M 7.1; 155 km NW of Ternate, Indonesia; (15 Nov 2014) (32km from the earthquake)
M 7.5; 126 km WNW of Ternate, Indonesia; (21 Jan 2007) (63km from the earthquake)
M 7.1; 137 km WNW of Ternate, Indonesia; (24 Feb 2001) (43km from the earthquake)
Seismic Activity Near Ternate, Indonesia: A Review of Recent Major Events
Ternate, located in North Maluku province, Indonesia, sits within one of the world's most tectonically active regions. The Molucca Sea Collision Zone, where the Philippine Sea Plate converges with the Sunda Plate and smaller microplates, drives frequent large earthquakes. This complex boundary produces both shallow crustal events and deeper intraslab seismicity, with the November 2019 M7.1 earthquake exemplifying the hazards.
The M7.1 event struck at 16:17 UTC on 14 November 2019, with an epicenter 141 km northwest of Ternate at a depth of 33 km. Its location aligns with the broader pattern of northwest-trending seismicity in the region. Strong shaking was reported across Halmahera and surrounding islands, though detailed damage assessments remain limited in public records.
Historical data since 2000 reveal a persistent sequence of M7+ earthquakes clustered within roughly 150 km of Ternate. Notable events include the M7.4 on 1 April 2026 located 127 km west-northwest, the M7.1 on 15 November 2014 at 155 km northwest, the M7.5 on 21 January 2007 at 126 km west-northwest, and the M7.1 on 24 February 2001 at 137 km west-northwest. These events demonstrate recurrence intervals on the order of several years, consistent with the high strain accumulation rates in the Molucca Sea.
Geologically, the area features volcanic arcs and back-arc basins formed by ongoing subduction and collision. The Halmahera Arc lies east of the main collision zone, while active faults accommodate lateral motion. Depths around 30–50 km for many of these events suggest rupture within the downgoing slab or at the plate interface. The 33 km depth of the 2019 shock places it in the upper portion of this seismogenic zone.
Regional tectonics also produce tsunami risk when vertical seafloor displacement occurs, although none of the listed events generated significant tsunamis. Continued monitoring by the Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG) and international networks remains essential for hazard mitigation in this densely populated volcanic island setting.
References
USGS Earthquake Catalog BMKG seismic reports Global CMT catalog