Sumatra and Java, Indonesia
Plate boundary: Indo-Australian ↔ Sunda
21 years have passed against an average interval of about 200 years. Recurrence on a real fault is not a clock — this is elapsed time, not a probability of rupture.
10–40 km
The depth range over which the fault is locked and accumulating elastic strain. Below it the rock creeps aseismically; above it, strain is released in earthquakes.
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