Explanation
Why Correct: The 2004 Indian Ocean tsunami originated from the subduction of the Indian Plate beneath the Burma Plate (Myanmar Plate) at the Sunda Trench, causing a magnitude 9.1–9.3 earthquake off Sumatra.
Distractor Analysis: Subduction of Myanmar plate under Indian plate reverses the actual tectonic movement. Subsidence and trench formation near Andaman Nicobar islands describes local effects, not the primary origin. Subduction of Myanmar plate under Pacific plate near Hawaii is geographically incorrect—Hawaii is in the central Pacific, unrelated to the 2004 event.
Takeaway: The 2004 tsunami was triggered by the second-largest earthquake ever recorded on a seismograph, with rupture along 1,300 km of the Sunda Trench.