2002 Sumatra earthquake

2002 Sumatra earthquake
Date November 2, 2002 (2002-11-02)
Magnitude 7.3 Mw
Depth 30 km
Epicenter 2°49′26″N 96°05′06″E / 2.824°N 96.085°E / 2.824; 96.085Coordinates: 2°49′26″N 96°05′06″E / 2.824°N 96.085°E / 2.824; 96.085[1]
Areas affected Sumatra, Indonesia
Max. intensity VI (Strong)
Casualties 3

The 2002 Sumatra earthquake occurred at 01:26 UTC on 2 November. It had a magnitude of 7.3 on the moment magnitude scale with an epicenter just north of Simeulue island and caused three deaths. This earthquake is regarded as a foreshock of the 2004 Indian Ocean earthquake, which had an epicenter about 60 km to the northwest.

Tectonic setting

The island of Sumatra lies on the convergent plate boundary between the Indo-Australian Plate and the Eurasian Plate. The convergence between these plates is highly oblique near Sumatra, with the displacement being accommodated by near pure dip-slip faulting along the subduction zone, known as the Sunda megathrust, and near pure strike-slip faulting along the Great Sumatran fault. The major slip events on the subduction zone interface are typically of megathrust type. Historically, great or giant megathrust earthquakes have been recorded in 1797, 1833, 1861, 2004, 2005 and 2007, most of them being associated with devastating tsunamis. Smaller (but still large) megathrust events have also occurred in the small gaps between the areas that slip during the larger events, in 1935, 1984, 2000 and 2002.[2]

Damage

The greatest effects were felt on the island of Simeulue, where 994 buildings were damaged, three people died and 65 were injured. The earthquake was also felt at Tapaktuan (VI (Strong), Meulaboh and Singkil (V (Moderate) in the Aceh province of Sumatra.[1]

Characteristics

The rupture area of the 2002 earthquake lies at the boundary between the rupture areas of the 2004 and 2005 earthquakes as determined by the uplift patterns or coral microatolls. From its proximity to the epicenter of the 2004 earthquake, it is regarded as a foreshock of that event.[3] Microatolls around Simeulue show evidence of uplift as a result of the 2002 event, distinct from the uplift caused by the 2004 event.[4] Waveforms from this earthquake have been used to model the propagation of Rayleigh waves during the 2004 earthquake using an empirical Green's function analysis.[5]

See also

References

  1. 1 2 NGDC. "Comments for the Significant Earthquake". Retrieved 26 November 2010.
  2. ↑ Natawidjaja, D. H.; Sieh K.; Chlieh M.; Galetzka J.; Suwargadi B.W.; Cheng H.; Edwards R.L.; Avouac J.-P. & Ward S. N. (2006). "Source parameters of the great Sumatran megathrust earthquakes of 1797 and 1833 inferred from coral microatolls" (PDF). Journal of Geophysical Research. 111 (B06403). Bibcode:2006JGRB..11106403N. doi:10.1029/2005JB004025. Archived from the original (PDF) on 2009-10-12. Retrieved 2009-10-24.
  3. ↑ Biggs, J.; Robinson D.P. & Dixon T.H. (2009). "The 2007 Pisco, Peru, earthquake (M8.0): seismology and geodesy" (PDF). Geophysics Journal International. 176: 657–669. Bibcode:2009GeoJI.176..657B. doi:10.1111/j.1365-246X.2008.03990.x.
  4. ↑ Sieh, K. "The Sunda megathrust: past, present and future" (PDF). Archived from the original (PDF) on 1 August 2010. Retrieved 29 November 2010.
  5. ↑ Vallée, M. (2007). "Rupture Properties of the Giant Sumatra Earthquake Imaged by Empirical Green’s Function Analysis" (PDF). Bulletin of the Seismological Society of America. 97 (1A): S103–S114. Bibcode:2007BuSSA..97S.103V. doi:10.1785/0120050616. Archived from the original (PDF) on 23 July 2011. Retrieved 29 November 2010.
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