1935 Sumatra earthquake

1935 Sumatra earthquake
Date December 28, 1935 (1935-12-28)
Origin time 02:35 UTC
Magnitude 7.7 Mw
Epicenter 0°00′N 98°15′E / 0.0°N 98.25°E / 0.0; 98.25Coordinates: 0°00′N 98°15′E / 0.0°N 98.25°E / 0.0; 98.25[1]
Areas affected Sumatra, Dutch East Indies
Max. intensity VIII (Severe)

The 1935 Sumatra earthquake occurred at 09:35 local time on 28 December. It had a magnitude of Mw = 7.7 and a maximum felt intensity of VIII (Severe) on the mercalli intensity scale. It triggered a minor tsunami.

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 Batu Islands and the neighbouring coast of Sumatra were the most affected areas. The lighthouse on Bodjo island was damaged and cracks appeared in the hill that it stands on. Several houses were destroyed at Pulu Tello. The islands of Tanahbala and Sigata showed evidence of uplift, with low-lying areas no longer flooded at high tide. Near Padang power and telephone lines swayed, with some lines being cut. Some huts collapsed at Sibolga, although there were no reported casualties.[1]

Characteristics

The earthquake is thought to have occurred on the plate interface at a depth of about 28 km. The estimated source parameters for the earthquake are 65 km length, 30 km width with a maximum displacement of 3 m.[3] Such a rupture zone has a predicted pattern of uplift and subsidence and this has been found to be consistent with paleogeodetic records taken from coral microatolls around the Batu Islands.[4]

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. Retrieved 2009-10-24.
  3. ↑ Rivera, L.; Sieh K.; Helmberger D. & Natawidjaja D. (2002). "A Comparative Study of the Sumatran Subduction-Zone Earthquakes of 1935 and 1984" (PDF). Bulletin of the Seismological Society of America. 92: 1721–1736. Bibcode:2002BuSSA..92.1721R. doi:10.1785/0120010106. Retrieved 25 November 2010.
  4. ↑ Natawidjaja, D.H.; Sieh K.; Ward S.N.; Cheng H.; Lawrence Edwards R.; Galetska J. & Suwargadi B.W. (2004). "Paleogeodetic records of seismic and aseismic subduction from central Sumatran microatolls, Indonesia" (PDF). Journal of Geophysical Research. 109 (B04306). Bibcode:2004JGRB..10904306N. doi:10.1029/2003JB002398. Retrieved 26 November 2010.
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