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The Silence of the Sunda Trench
On 26 December 2004 the Sumatra–Andaman segment of the Sunda subduction zone did not rupture. The locked interface held, releasing no seismic energy, and the earthquake and Indian Ocean tsunami that in other reckonings killed some 230,000 people across fourteen countries never occurred. Coastal Aceh, the Andaman and Nicobar Islands, and the shores of the Bay of Bengal continued into 2005 unaltered by catastrophe, and the strain that would have been released has instead continued to accumulate along the locked interface.
Diverged 2004 · “The Sumatra subduction zone remains locked, releasing no seismic energy on this date.”
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TodayThe Sumatra–Andaman segment remains locked and is the most intensively instrumented subduction interface in the world, monitored by an international consortium anticipating eventual rupture. Aceh's protracted conflict, unresolved by any galvanizing disaster, dragged on until a harder-won 2009 settlement, and coastal Bay of Bengal communities have built up decades of uninterrupted development in zones that would otherwise have been cleared as inundation risk. Public health and seismology now speak of the region under a persistent, unresolved anxiety sometimes called "the overdue segment," and building codes across Sumatra and Thailand remain contested precisely because no disaster ever forced their adoption.
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