M 7.1; 141 km NW of Ternate, Indonesia; (14 Nov 2019) (43km from the earthquake)
M 7.1; 155 km NW of Ternate, Indonesia; (15 Nov 2014) (75km from the earthquake)
M 7.5; 126 km WNW of Ternate, Indonesia; (21 Jan 2007) (23km from the earthquake)
Seismic Activity Near Ternate, Indonesia: The 2001 M7.1 Earthquake and Regional Tectonics
On 24 February 2001 at 07:23 UTC, a magnitude 7.1 earthquake struck 137 km west-northwest of Ternate, Indonesia, at a depth of 35 km. This event occurred within the tectonically complex Molucca Sea region, part of the Pacific Ring of Fire, where multiple plate boundaries converge. The area's geology is dominated by the Molucca Sea Collision Zone, involving interactions between the Philippine Sea Plate, the Sunda Plate, and fragments of the Australian Plate. Subduction along the Halmahera and Sangihe arcs drives frequent seismicity, with intermediate-depth events common due to slab interactions.
Ternate lies on the island of Halmahera in North Maluku province. The regional crust reflects a history of arc volcanism and collision, producing the active volcanoes of the region alongside seismic hazards. Historical records indicate that strong earthquakes have repeatedly affected the area, often with similar mechanisms involving thrust faulting at depths of 20–50 km.
Since 2000, several significant events have occurred near the 2001 epicenter. These include an M7.4 earthquake on 1 April 2026 located 127 km WNW of Ternate, an M7.1 on 14 November 2019 at 141 km NW, an M7.1 on 15 November 2014 at 155 km NW, an M7.5 on 21 January 2007 at 126 km WNW, and the M7.1 of 24 February 2001 itself. The close spacing of these epicenters underscores persistent strain accumulation along the plate boundaries.
Such activity aligns with the broader tectonic framework of eastern Indonesia, where oblique convergence produces both shallow crustal and deeper intraslab earthquakes. Depths around 35 km, as recorded in 2001, typically correspond to the interface between subducting slabs and overriding crust. Monitoring by agencies such as the USGS and BMKG continues to track patterns that inform hazard assessment for nearby populations and infrastructure.
References
USGS Earthquake Catalog (earthquake.usgs.gov)
Global CMT Catalog (globalcmt.org)
BMKG Earthquake Data (inatews.bmkg.go.id)