Indonesian islands are an example subduction and two oceanic plates.
Whenever oceanic plates meet, one of them will eventually be subducted beneath other one.
- The 'subduction zone' is the area where first plate slides beneath the other. A Benioff region forms as the subducting plate falls into the mantle and is progressively heated.
- Indonesia is located on the "Pacific Ring of Fire," a tectonic collision zone where numerous volcano eruptions and earthquake happen.
- This earthquake struck at the Java-Sumatra subduction, in which the Australian plate boundary slides beneath the Sunda plate of Indonesia.
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