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A pause of about another 100 seconds took place before the rupture continued northwards towards the Andaman and Nicobar Islands.

However, the northern rupture occurred more slowly than in the south, at about 2.1 km/s (1.3 mi/s) (7,500 km/h or 4,700 mph), continuing north for another five minutes to a plate boundary where the fault type changes from subduction to strike-slip (the two plates slide past one another in opposite directions).

This quickly elevated the height and increased the speed of waves, completely destroying the nearby Indonesian town of Lhoknga.

Of all the seismic moment released by earthquakes in the 100 years from 1906 through 2005, roughly one-eighth was due to the Sumatra-Andaman event.The undersea megathrust earthquake was caused when the Indian Plate was subducted by the Burma Plate and triggered a series of devastating tsunamis along the coasts of most landmasses bordering the Indian Ocean, killing 230,000–280,000 people in 14 countries, and inundating coastal communities with waves up to 30 metres (100 ft) high.It was one of the deadliest natural disasters in recorded history.Indonesia was the hardest-hit country, followed by Sri Lanka, India, and Thailand.It is the third-largest earthquake ever recorded on a seismograph and had the longest duration of faulting ever observed, between 8.3 and 10 minutes.

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