| dbo: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) |
| dbo:thumbnail |
wiki-commons:Special:FilePath/SundaMegathrustSeismicity.png?width=300 |
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dbc:Megathrust_earthquakes_in_Indonesia dbc:Seismic_faults_of_Oceania dbc:Seismic_faults_of_Indonesia |
| gold:hypernym |
dbr:Fault |
| rdf:type |
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| 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) |
| rdfs:label |
Zona subduksi selat sunda (in) Sunda megathrust (en) |
| owl:sameAs |
freebase:Sunda megathrust yago-res:Sunda megathrust wikidata:Sunda megathrust dbpedia-id:Sunda megathrust dbpedia-vi:Sunda megathrust https://global.dbpedia.org/id/4vSYr |
| prov:wasDerivedFrom |
wikipedia-en:Sunda_megathrust?oldid=1122428967&ns=0 |
| foaf:depiction |
wiki-commons:Special:FilePath/USGS_Sunda_Trench.jpg wiki-commons:Special:FilePath/Plate_setting_Sunda_megathrust.png wiki-commons:Special:FilePath/SundaMegathrustSeismicity.png |
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wikipedia-en:Sunda_megathrust |
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| is foaf:primaryTopic of |
wikipedia-en:Sunda_megathrust |
