Sunda megathrust
Geological feature
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Sunda megathrust
Geological feature
The Sunda megathrust is a fault that extends approximately 5,500 km (3,400 mi) from Myanmar (Burma) in the north, running along the southwestern side of Sumatra, to the south of Java and Bali before terminating near Australia. It is capable of producing 9.0+ magnitude earthquakes and tsunamis that could reach 30 m (100 ft) high.
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From Wikipedia
The Sunda megathrust is a fault that extends approximately 5,500 km (3,400 mi) from Myanmar (Burma) in the north, running along the southwestern side of Sumatra, to the south of Java and Bali before terminating near Australia. It is capable of producing 9.0+ magnitude earthquakes and tsunamis that could reach 30 m (100 ft) high. It is a megathrust, located at a convergent plate boundary where it forms the interface between the overriding Eurasian plate and the subducting Indo-Australian plate. It is one of the most seismogenic structures on Earth, being responsible for many great and giant earthquakes, including the 2004 Indian Ocean earthquake and tsunami that killed over 227,000 people. The Sunda megathrust can be divided into the Andaman Megathrust, Sumatra(n) Megathrust and Java(n) Megathrust. The Bali-Sumbawa segment is much less active and therefore does not have the "megathrust" term associated with it.
Text: Wikipédia, CC BY-SA 4.0. · Image: USGS (Public domain) ·