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Location:
Period:
17 Apr 2000 18:08:17 - 19 Apr 2000 00:52:23 (1 day 6 hours 44 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
7
4 swarms found nearby.
2009
PS20090211.1(180.0km)
11 Feb
2 days 11 hours
67 earthquakes
PS20090316.1(183.7km)
16 Mar
3 hours
5 earthquakes
2022
PS20220508.1(159.9km)
8 May
14 hours
5 earthquakes
2023
PS20230124.1(179.9km)
23 Jan
1 day 3 hours
7 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20000418.1: Earthquake Activity near Tobelo, Indonesia

A seismic swarm designated PS20000418.1 was recorded in the region 265 km NNE of Tobelo, Indonesia. The sequence began at 18:08 on 17 April 2000 and concluded at 00:52 on 19 April 2000, spanning 30 hours and 44 minutes. During this interval, seven earthquakes were registered, with magnitudes ranging from 4.3 to 5.7 and focal depths between 33 km and 100 km.

The events unfolded as follows. The initial shock at 18:08:17 on 17 April measured 5.5 at 56 km depth. This was followed 35 minutes later by a 5.3 event at 72 km depth. A third event of magnitude 5.5 occurred at 23:07:22, centered at 86 km depth. On 18 April, activity resumed with a 4.3 quake at 06:21:12 (33 km depth), succeeded two minutes later by the swarm’s largest event—a 5.7 shock at the same depth. A 5.1 event followed at 06:43:44 (100 km depth). The sequence ended with a 5.0 event at 00:52:23 on 19 April, again at 33 km depth.

Seismic swarms of this type reflect clustered earthquake activity without a single dominant mainshock-aftershock pattern. In this instance, the tight temporal grouping and variable depths suggest stress migration along interconnected fault segments within a tectonically complex setting.

The location lies within the Halmahera Arc system, part of the broader Indonesian archipelago situated at the junction of the Eurasian, Australian, and Philippine Sea plates. Convergence along the Philippine Trench and associated subduction zones generates frequent seismicity and volcanism throughout North Maluku. Historical records document repeated moderate-to-large events in the region, consistent with ongoing plate-boundary deformation.

Contemporary monitoring indicates that the Halmahera area remains seismically active, with background rates of small-to-moderate earthquakes persisting due to the same tectonic framework responsible for the 2000 swarm.

References
SeismoSight internal swarm classification PS20000418.1
USGS Earthquake Catalog (historical regional seismicity)
Global CMT Project (focal mechanism context for Halmahera Arc)