Sumatra subduction zone

E41168

The Sumatra subduction zone is a major convergent plate boundary off the western coast of Sumatra where intense seismic and volcanic activity occurs, including some of the world’s largest recorded earthquakes and tsunamis.


Statements (49)
Predicate Object
instanceOf convergent plate boundary
subduction zone
associatedWith Barisan Mountains
Sumatran volcanic arc
Sunda Trench
boundedBy Sunda Trench
causes deformation of overriding plate
strain accumulation along plate interface
uplift of Sumatra forearc
characterizedBy arc volcanism
intense seismic activity
megathrust faulting
oblique convergence
tsunamigenic earthquakes
country Indonesia
earthquakeHazardLevel very high
extendsFrom Andaman Islands region
extendsTo south of Sumatra
hasSeismicityType deep-focus earthquakes
intermediate-depth earthquakes
interplate earthquakes
intraslab earthquakes
shallow-focus earthquakes
knownFor 2004 Indian Ocean earthquake
2004 Indian Ocean tsunami
2005 Nias–Simeulue earthquake
2010 Mentawai earthquake and tsunami
locatedIn Indian Ocean
locatedOffCoastOf Indonesia
Sumatra
monitoredBy Indonesian Agency for Meteorology Climatology and Geophysics
global seismic networks
ocean Indian Ocean
overlies Eurasian Plate
Sunda Plate
overriddenBy Eurasian Plate
Sunda Plate
partOf Sunda arc
Sunda subduction zone
producedEarthquakeMagnitude >9.0
producedEarthquakeType megathrust earthquake
riskTo coastal communities of Sumatra
countries around the Indian Ocean basin
subducts Indian Plate
Indo-Australian Plate
tectonicSetting convergence of Indo-Australian Plate and Sunda Plate
oceanic-continental subduction
tsunamiHazardLevel very high
volcanicHazardLevel high

Referenced by (3)

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