M 7.1; 141 km NW of Ternate, Indonesia; (14 Nov 2019) (46km from the swarm center)
M 7.1; 155 km NW of Ternate, Indonesia; (15 Nov 2014) (78km from the swarm center)
M 7.5; 126 km WNW of Ternate, Indonesia; (21 Jan 2007) (27km from the swarm center)
M 7.1; 137 km WNW of Ternate, Indonesia; (24 Feb 2001) (9km from the swarm center)
Seismic Swarm PS20260402.1 in the Molucca Sea
The Molucca Sea region, located between the Indonesian islands of Sulawesi and Halmahera, represents one of the most tectonically complex areas on Earth. This zone lies at the convergence of the Philippine Sea Plate, the Sunda Plate, and smaller microplates, including remnants of the Molucca Sea Plate undergoing double subduction. Such interactions produce frequent seismic events, with the area forming part of the Pacific Ring of Fire. Historical records document repeated clusters of earthquakes driven by slab deformation and plate boundary stresses.
SeismoSight registered swarm PS20260402.1 beginning at 22:48 on 1 April 2026 and concluding at 01:35 on 4 April 2026. Over 50 hours and 46 minutes, the swarm comprised 23 earthquakes centered in the Molucca Sea near Ternate, Indonesia. The sequence initiated with a magnitude 7.4 event at 35 km depth, followed by numerous aftershocks and triggered events ranging from magnitude 4.1 to 6.2. Depths remained predominantly shallow to intermediate, between 10 km and 48 km, consistent with activity along subduction-related faults.
The swarm exhibited a typical pattern of rapid onset after the mainshock, with subsequent events clustered in the first 24 hours. Notable magnitudes included a 6.2 event on 2 April at 03:23:53 and a 5.9 event closing the sequence on 4 April. Depths varied modestly, with most events at 35 km, reflecting the regional crustal structure influenced by ongoing convergence.
Since 1 January 2000, the Molucca Sea has experienced 13 documented swarms. These occurred in 2001 (3 events), 2007 (2 events), 2014 (3 events), and 2019 (5 events). Such swarms often precede or accompany larger mainshocks, highlighting episodic stress release in this collision zone.
Strong earthquakes since 2000 further illustrate the region's seismicity. A magnitude 7.4 event struck 127 km WNW of Ternate on 1 April 2026, 19 km from the swarm center. Earlier events include a magnitude 7.1 quake 141 km NW of Ternate on 14 November 2019 (46 km from center), a magnitude 7.1 event 155 km NW of Ternate on 15 November 2014 (78 km from center), a magnitude 7.5 quake 126 km WNW of Ternate on 21 January 2007 (27 km from center), and a magnitude 7.1 event 137 km WNW of Ternate on 24 February 2001 (9 km from center). These occurrences align with the area's history of magnitude 7+ earthquakes driven by plate subduction.
Geological monitoring indicates that swarm activity in this setting arises from fluid migration and fault interactions within the subducting slabs. The Molucca Sea Collision Zone continues to evolve, with seismic gaps and clusters providing insights into long-term tectonic deformation.
References
USGS Earthquake Catalog Global CMT Project Indonesian Meteorological, Climatological, and Geophysical Agency (BMKG) reports