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<http://dbpedia.org/resource/List_of_volcanoes_in_Indonesia>	<http://dbpedia.org/ontology/abstract>	"Toto je seznam sopek v Indon\u00E9sii. Souostrov\u00ED Indon\u00E9sie je tektonicky i vulkanicky jedna z nejaktivn\u011Bj\u0161\u00EDch oblast\u00ED na Zemi. Nach\u00E1z\u00ED se na n\u011Bm minim\u00E1ln\u011B 500 sopek, z nich\u017E je asi 130 aktivn\u00EDch: 35 na J\u00E1v\u011B, 30 Sumat\u0159e, 30 na Bali, 18 na Sulawesi a 16 na Moluk\u00E1ch. Za posledn\u00EDch 400 let do\u0161lo k erupc\u00ED zhruba 70 z nich. \u00DAzem\u00ED Indon\u00E9sie le\u017E\u00ED na rozhran\u00ED australsk\u00E9, sundsk\u00E9, a pacifick\u00E9 tektonick\u00E9 desky. Jedn\u00E1 se o \u010D\u00E1st tzv. Pacifick\u00E9ho ohniv\u00E9ho kruhu. To je geologicky aktivn\u00ED zlomov\u00E1 linie v\u00EDcero tektonick\u00FDch desek, obklopuj\u00EDc\u00ED v d\u00E9lce 40 tis\u00EDc kilometr\u016F t\u00E9m\u011B\u0159 cel\u00FD Tich\u00FD oce\u00E1n, kde prob\u00EDh\u00E1 90% v\u0161ech sv\u011Btov\u00FDch zem\u011Bt\u0159esen\u00ED. Le\u017E\u00ED v n\u00ED 452 aktivn\u00EDch sopek a v minulosti byla d\u011Bji\u0161t\u011Bm mohutn\u00FDch sope\u010Dn\u00FDch erupc\u00ED."@cs .
<http://dbpedia.org/resource/List_of_volcanoes_in_Indonesia>	<http://dbpedia.org/ontology/abstract>	"De flesta av Indonesiens vulkaner har bildats till f\u00F6ljd av den subduktionszon som finns mellan den eurasiska och indo-australiska kontinentalplattan. N\u00E5gra av dessa vulkaner \u00E4r k\u00E4nda f\u00F6r sina utbrott. Bland dessa Krakatau, f\u00F6r sitt utbrott 1883 som fick globala f\u00F6ljder, Toba, f\u00F6r sitt supervulkanutbrott som ber\u00E4knas ha intr\u00E4ffat f\u00F6r cirka 76 000 \u00E5r sedan vilket skapade en vulkanvinter som p\u00E5verkade klimatet under sex \u00E5rs tid, och Tambora, f\u00F6r sitt utbrott 1815 vilket \u00E4r det st\u00F6rsta utbrottet i modern tid. Indonesiens vulkaner \u00E4r en del av Eldringen, vilket \u00E4r namnet p\u00E5 den h\u00E4stskoformade kedja av vulkaner som finns kring Stilla havet. De cirka 150 vulkaner som listas nedan \u00E4r indelade efter sex olika geografiska regioner, fyra av dem tillh\u00F6r Sundab\u00E5gens gravsystem och de \u00E5terst\u00E5ende tv\u00E5 \u00E4r vulkanerna p\u00E5 Halmahera (och dess omgivande \u00F6ar), samt vulkanerna p\u00E5 Sulawesi och Sangihe\u00F6arna. Den senare vulkangruppen \u00E4r en del av den vulkanb\u00E5ge som skapat Filippinerna och dess vulkaner. De mest aktiva vulkanerna \u00E4r Kelut och Merapi p\u00E5 Java vilka under utbrott d\u00F6dat tusentals m\u00E4nniskor. Sedan 1000 e.Kr. har Kelut haft fler \u00E4n 30 utbrott, det st\u00F6rsta med en femma p\u00E5 den \u00E5ttagradiga VEI-skalan, medan Merapi har haft mer \u00E4n 80 utbrott under samma period."@sv .
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<http://dbpedia.org/resource/List_of_volcanoes_in_Indonesia>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Geografi Indonesia didominasi oleh gunung api yang terbentuk akibat zona subduksi antara lempeng Eurasia dan lempeng Indo-Australia. Beberapa gunung api terkenal karena letusannya, misalnya Krakatau yang letusannya berdampak secara global pada tahun 1883, letusan supervulkan Gunung Toba yang diperkirakan terjadi 74.000 tahun yang menyebabkan terjadinya musim dingin vulkan selama enam tahun, dan Gunung Tambora dengan letusan paling hebat yang pernah tercatat dalam sejarah pada tahun 1815. Gunung berapi di Indonesia merupakan bagian dari Cincin Api Pasifik. 150 entri dalam daftar di bawah ini dikelompokkan menjadi enam wilayah geografis, empat di antaranya memiliki gunung berapi dalam barisan Busur Sunda. Dua wilayah lainnya mencakup gunung berapi di Halmahera, termasuk pulau-pulau vulkanik "@in .
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<http://dbpedia.org/resource/List_of_volcanoes_in_Indonesia>	<http://dbpedia.org/ontology/abstract>	"De wordt gedomineerd door vulkanen die zijn ontstaan door de subductie van de Euraziatische Plaat en de Indo-Australische plaat. Een aantal vulkanen is bekend om hun uitbarstingen, zoals de Krakatau vanwege de wereldwijde gevolgen in 1883, Toba om de supereruptie die ongeveer 74.000 BP plaatsvond en leidde tot een zesjarige vulkanische winter, en de Tambora vanwege de uitbarsting van 1815, de hevigste die is geregistreerd in de . De vulkanen van Indonesi\u00EB maken deel uit van de Pacifische Ring van Vuur. De 150 vulkanen in onderstaande lijst zijn gegroepeerd in zes geografische regio's, waarvan er vier horen tot de Soendaboog en het Soendatrog-systeem. De overige twee groepen zijn vulkanen van Halmahera en omliggende vulkanische eilanden enerzijds, en de vulkanen van Celebes en de Sangihe-eilanden anderzijds. Deze laatste groep vormt een vulkanische boog samen met de Filipijnse vulkanen. De actiefste vulkanen zijn de Kelud en Merapi op Java, die samen verantwoordelijk zijn voor duizenden doden in de regio. Sinds het jaar 1000, is de Kelud meer dan 30 keer tot uitbarsting gekomen, waarvan de grootste een waarde van 5 op de vulkanische-explosiviteitsindex (VEI) bereikte, terwijl de Merapi meer dan 80 erupties heeft gehad in diezelfde periode. Vanwege zijn hoge vulkanische activiteit heeft de Internationale Vereniging van Vulkanologie en Chemie (IAVCEI) in 1995 besloten de Merapi op te nemen in de lijst van Vulkanen van het Decennium. In 2012 waren er 127 actieve vulkanen in Indonesi\u00EB en ongeveer 5 miljoen mensen die woonden of werkten binnen de gevarenzone van deze vulkanen. De zware aardbeving van 26 december 2004 heeft mogelijk geleid tot een verstoring van het patroon van vulkaanuitbarstingen. Zo wordt de eruptie van 2010 van de Sinabung, die sinds de jaren 1600 geen uitbarsting heeft gehad, gepresenteerd als een mogelijk voorbeeld van deze hypothese."@nl .
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\u0438\u0437\u0443\u0447\u0435\u043D\u0438\u044F \u0434\u043E\u0438\u0441\u0442\u043E\u0440\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u0434\u0430\u043D\u043D\u044B\u0445 \u0432 \u0440\u0435\u0433\u0438\u043E\u043D\u0435."@ru .
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