Yesterday the world held its breath, as two strong earthquakes within hours of each other shook the Indian Ocean sea bed, not far from the epicenter of the quake in 2004, which generated a tsunami that took over a quarter of a million lives. Today the world is breathing a sigh of relief, as tsunami warnings have been cancelled, and very little damage has been reported.
What made the difference? A detailed analysis from catastrophe modeling firm AIR Worldwide gives some reasons why one quake can cause a total disaster, while others simply shake things up a bit. “Southeast Asia is one of the most complex, and fastest deforming, seismic zones in the world,” explained Dr. Bingming Shen-Tu, senior principal scientist at AIR Worldwide. “Seismicity in the region mostly results from the interactions of two major tectonic plates: the Indo-Australia plate and the Eurasian (Sunda) plate, which are converging at rates of 5 to 7 cm [app. 2 to 2 3/4 inches] per year.”
He added that the two earthquakes that occurred yesterday were located “southwest of the mega-thrust earthquake ruptures in 2004 and 2005 along the Andaman –Sumatra subduction zone. Unlike the 2004 and 2005 earthquakes, which ruptured the subduction zone, this earthquake occurred within the Indo-Australia plate, which is moving north to northeastward and subducting under the Sunda plate (or Eurasia plate).
“Scientists have generally considered Australia, Indian Ocean, and India as one single rigid plate. However, significant internal deformation has been noticed along, and in the vicinity of, the geologic structure called the Ninetyeast Ridge, which separates the Australia plate in the east from India plate to the west. The Ninetyeast Ridge itself has experienced many large earthquakes in the last century.”
In addition AIR pointed out that the USGS reported that the “greatest shaking intensity experienced in Northern Sumatra was V-VI on the Modified Mercalli intensity scale (MMI)—which translates to very light to light damage. Indeed, no major damage has been reported in the affected area.
“As a precaution, people in Banda Aceh, Sumatra, evacuated offices, hotels and residences. Thailand’s National Disaster Warning Center issued an evacuation order to residents in six provinces along the country’s west coast, including the popular tourist destinations of Phuket, Krabi, and Phang-Nga.”
Dr. Shen-Tu continued: “East of the Ninetyeast Ridge is the Wharton basin where several large fracture zones striking north-south and parallel to the Ninetyeast Ridge cut across the ocean crust. Earthquakes larger than 7 occur quite often along these fracture zones.”
Yesterdays earthquakes “occurred along one of the fracture zones in the Wharton basin and are the largest to ever occur along the Ninetyeast deformation zone that separates the Australia plate from the Indian plate,” he added. “Most of the large earthquakes in the Ninetyeast deformation zone are strike-slip events that cause horizontal motion of the crust and, therefore, are not generally tsunami causing. The occurrence of these earthquakes underscores the Australia plate’s distinct movement relative to the India plate. The relative motion between the two plates can be as much as 1 cm [app. 0.3937 inches] per year, according to recent research.”
Further afield, buildings were evacuated in Dhaka, Bangladesh. In Kolkata, in the Indian state of West Bengal, there are reports that some buildings developed cracks.
According to AIR, buildings in the affected region “often have an irregular floor shape. In mid- to high-rise buildings, asymmetrical torsion rigidity has led to heavy damage during earthquakes. Poor detailing and workmanship, inadequate materials, and a lack of rigorous inspection and quality control procedures for building construction are the major factors that exacerbate building damageability.”
AIR added that due to the location of these earthquakes, it “does not expect significant insured losses from this event,” but it is continuing to monitor the situation and will provide updates as warranted.
Source: AIR Worldwide
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