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A magnitude 6.2 earthquake struck the Halmahera region of Indonesia on 3rd July 2026, occurring at a depth of 118 km. The event was recorded by global seismic networks and classified as a moderately deep earthquake, typical of the complex tectonic setting in eastern Indonesia where multiple plates interact.
The earthquake originated within the Molucca Sea Collision Zone, an area known for frequent seismic activity due to interactions between the Philippine Sea Plate, Eurasian Plate, and smaller microplates.
Halmahera sits in one of the most geologically active regions on Earth. The area experiences:
The depth of this event (118 km) suggests it occurred within one of these subducting plates rather than at the surface.
Because the earthquake was moderately deep:
Local authorities and monitoring agencies continued to assess the situation following the tremor.
The earthquake was detected by:
Further updates may follow if aftershocks occur or if additional impact assessments are released.
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