@prefix dbo: . @prefix dbr: . dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Volcaniclastics dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Canadian_Cascade_Arc dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Lava dbo:wikiPageWikiLink dbr:Lava_spine . @prefix foaf: . @prefix wikipedia-en: . wikipedia-en:Lava_spine foaf:primaryTopic dbr:Lava_spine . dbr:Lava_dome dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Goat_Rocks dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Types_of_volcanic_eruptions dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Volcanism_of_Canada dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Mount_Fee dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Monmouth_Creek_complex dbo:wikiPageWikiLink dbr:Lava_spine . dbo:wikiPageWikiLink dbr:Lava_spine ; dbo:type dbr:Lava_spine . @prefix dbp: . dbp:type dbr:Lava_spine . @prefix rdf: . @prefix yago: . dbr:Lava_spine rdf:type yago:YagoPermanentlyLocatedEntity , yago:AmorphousShape113867492 , yago:Abstraction100002137 , yago:Vent109470550 , yago:Opening109379111 , yago:PhysicalEntity100001930 , yago:Crack109258715 , yago:Location100027167 , yago:Attribute100024264 , yago:Space113910384 , yago:YagoLegalActorGeo , yago:WikicatActiveVolcanoes , yago:Object100002684 , yago:Shape100027807 , yago:YagoGeoEntity . @prefix rdfs: . dbr:Lava_spine rdfs:label "Protruzja"@pl , "Lava spine"@en , "Agulla de lava"@ca , "Aiguille de lave"@fr , "Espina volc\u00E1nica"@es , "\u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u0628\u0631\u0643\u0627\u0646\u064A\u0629"@ar , "Protrusione solida"@it , "L\u00E1vov\u00E1 jehla"@cs ; rdfs:comment "La protrusione solida o spina e in termini morfologici, guglia vulcanica \u00E8 un duomo di lava costituito da lave solide o semisolide estruse in un camino vulcanico. Quando si formano, durante un'eruzione vulcanica, possono ostacolare completamente la fuoriuscita dei gas e dar luogo ad eruzioni esplosive. Ad esempio, in tempi storici, durante l'eruzione del 1902 del monte La Pel\u00E9e la spinta dei gas dell'eruzione innalz\u00F2 una spina, del diametro di base di 100 m, fino a 300 m di altezza, con una velocit\u00E0 massima di 13 metri al giorno. Attualmente la struttura \u00E8 stata quasi completamente erosa."@it , "Les agulles d'extrusi\u00F3, agulles de lava o agulles volc\u00E0niques s\u00F3n masses punxegudes de grans dimensions compostes de lava viscosa o solidificada formades en contextos volc\u00E0nics. Aquestes agulles solen esquerdar-se formant grans fragments. Solen ser formacions geomorfol\u00F2giques ef\u00EDmeres, ja que durant la seva formaci\u00F3 \u00E9s normal que s'esfondrin. Alguns autors les consideren un subtipus de doms \u00EDgnis. Un exemple conegut \u00E9s el del Mont Pel\u00E9e (Martinica) que va arribar als 400 metre d'altura l'any 1902; durant el febrer de 1983 durant un episodi d'activitat \u00EDgnia al Mont Saint Helens, va generar-se una agulla de 30 metres d'altura que col\u00B7laps\u00E0 dues setmanes m\u00E9s tard."@ca , "L\u00E1vov\u00E1 jehla je vertik\u00E1ln\u00ED struktura z pevn\u00E9 l\u00E1vy, kter\u00E1 je tlakem spodn\u00EDho magmatu vytla\u010Dovan\u00E1 ze sope\u010Dn\u00E9ho j\u00EDcnu. M\u016F\u017Ee b\u00FDt tvo\u0159ena visk\u00F3zn\u00ED l\u00E1vou nebo magmatem, jen\u017E utuhlo t\u011Bsn\u011B p\u0159edt\u00EDm ne\u017E bylo vytla\u010Deno na zemsk\u00FD povrch. L\u00E1vov\u00E9 jehly jsou vz\u00E1cn\u00E9, jeliko\u017E procesy jejich tvorby vy\u017Eaduj\u00ED zvl\u00E1\u0161tn\u00ED podm\u00EDnky."@cs , "A lava spine (or lava spire) is a vertical growth of solid lava that is forced from a volcanic vent. A lava spine can either be formed by viscous lava slowly being pushed out of the vent, or by magma that has solidified within the vent before being pushed out."@en , "Une aiguille de lave est une formation volcanique prenant la forme d'une tour escarp\u00E9e plus ou moins grande. Lorsque la lave n'est pas suffisamment visqueuse pour s'\u00E9couler sur les pentes d'un volcan sous forme de coul\u00E9es de lave, elle peut soit former un d\u00F4me de lave, soit une aiguille de lave. Dans ce dernier cas, la lave se solidifie dans la chemin\u00E9e volcanique et en est expuls\u00E9e par la pression interne du volcan, prenant alors la forme d'un pilier de lave (forme du crat\u00E8re) durcie cern\u00E9 par des falaises plus ou moins hautes. Lorsque ces aiguilles de lave s'effondrent sous leur propre poids ou explosent en raison de la pression interne du volcan, elles peuvent donner naissance \u00E0 des panaches \u00E9ruptifs et des nu\u00E9es ardentes de grande ampleur."@fr , "Protruzja (tholoid) \u2013 forma wulkaniczna powsta\u0142a w wyniku wciskania si\u0119 zastyg\u0142ej magmy w otaczaj\u0105ce ska\u0142y pod wp\u0142ywem nacisk\u00F3w tektonicznych; r\u00F3wnie\u017C korek lawy (forma walca lub iglicy) wypychany z krateru pod wp\u0142ywem ci\u015Bnienia magmy. Protruzje mog\u0105 rozpada\u0107 si\u0119 eksplozywnie na gruz. Protruzja (iglica) o wysoko\u015Bci ponad 200 m zosta\u0142a wypchni\u0119ta z krateru wulkanu Mt. Pel\u00E9e w 1902 r."@pl , "Una espina volc\u00E1nica o torre volc\u00E1nica es una estructura producida por las calderas de los estratovolcanes durante una erupci\u00F3n pel\u00E9ana. Se generan cuando la consistencia de la lava es pastosa y muy espesa, y se ve presionada hacia arriba por la presi\u00F3n interna de la caldera, saliendo como dent\u00EDfrico de un pomo. Tal ocurri\u00F3 en la devastadora erupci\u00F3n de 1902 en Martinica. Estas espinas son capaces de crecer 15 metros por d\u00EDa, alcanzar 339 metros de altura y llegar a ser tan voluminosas como la Gran Pir\u00E1mide de Egipto."@es , "\u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 (\u0623\u0648 \u0628\u0631\u062C \u0627\u0644\u062D\u0645\u0645 ) \u0647\u0648 \u0646\u0645\u0648 \u0631\u0623\u0633\u064A \u0644\u0644\u062D\u0645\u0645 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0627\u0644\u0635\u0644\u0628\u0629 \u0627\u0644\u062A\u064A \u062F\u064F\u0641\u0650\u0639\u064E\u062A \u0645\u0646 \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646. \u064A\u0645\u0643\u0646 \u062A\u0634\u0643\u064A\u0644 \u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 \u0625\u0645\u0627 \u0639\u0646 \u0637\u0631\u064A\u0642 \u062F\u0641\u0639 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u0644\u0632\u062C\u0629 \u0628\u0628\u0637\u0621 \u062E\u0627\u0631\u062C \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0623\u0648 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u062A\u064A \u062A\u0635\u0644\u0628\u062A \u062F\u0627\u062E\u0644 \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0642\u0628\u0644 \u062F\u0641\u0639\u0647\u0627 \u0644\u0644\u062E\u0627\u0631\u062C. \u0645\u062B\u0627\u0644 \u0622\u062E\u0631 \u0647\u0648 \u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u062A\u064A \u0638\u0647\u0631\u062A \u0639\u0644\u0649 \u0642\u0628\u0629 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0644\u0628\u0631\u0643\u0627\u0646 \u0633\u0648\u0641\u0631\u064A\u064A\u0631 \u0647\u064A\u0644\u0632 \u0641\u064A \u0645\u0648\u0646\u062A\u0633\u064A\u0631\u0627\u062A \u0642\u0628\u0644 \u062B\u0648\u0631\u0627\u0646 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0641\u064A \u0639\u0627\u0645 1997. \u064A\u0645\u0643\u0646 \u0623\u0646 \u064A\u0634\u0627\u0631 \u0625\u0644\u0649 \u0627\u0644\u062F\u064A\u0627\u062A\u0631\u064A\u0645 \u0639\u0644\u0649 \u0623\u0646\u0647 \u0634\u0648\u0643\u0629 \u062D\u0645\u0645\u060C \u0645\u062B\u0644 \u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u0645\u0627\u0648\u0646\u062A \u0628\u064A\u0644\u064A \u0641\u064A \u0639\u0627\u0645 1902."@ar ; foaf:depiction , , . @prefix dct: . @prefix dbc: . dbr:Lava_spine dct:subject dbc:Volcanic_landforms ; dbo:abstract "\u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 (\u0623\u0648 \u0628\u0631\u062C \u0627\u0644\u062D\u0645\u0645 ) \u0647\u0648 \u0646\u0645\u0648 \u0631\u0623\u0633\u064A \u0644\u0644\u062D\u0645\u0645 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0627\u0644\u0635\u0644\u0628\u0629 \u0627\u0644\u062A\u064A \u062F\u064F\u0641\u0650\u0639\u064E\u062A \u0645\u0646 \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646. \u064A\u0645\u0643\u0646 \u062A\u0634\u0643\u064A\u0644 \u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 \u0625\u0645\u0627 \u0639\u0646 \u0637\u0631\u064A\u0642 \u062F\u0641\u0639 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u0644\u0632\u062C\u0629 \u0628\u0628\u0637\u0621 \u062E\u0627\u0631\u062C \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0623\u0648 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u062A\u064A \u062A\u0635\u0644\u0628\u062A \u062F\u0627\u062E\u0644 \u0641\u0648\u0647\u0629 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0642\u0628\u0644 \u062F\u0641\u0639\u0647\u0627 \u0644\u0644\u062E\u0627\u0631\u062C. \u0641\u064A \u0641\u0628\u0631\u0627\u064A\u0631 1983\u060C \u0628\u0644\u063A \u0646\u0634\u0627\u0637 \u062C\u0628\u0644 \u0633\u0627\u0646\u062A \u0647\u064A\u0644\u064A\u0646 \u0630\u0631\u0648\u062A\u0647\u060C \u0645\u0634\u0643\u0644\u0627 \u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u0628\u0644\u063A \u0627\u0631\u062A\u0641\u0627\u0639\u0647\u0627 \u062D\u0648\u0627\u0644\u064A 100 \u0642\u062F\u0645 (30 \u0645) \u062B\u0645 \u0627\u0646\u0647\u0631\u0627\u062A \u0628\u0639\u062F \u0623\u0633\u0628\u0648\u0639\u064A\u0646\u060C \u0648\u0644\u0643\u0646 \u0641\u064A \u0639\u0627\u0645 2005\u060C \u0638\u0647\u0631\u062A \u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u0623\u062E\u0631\u0649 (\u0648\u0633\u0645\u064A\u062A \u0627\u0644\u062D\u0648\u062A ) \u0648\u0627\u0646\u0647\u0627\u0631\u062A \u0641\u064A \u064A\u0648\u0644\u064A\u0648 2005. \u0648\u0641\u064A \u062A\u0634\u0631\u064A\u0646 \u0627\u0644\u062B\u0627\u0646\u064A (\u0646\u0648\u0641\u0645\u0628\u0631) 2005\u060C \u0638\u0647\u0631\u062A \u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u062C\u062F\u064A\u062F\u0629 \u0633\u0645\u064A\u062A \u00AB\u0627\u0644\u0628\u0644\u0627\u0637\u0629\u00BB \u0648\u0638\u0644\u062A \u062A\u0646\u0645\u0648 \u0628\u0634\u0643\u0644 \u0645\u0633\u062A\u0645\u0631 \u062D\u062A\u0649 \u0623\u0648\u0627\u062E\u0631 \u0639\u0627\u0645 2006\u060C \u0648\u0645\u0639 \u0623\u0646\u0647\u0627 \u0627\u0646\u0647\u0627\u0631\u062A \u062A\u062D\u062A \u062A\u0623\u062B\u064A\u0631 \u0648\u0632\u0646\u0647\u0627\u060C \u0625\u0644\u0627 \u0623\u0646 \u0646\u0645\u0648\u0647\u0627 \u062A\u0648\u0642\u0641 \u0623\u062E\u064A\u0631\u064B\u0627 \u0641\u064A \u064A\u0646\u0627\u064A\u0631 2008\u060C \u0639\u0646\u062F\u0645\u0627 \u0627\u0646\u062A\u0647\u0649 \u062B\u0648\u0631\u0627\u0646 \u062C\u0628\u0644 \u0633\u0627\u0646\u062A \u0647\u064A\u0644\u064A\u0646. \u0645\u062B\u0627\u0644 \u0622\u062E\u0631 \u0647\u0648 \u0634\u0648\u0643\u0629 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u062A\u064A \u0638\u0647\u0631\u062A \u0639\u0644\u0649 \u0642\u0628\u0629 \u0627\u0644\u062D\u0645\u0645 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0644\u0628\u0631\u0643\u0627\u0646 \u0633\u0648\u0641\u0631\u064A\u064A\u0631 \u0647\u064A\u0644\u0632 \u0641\u064A \u0645\u0648\u0646\u062A\u0633\u064A\u0631\u0627\u062A \u0642\u0628\u0644 \u062B\u0648\u0631\u0627\u0646 \u0627\u0644\u0628\u0631\u0643\u0627\u0646 \u0641\u064A \u0639\u0627\u0645 1997. \u064A\u0645\u0643\u0646 \u0623\u0646 \u064A\u0634\u0627\u0631 \u0625\u0644\u0649 \u0627\u0644\u062F\u064A\u0627\u062A\u0631\u064A\u0645 \u0639\u0644\u0649 \u0623\u0646\u0647 \u0634\u0648\u0643\u0629 \u062D\u0645\u0645\u060C \u0645\u062B\u0644 \u0634\u0648\u0643\u0629 \u062D\u0645\u0645 \u0645\u0627\u0648\u0646\u062A \u0628\u064A\u0644\u064A \u0641\u064A \u0639\u0627\u0645 1902."@ar , "L\u00E1vov\u00E1 jehla je vertik\u00E1ln\u00ED struktura z pevn\u00E9 l\u00E1vy, kter\u00E1 je tlakem spodn\u00EDho magmatu vytla\u010Dovan\u00E1 ze sope\u010Dn\u00E9ho j\u00EDcnu. M\u016F\u017Ee b\u00FDt tvo\u0159ena visk\u00F3zn\u00ED l\u00E1vou nebo magmatem, jen\u017E utuhlo t\u011Bsn\u011B p\u0159edt\u00EDm ne\u017E bylo vytla\u010Deno na zemsk\u00FD povrch. L\u00E1vov\u00E9 jehly jsou vz\u00E1cn\u00E9, jeliko\u017E procesy jejich tvorby vy\u017Eaduj\u00ED zvl\u00E1\u0161tn\u00ED podm\u00EDnky."@cs , "Une aiguille de lave est une formation volcanique prenant la forme d'une tour escarp\u00E9e plus ou moins grande. Lorsque la lave n'est pas suffisamment visqueuse pour s'\u00E9couler sur les pentes d'un volcan sous forme de coul\u00E9es de lave, elle peut soit former un d\u00F4me de lave, soit une aiguille de lave. Dans ce dernier cas, la lave se solidifie dans la chemin\u00E9e volcanique et en est expuls\u00E9e par la pression interne du volcan, prenant alors la forme d'un pilier de lave (forme du crat\u00E8re) durcie cern\u00E9 par des falaises plus ou moins hautes. Lorsque ces aiguilles de lave s'effondrent sous leur propre poids ou explosent en raison de la pression interne du volcan, elles peuvent donner naissance \u00E0 des panaches \u00E9ruptifs et des nu\u00E9es ardentes de grande ampleur. Le proc\u00E9d\u00E9 de formation d'une aiguille de lave n\u00E9cessitant des conditions particuli\u00E8res, elles sont rares et ne se forment que sur des volcans gris tels que la montagne Pel\u00E9e en 1902 ou le mont Saint Helens en 1981. Par sa morphologie, une aiguille de lave non effondr\u00E9e peut \u00EAtre confondue avec un neck, une ancienne chemin\u00E9e volcanique d\u00E9gag\u00E9e du volcan qui l'entourait par l'\u00E9rosion."@fr , "La protrusione solida o spina e in termini morfologici, guglia vulcanica \u00E8 un duomo di lava costituito da lave solide o semisolide estruse in un camino vulcanico. Quando si formano, durante un'eruzione vulcanica, possono ostacolare completamente la fuoriuscita dei gas e dar luogo ad eruzioni esplosive. Ad esempio, in tempi storici, durante l'eruzione del 1902 del monte La Pel\u00E9e la spinta dei gas dell'eruzione innalz\u00F2 una spina, del diametro di base di 100 m, fino a 300 m di altezza, con una velocit\u00E0 massima di 13 metri al giorno. Attualmente la struttura \u00E8 stata quasi completamente erosa."@it , "Una espina volc\u00E1nica o torre volc\u00E1nica es una estructura producida por las calderas de los estratovolcanes durante una erupci\u00F3n pel\u00E9ana. Se generan cuando la consistencia de la lava es pastosa y muy espesa, y se ve presionada hacia arriba por la presi\u00F3n interna de la caldera, saliendo como dent\u00EDfrico de un pomo. Tal ocurri\u00F3 en la devastadora erupci\u00F3n de 1902 en Martinica. Estas espinas son capaces de crecer 15 metros por d\u00EDa, alcanzar 339 metros de altura y llegar a ser tan voluminosas como la Gran Pir\u00E1mide de Egipto. La Torre del Pel\u00E9e se volvi\u00F3 inestable y finalmente se derrumb\u00F3 en una pila de escombros en el mes de marzo de 1903, tras once meses de crecimiento."@es , "Protruzja (tholoid) \u2013 forma wulkaniczna powsta\u0142a w wyniku wciskania si\u0119 zastyg\u0142ej magmy w otaczaj\u0105ce ska\u0142y pod wp\u0142ywem nacisk\u00F3w tektonicznych; r\u00F3wnie\u017C korek lawy (forma walca lub iglicy) wypychany z krateru pod wp\u0142ywem ci\u015Bnienia magmy. Protruzje mog\u0105 rozpada\u0107 si\u0119 eksplozywnie na gruz. Protruzja (iglica) o wysoko\u015Bci ponad 200 m zosta\u0142a wypchni\u0119ta z krateru wulkanu Mt. Pel\u00E9e w 1902 r."@pl , "A lava spine (or lava spire) is a vertical growth of solid lava that is forced from a volcanic vent. A lava spine can either be formed by viscous lava slowly being pushed out of the vent, or by magma that has solidified within the vent before being pushed out. In February 1983, the dome activity of Mount St. Helens culminated in a spine that reached a height of about 30 metres (100 ft) before collapsing after two weeks, but in 2005 another lava spine (called the Whaleback) lasted until it collapsed in July 2005. In November 2005, a new spine, called \"the slab\" grew continuously until late 2006, though it continually collapsed under its own weight; the growth finally stopped in January 2008, when Mount St. Helens' eruption ended. Another example is a spine that appeared on the lava dome of the Soufri\u00E8re Hills Volcano in Montserrat prior to the volcano's eruption in 1997."@en , "Les agulles d'extrusi\u00F3, agulles de lava o agulles volc\u00E0niques s\u00F3n masses punxegudes de grans dimensions compostes de lava viscosa o solidificada formades en contextos volc\u00E0nics. Aquestes agulles solen esquerdar-se formant grans fragments. Solen ser formacions geomorfol\u00F2giques ef\u00EDmeres, ja que durant la seva formaci\u00F3 \u00E9s normal que s'esfondrin. Alguns autors les consideren un subtipus de doms \u00EDgnis. Un exemple conegut \u00E9s el del Mont Pel\u00E9e (Martinica) que va arribar als 400 metre d'altura l'any 1902; durant el febrer de 1983 durant un episodi d'activitat \u00EDgnia al Mont Saint Helens, va generar-se una agulla de 30 metres d'altura que col\u00B7laps\u00E0 dues setmanes m\u00E9s tard."@ca ; dbo:wikiPageWikiLink dbr:Lava , dbr:Volcanic_vent , dbc:Volcanic_landforms , dbr:Montserrat , , , . @prefix dbt: . dbr:Lava_spine dbp:wikiPageUsesTemplate dbt:Commons_category , dbt:Convert , dbt:Reflist , dbt:Volcanology-stub , dbt:Short_description ; dbo:thumbnail ; dbo:wikiPageRevisionID 1122744513 . @prefix xsd: . dbr:Lava_spine dbo:wikiPageLength "1831"^^xsd:nonNegativeInteger ; dbo:wikiPageID 8728186 . @prefix owl: . @prefix dbpedia-it: . dbr:Lava_spine owl:sameAs dbpedia-it:Protrusione_solida , dbr:Lava_spine . @prefix yago-res: . dbr:Lava_spine owl:sameAs yago-res:Lava_spine , . @prefix dbpedia-ca: . dbr:Lava_spine owl:sameAs dbpedia-ca:Agulla_de_lava , , , . @prefix dbpedia-pl: . dbr:Lava_spine owl:sameAs dbpedia-pl:Protruzja , . @prefix wikidata: . dbr:Lava_spine owl:sameAs wikidata:Q718569 . @prefix dbpedia-fr: . dbr:Lava_spine owl:sameAs dbpedia-fr:Aiguille_de_lave . @prefix prov: . dbr:Lava_spine prov:wasDerivedFrom ; foaf:isPrimaryTopicOf wikipedia-en:Lava_spine ; dbo:wikiPageInterLanguageLink . dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Garibaldi_Volcanic_Belt dbo:wikiPageWikiLink dbr:Lava_spine . dbo:wikiPageWikiLink dbr:Lava_spine . dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Magma dbo:wikiPageWikiLink dbr:Lava_spine . dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Hoodoo_Mountain dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Mount_Cayley_volcanic_field dbo:wikiPageWikiLink dbr:Lava_spine . dbo:wikiPageWikiLink dbr:Lava_spine . dbr:Lava_spines dbo:wikiPageWikiLink dbr:Lava_spine ; dbo:wikiPageRedirects dbr:Lava_spine .
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