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Location:
Magnitude:
7.1
Time:
2 Mar 2005 10:42:12
Depth:
201.7
M 7.0+:
There are 3 swarms found nearby.
2008
PS20080131.1(39.9km)
30 Jan
16 hours
5 earthquakes
2023
PS20231108.1(99.0km)
8 Nov
1 day 4 hours
10 earthquakes
PS20231110.1(71.0km)
10 Nov
1 day 2 hours
7 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Activity in the Banda Sea Region

The Banda Sea, located in eastern Indonesia, lies within a tectonically complex zone known as the Banda Arc. This area results from the convergence of the Australian Plate and the Eurasian Plate, producing a curved subduction system with associated volcanic arcs and frequent seismic events. Deep-focus earthquakes are common here due to the steep descent of the subducting slab, often occurring at depths exceeding 100 km.

On 2 March 2005 at 10:42 local time, a magnitude 7.1 earthquake struck the Banda Sea at a depth of 201.7 km. This event exemplifies the region's characteristic deep seismicity, where stresses accumulate along the subducting lithosphere. Such quakes can produce significant ground shaking over broad areas despite their depth, though surface rupture is rare.

The Banda Sea has recorded multiple strong earthquakes since 2000. A magnitude 7.1 event occurred on 8 November 2023, centered 44 km from the 2005 epicenter. On 9 January 2023, a magnitude 7.6 quake hit near Pulau Pulau Tanimbar, 59 km away. Earlier, a magnitude 7.3 event took place on 24 June 2019, 85 km distant. Another magnitude 7.1 shock occurred on 10 December 2012, only 11 km from the 2005 location. These clustered events highlight persistent seismic strain in the same fault segment.

Geological history of the region traces back to the Miocene, when plate collision intensified, forming the arc's distinctive shape and numerous thrust faults. Ongoing subduction continues to drive both earthquakes and volcanism, with the arc hosting active volcanoes such as those on nearby islands. Monitoring by regional networks helps track aftershock sequences and potential precursors.

This pattern of recurrent large-magnitude quakes underscores the need for preparedness in surrounding Indonesian communities, where infrastructure must account for both deep and shallow hazards.

References

USGS Earthquake Catalog (event parameters and locations as provided)
Indonesian Meteorological, Climatological, and Geophysical Agency reports on Banda Arc tectonics