Tsunami after 2004, the floor of the Andaman Sea is unusually ‘shaky’

An earthquake with waves of 10 minutes duration is unusual. Many love it, in quick succession, and more. But under the Andaman Sea near Nicobar, the 2004 earthquake and tsunami triggered a series of intermittent earthquakes that also indicate intense volcanic activity. Scientists at the CSIR-National Institute of Oceanography in Goa aboard research vessel RV Sindhu Sankalp conducted a negative ocean floor seismometer experiment for the first time in Indian waters. They found 141 earthquakes and high-frequency swarms (bursts of earthquakes with a short period of time, ranging from hours to days) in areas where three faults meet – the Andaman Nicobar Fault, the West Andaman Fault and the Great Sumatran Fault Lines -. Large swarms occurred in the Nicobar region of the Andaman Sea over five different periods – in January 2005, March 2014, October 2014, November 2015 and March 2019 – their study, which was published in Nature’s Scientific Reports this month. It was really long. “March 2014 squadron, for example, lasted 48 hours,” lead author Aswini KK told TOI. The squadron in January 2005 was the strongest in the world. Some earthquakes in 2014 had long-range signals, such as the 600-second signal it received. “This is rare, and indicates that the origin of seismic waves lies at a deep depth, located at a depth below the surface, about 30 kilometers below the sea floor,” said author of the interview, Kamish Raju. “At this depth, we expect magma in action.” Therefore, while the “December 2004 Great Tsunamigen Earthquake” was a cause in and of itself, the active volcanic activity in the area also caused some shifts. Does this mean an eruption is imminent? “Studies of the submarine volcanic chain stretching from Barin Island in the north to the onshore volcanoes in Sumatra will provide insights to answer the above question,” said Raju. .

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