The seismic network recorded a total of 45 deep volcanic earthquakes during 0000-0600 on 4 January; an average of 2-3 events per day had been recorded since January 2023. Diffuse white plumes only rose as high as 120 m above the summit during the previous month whereas typically they can rise as high as 300 m. PVMBG noted that the most likely hazard would be a phreatic event that could ejected material within the 1.5-km radius, though ash may be carried farther by wind. The Alert Level remained at 2 (on a scale of 1-4); visitors and residents were warned not to approach the crater within a 1.5-km radius.

Geological Summary. Gamalama is a near-conical stratovolcano that comprises the entire island of Ternate off the western coast of Halmahera, and is one of Indonesia's most active volcanoes. The island was a major regional center in the Portuguese and Dutch spice trade for several centuries, which contributed to the extensive documentation of activity. Three cones, progressively younger to the north, form the summit. Several maars and vents define a rift zone, parallel to the Halmahera island arc, that cuts the volcano; the S-flank Ngade maar formed after about 14,500–13,000 cal. BP (Faral et al., 2022). Eruptions, recorded frequently since the 16th century, typically originated from the summit craters, although flank eruptions have occurred in 1763, 1770, 1775, and 1962-63.

Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)