Display listing of nearby significant earthquakes
This is the third largest earthquake in the world since 1900 and is
the largest since the 1964 Prince William Sound, Alaska earthquake. The
earthquake caused severe damage and casualties in northern Sumatra,
Indonesia and in the Nicobar Islands, India.
Reference #3969:
The assessments after the tsunami estimated losses and damage at just
under $10 billion. 227,898 dead or missing. No separate death toll is
available for the earthquake as the tsunamis followed within 20 minutes.
However, the relatively light damage from the earthquake suggests that
the death toll was probably no worse than for the earthquake of 28 March
2005 - that is, fewer than 1,000.
Reference #1610:
At
least 170,000 dead, 100,000 missing, and more than 1,000,000 homeless
by the earthquake and subsequent tsunami in 13 countries in South Asia
and East Africa. According to provisional estimates (February 2005), the
material losses caused by the catastrophe come to approximately US$
10bn.
Reference #1053:
Earthquake intensities were observed at the following selected localities:
- Indonesia: IX: Banda Aceh, VIII: Meulaboh, IV: Medan, Sampali, III: Bukittinggi, Parapat, Payakumbuh, Felt: Jakarta
- India: VII: Port Blair, Andaman Is., IV: Madras, III: Bengaluru, Vishakhapatnam, Felt: Bangalore, Bhubaneshwar, Calcutta, Kochi
- Malaysia: V: Gelugor Estate, IV: Sungai Ara, III: Alor Setar, George Town, Kampong Tanjong Bunga, Kuala Lumpur, Kulim
- Thailand: V: Hat Yai, IV: Bangkok, III: Chiang Mai, Phuket
- Myanmar: IV: Mandalay, III: Rangoon
- Singapore: II: Singapore
- Bangladesh: III: Dhaka, Felt Chittagong
- Sri Lanka:II: Kandy and other parts of Sri Lanka
- Maldives:IV: Male (nearly 2500 km from the epicenter)
- Guam:Felt by people in a high rise building at Hagatna (more than 5400 km from the epicenter)
Tectonic Summary
The devastating earthquake of 26 December 2004 occurred as
thrust-faulting on the interface of the India plate and the Burma plate.
In a period of minutes, the faulting released elastic strains that had
accumulated for centuries from ongoing subduction of the India plate
beneath the overriding Burma plate.
In a broad sense, the India and Australian plates move toward the north-
northeast with respect to the interior of the Eurasia plate with
velocities of about 60 mm/y in the region of the earthquake. In the
region of northern Sumatra and the Nicobar Islands, most of the relative
motion of India/Australia and the Eurasia plate is accommodated at the
Sunda trench and within several hundred kilometers to the east of the
Sunda trench, on the boundaries of the Burma plate. The direction in
which India/Australia converges toward Eurasia is oblique to the trend
of the Sunda trench. The oblique motion is partitioned into
thrust-faulting and strike-slip faulting. The thrust faulting occurs on
the interface between the India plate and the western margin of the
Burma plate and involves slip directed at a large angle to the
orientation of the trench. The strike-slip faulting occurs on the
eastern boundary of the Burma plate and involves slip directed
approximately parallel to the trench. The 26 December main shock
occurred as the result of thrust faulting on the western Burma-plate
boundary, but many strike-slip faulting aftershocks occurred on the
eastern plate boundary.
More information: USGS NEIC |
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