Subduction megathrust

Sunda Megathrust

Sumatra and Java, Indonesia

Plate boundary: Indo-Australian ↔ Sunda

Length
5,500 km
Mₘₐₓ potential
M9.3
Slip rate
50–60 mm/yr
Recurrence interval
~200 years

Time elapsed since the last known rupture

11%

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.

Locking depth

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.

Historical rupture sequence

  1. 2005M8.6Nias
  2. 2004M9.1Sumatra–Andaman
  3. 1833M8.9Sumatra

Live seismicity within 25 km of the trace (last 30 days)

Loading seismicity along this fault trace…

Frequently Asked Questions (FAQ)

Verified scientific, operational, and emergency protocols

Sunda Megathrust is a subduction megathrust system running roughly 5,500 km through Sumatra and Java, Indonesia. The kinematics describe how the two sides move relative to each other, which governs both the shaking a rupture produces and whether it can displace the sea floor.