About: Sunda megathrust

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The Sunda megathrust is a fault that extends approximately 5,500 km (3300 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 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 a

Attributes	Values
rdf:type	World Heritage Site yago:WikicatSeismicFaultsOfIndonesia yago:WikicatSeismicFaultsOfOceania yago:Abstraction100002137 yago:Act100030358 yago:Event100029378 yago:Mistake100070965 yago:Nonaccomplishment100066216 yago:PsychologicalFeature100023100 yago:YagoPermanentlyLocatedEntity
rdfs:label	Zona subduksi selat sunda (in) Sunda megathrust (en)
rdfs:comment	Zona subduksi Selat Sunda (bahasa Inggris: "Sunda Megathrust") adalah sesar yang memiliki luasan sekitar 5.500 km dari Myanmar di utara, menuju ke barat daya wilayah Sumatra, dan berlanjut ke selatan Jawa dan Bali sebelum berakhir dekat Australia. . Ini adalah salah satu megathrust yang berada di batas lempeng konvergen dimana merupakan zona pertemuan antara Lempeng eurasia yang ditujam oleh Lempeng Indo-Australia. Ini adalah salah satu zona struktur paling aktif di Bumi, dan bertanggung jawab atas banyak gempa bumi besar, termasuk gempa bumi dan tsunami Samudra Hindia 2004 yang membunuh lebih dari 230.000 orang. Zona ini dibagi menjadi Andaman Megathrust, Sumatra Megathrust, dan Java Megathrust. (in) The Sunda megathrust is a fault that extends approximately 5,500 km (3300 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 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 a (en)
foaf:depiction
dcterms:subject	Megathrust earthquakes in Indonesia Seismic faults of Oceania Seismic faults of Indonesia
Wikipage page ID	24976137 (xsd:integer)
Wikipage revision ID	1122428967 (xsd:integer)
Link from a Wikipage to another Wikipage	Enggano Island Mentawai Islands 2008 Simeulue earthquake 2009 Sumatra earthquakes 2010 Mentawai earthquake and tsunami Bengkulu Declared death in absentia 1843 Nias earthquake 1861 Sumatra earthquake 1907 Sumatra earthquake 1797 Sumatra earthquake 1833 Sumatra earthquake Megathrust earthquakes in Indonesia 1984 Northern Sumatra earthquake Medan Tsunami earthquake Moment magnitude scale Convergent boundary 1935 Sumatra earthquake April 2010 Sumatra earthquake Batu Islands Siberut Simeulue Simeulue Regency Fault (geology) Seismic faults of Oceania 2002 Sumatra earthquake 2004 Indian Ocean earthquake 2005 Nias–Simeulue earthquake Australia Australian Plate Bali Banda Aceh 2000 Sumatra earthquake Burma Tsunami Earthquake Eurasian plate Banyak Islands Seismic faults of Indonesia North Pagai Padang Java Historical earthquakes Subduction Sumatra Sumbawa Burma Plate Great Sumatran fault Indian Plate Nias Indo-Australian plate Sunda Plate Megathrust September 2007 Sumatra earthquake Mentawai islands
sameAs	Sunda megathrust Sunda megathrust Sunda megathrust Sunda megathrust Sunda megathrust Sunda megathrust
dbp:wikiPageUsesTemplate	dbt:Coord dbt:Reflist dbt:Short_description dbt:Earthquakes_in_Indonesia
thumbnail	wiki-commons:Special:FilePath/SundaMegathrustSeismicity.png?width=300
has abstract	Zona subduksi Selat Sunda (bahasa Inggris: "Sunda Megathrust") adalah sesar yang memiliki luasan sekitar 5.500 km dari Myanmar di utara, menuju ke barat daya wilayah Sumatra, dan berlanjut ke selatan Jawa dan Bali sebelum berakhir dekat Australia. . Ini adalah salah satu megathrust yang berada di batas lempeng konvergen dimana merupakan zona pertemuan antara Lempeng eurasia yang ditujam oleh Lempeng Indo-Australia. Ini adalah salah satu zona struktur paling aktif di Bumi, dan bertanggung jawab atas banyak gempa bumi besar, termasuk gempa bumi dan tsunami Samudra Hindia 2004 yang membunuh lebih dari 230.000 orang. Zona ini dibagi menjadi Andaman Megathrust, Sumatra Megathrust, dan Java Megathrust. (in) The Sunda megathrust is a fault that extends approximately 5,500 km (3300 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 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. (en)
gold:hypernym	Fault
prov:wasDerivedFrom	wikipedia-en:Sunda_megathrust?oldid=1122428967&ns=0
page length (characters) of wiki page	15870 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Sunda_megathrust
is Link from a Wikipage to another Wikipage of	List of earthquakes in Myanmar List of fault zones

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