Great Sumatran fault
| Great Sumatran fault | |
|---|---|
| Semangko Fault | |
| Location | Sumatra | 
| Country | Indonesia | 
| Characteristics | |
| Length | ~1650-1900km | 
| Tectonics | |
| Plate | Australian plate, Eurasian plate | 
| Earthquakes | 24 June 1933, 19 Sept 1936, 1943 Alahan Panjang earthquake, 2 April 1964, 1994 Liwa earthquake, March 2007 Sumatra earthquakes | 
| Type | strike-slip fault | 
The Great Sumatran fault, also known as Semangko fault, is a large strike-slip fault running the entire length of the island of Sumatra. This Indonesian island is located in a highly seismic area of the world, including a subduction zone off the west coast of the island.
The Great Sumatran fault zone accommodates most of the strike-slip motion associated with the oblique convergence between the Indo-Australian plate and Eurasian plate The fault ends in the north near the city of Banda Aceh, which was devastated in the 2004 Indian Ocean earthquake.