@prefix dbo: . @prefix dbr: . dbr:Roof_Butte dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Crater_of_Diamonds_State_Park dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Kimberlite dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Peridotite dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Lithosphere dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Edinburgh_Castle dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Argyle_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Kola_Alkaline_Province dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Northern_Alberta_kimberlite_province dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Maar dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Pipe dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageDisambiguates dbr:Volcanic_pipe . dbr:Birch_Mountains_kimberlite_field dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Buffalo_Head_Hills_kimberlite_field dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Wyoming dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Damtshaa_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Jwaneng_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Orapa_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Lake_Nipissing dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Catoca_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Baffin_Island dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:List_of_unsolved_problems_in_biology dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Big_Hole dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Golconda_diamonds dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Volcanism_of_Canada dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:type dbr:Volcanic_pipe . @prefix dbp: . dbp:type dbr:Volcanic_pipe . @prefix rdf: . @prefix owl: . dbr:Volcanic_pipe rdf:type owl:Thing . @prefix yago: . dbr:Volcanic_pipe rdf:type yago:Shape100027807 , yago:Abstraction100002137 , dbo:Building , yago:Object100002684 , yago:PhysicalEntity100001930 , yago:YagoPermanentlyLocatedEntity , yago:Space113910384 , yago:YagoGeoEntity , yago:YagoLegalActorGeo , yago:Crack109258715 , yago:AmorphousShape113867492 , yago:Location100027167 , yago:WikicatVolcanoes , yago:Vent109470550 , yago:Opening109379111 , yago:Attribute100024264 . @prefix rdfs: . dbr:Volcanic_pipe rdfs:label "Schlot (Geologie)"@de , "\u041A\u0456\u043C\u0431\u0435\u0440\u043B\u0456\u0442\u043E\u0432\u0430 \u0442\u0440\u0443\u0431\u043A\u0430"@uk , "Camino kimberlitico"@it , "Chamin\u00E9 vulc\u00E2nica"@pt , "Xemeneia volc\u00E0nica"@ca , "\u706B\u5C71\u7B52"@zh , "\u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u0432\u0430\u044F \u0442\u0440\u0443\u0431\u043A\u0430"@ru , "\u0623\u0646\u0628\u0648\u0628 \u0628\u0631\u0643\u0627\u0646\u064A"@ar , "\u0397\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC\u03C2 \u03C0\u03CC\u03C1\u03BF\u03C2"@el , "Pipa vulkanik"@in , "Komin wulkaniczny"@pl , "\u706B\u9053"@ja , "Sumendi-tximinia"@eu , "Chimenea volc\u00E1nica"@es , "Volcanic pipe"@en , "Chemin\u00E9e volcanique"@fr ; rdfs:comment "\u041A\u0456\u043C\u0431\u0435\u0440\u043B\u0301\u0456\u0442\u043E\u0432\u0430 \u0442\u0440\u0443\u0431\u043A\u0430 (\u0434\u0456\u0430\u0442\u0440\u0301\u0435\u043C\u0430) \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0430 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0430 \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440\u0430 (\u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0435 \u0442\u0456\u043B\u043E) \u043D\u0435\u043F\u0440\u0430\u0432\u0438\u043B\u044C\u043D\u043E\u0457 \u043A\u043E\u043D\u0443\u0441\u043E\u043F\u043E\u0434\u0456\u0431\u043D\u043E\u0457 \u0430\u0431\u043E \u0446\u0438\u043B\u0456\u043D\u0434\u0440\u0438\u0447\u043D\u043E\u0457 \u0444\u043E\u0440\u043C\u0438 (\u0442\u0440\u0443\u0431\u043A\u0430 \u0432\u0438\u0431\u0443\u0445\u0443), \u0437\u0430\u043F\u043E\u0432\u043D\u0435\u043D\u0430 \u0430\u043B\u043C\u0430\u0437\u043E\u043D\u043E\u0441\u043D\u043E\u044E \u043F\u043E\u0440\u043E\u0434\u043E\u044E (\u043A\u0456\u043C\u0431\u0435\u0440\u043B\u0456\u0442\u043E\u043C \u0447\u0438 \u043B\u0430\u043C\u043F\u0440\u043E\u0457\u0442\u043E\u043C). \u0427\u0438\u0441\u043B\u0435\u043D\u043D\u0456 \u0430\u043B\u043C\u0430\u0437\u043E\u043D\u043E\u0441\u043D\u0456 \u043A\u0456\u043C\u0431\u0435\u0440\u043B\u0456\u0442\u043E\u0432\u0456 \u0442\u0440\u0443\u0431\u043A\u0438 \u0437\u043D\u0430\u0439\u0434\u0435\u043D\u0456 \u0432 \u041F\u0410\u0420 \u0442\u0430 \u042F\u043A\u0443\u0442\u0456\u0457."@uk , "Une chemin\u00E9e volcanique est un conduit \u00E9ruptif cr\u00E9\u00E9 par l'ascension des magmas d'une chambre magmatique jusqu'\u00E0 la surface d'un crat\u00E8re volcanique et par lequel sont \u00E9mis les produits volcaniques (gaz, laves et projections). Le terme conduit volcanique est plus g\u00E9n\u00E9ral car il n'implique pas un d\u00E9bouch\u00E9 sur la surface[r\u00E9f. souhait\u00E9e]. Les recherches sur l'\u00E9tude de la dynamique du magma durant son ascension se multiplient car les processus dans le conduit volcanique gouvernent l'\u00E9volution de l'activit\u00E9 \u00E9ruptive des volcans."@fr , "\u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0647\u064A \u062A\u0634\u0643\u064A\u0644\u0627\u062A \u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629 \u062A\u062D\u062A \u0623\u0631\u0636\u064A\u0629 \u062A\u062A\u0634\u0643\u0644 \u0646\u062A\u064A\u062C\u0629 \u062D\u062F\u0648\u062B \u0647\u064A\u062C\u0627\u0646\u0627\u062A \u0623\u0633\u0631\u0639 \u0645\u0646 \u0627\u0644\u0635\u0648\u062A \u0645\u0646 \u0628\u0631\u0627\u0643\u064A\u0646 \u0639\u0645\u064A\u0642\u0629. \u062A\u062A\u0623\u0644\u0641 \u0647\u0630\u0647 \u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0646 \u0645\u062E\u0631\u0648\u0637 \u0639\u0645\u064A\u0642 \u0648\u0636\u064A\u0642 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 (\u0627\u0644\u0645\u0627\u063A\u0645\u0627) \u0627\u0644\u0645\u062A\u0635\u0644\u0628\u0629\u060C \u0648\u0647\u064A \u0646\u0627\u062F\u0631\u0629 \u0627\u0644\u0648\u062C\u0648\u062F \u0639\u0644\u0649 \u0627\u0644\u0639\u0645\u0648\u0645\u060C \u0648\u062A\u0639\u0631\u0641 \u0628\u0623\u0646\u0647\u0627 \u0623\u062D\u062F \u0627\u0644\u0645\u0643\u0627\u0645\u0646 \u0627\u0644\u0623\u0633\u0627\u0633\u064A\u0629 \u0644\u0644\u0623\u0644\u0645\u0627\u0633. \u063A\u0627\u0644\u0628\u0627\u064B \u0645\u0627 \u062A\u0643\u0648\u0646 \u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0624\u0644\u0641\u0629 \u0645\u0646 \u0646\u0648\u0639 \u0648\u0627\u062D\u062F \u0623\u0648 \u0627\u062B\u0646\u064A\u0646 \u0645\u0646 \u0627\u0644\u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0645\u062B\u0644 \u0627\u0644\u0643\u0645\u0628\u0631\u0644\u064A\u062A \u0648\u0627\u0644\u0644\u0627\u0645\u0628\u0631\u0648\u064A\u062A. \u062A\u0639\u0643\u0633 \u0623\u0646\u0648\u0627\u0639 \u0647\u0630\u0647 \u0627\u0644\u0635\u062E\u0648\u0631 \u062A\u0631\u0643\u064A\u0628 \u0645\u0635\u0627\u062F\u0631 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0627\u0644\u0639\u0645\u064A\u0642\u0629\u060C \u062D\u064A\u062B \u0623\u0646 \u0644\u0628 \u0627\u0644\u0623\u0631\u0636 \u063A\u0646\u064A \u0628\u0641\u0644\u0632 \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645."@ar , "Komin wulkaniczny \u2013 kana\u0142, \u0142\u0105cz\u0105cy komor\u0119 wulkaniczn\u0105 z powierzchni\u0105 ziemi, z kt\u00F3rego produkty wulkaniczne (lawa, gazy, popio\u0142y i inne) wydobywaj\u0105 si\u0119 z g\u0142\u0119bi na powierzchni\u0119 Ziemi. Wylot komina tworzy krater. Je\u015Bli w kominie wulkanicznym zastygnie lawa, to powstaje nek."@pl , "Una chimenea volc\u00E1nica es el conducto por donde sale el magma de los volcanes a la superficie"@es , "Uma chamin\u00E9 vulc\u00E2nica \u00E9 o duto ou canal por onde escapam os gases e o magma que v\u00EAm do interior da c\u00E2mara magm\u00E1tica ou das estruturas do manto, pondo o magma em comunica\u00E7\u00E3o com o exterior. A chamin\u00E9 \u00E9 uma das partes constituintes essenciais do vulc\u00E3o."@pt , "\u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u0432\u0430\u044F \u0442\u0440\u0443\u0431\u043A\u0430 \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u043E\u0435 \u0438\u043B\u0438 \u0431\u043B\u0438\u0437\u043A\u043E\u0435 \u043A \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u043E\u043C\u0443 \u0433\u0435\u043E\u043B\u043E\u0433\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0442\u0435\u043B\u043E, \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u0432\u0448\u0435\u0435\u0441\u044F \u043F\u0440\u0438 \u043F\u0440\u043E\u0440\u044B\u0432\u0435 \u043C\u0430\u0433\u043C\u044B \u0441\u043A\u0432\u043E\u0437\u044C \u0437\u0435\u043C\u043D\u0443\u044E \u043A\u043E\u0440\u0443. \u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u0432\u0430\u044F \u0442\u0440\u0443\u0431\u043A\u0430 \u0437\u0430\u043F\u043E\u043B\u043D\u0435\u043D\u0430 \u043A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u043C. \u0413\u0435\u043E\u043B\u043E\u0433\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440\u0430 \u0438 \u0441\u043E\u043F\u0443\u0442\u0441\u0442\u0432\u0443\u044E\u0449\u0438\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u043D\u0430\u0437\u0432\u0430\u043D\u044B \u043F\u043E \u0438\u043C\u0435\u043D\u0438 \u0433\u043E\u0440\u043E\u0434\u0430 \u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438 \u0432 \u042E\u0436\u043D\u043E\u0439 \u0410\u0444\u0440\u0438\u043A\u0435."@ru , "Una xemeneia volc\u00E0nica \u00E9s el conducte per on surt el magma dels volcans a la superf\u00EDcie."@ca , "Sumendi-tximinia da sumendien magma azalera ateratzen den hodia."@eu , "\u039F \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC\u03C2 \u03C0\u03CC\u03C1\u03BF\u03C2, \u03AE \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC \u03C6\u03C1\u03AD\u03B1\u03C1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C5\u03C0\u03CC\u03B3\u03B5\u03B9\u03B1 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03B4\u03B9\u03AC\u03C4\u03C1\u03B7\u03C3\u03B7, \u03BC\u03AD\u03C3\u03B1 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BF\u03C0\u03BF\u03AF\u03B1 \u03C4\u03BF \u03BC\u03AC\u03B3\u03BC\u03B1 \u03C6\u03B8\u03AC\u03BD\u03B5\u03B9 \u03BC\u03B5 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03B5\u03AF\u03C2 \u03B4\u03B9\u03B5\u03C1\u03B3\u03B1\u03C3\u03AF\u03B5\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03B1 \u03C4\u03BF\u03C5 \u03B3\u03B5\u03C9\u03C6\u03BB\u03BF\u03B9\u03BF\u03CD. \u03A3\u03C4\u03B7\u03BD \u03BF\u03C5\u03C3\u03AF\u03B1 \u03C0\u03C1\u03CC\u03BA\u03B5\u03B9\u03C4\u03B1\u03B9 \u03B3\u03B9\u03B1 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03AE \u03B4\u03BF\u03BC\u03AE \u03BF\u03C7\u03B5\u03C4\u03BF\u03CD \u03B4\u03B9\u03B1\u03C6\u03C5\u03B3\u03AE\u03C2 \u03B1\u03B5\u03C1\u03AF\u03C9\u03BD \u03BA\u03B1\u03B9 \u03BC\u03B1\u03B3\u03BC\u03B1\u03C4\u03B9\u03BA\u03AE\u03C2 \u03BC\u03AC\u03B6\u03B1\u03C2 \u03BB\u03CC\u03B3\u03C9 \u03C5\u03C0\u03B5\u03C1\u03B2\u03BF\u03BB\u03B9\u03BA\u03AE\u03C2 \u03C0\u03AF\u03B5\u03C3\u03B7\u03C2. \u039F \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC\u03C2 \u03C0\u03CC\u03C1\u03BF\u03C2 \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF \u03C4\u03BF\u03BD \u03BA\u03B5\u03BD\u03C4\u03C1\u03B9\u03BA\u03CC \u03AC\u03BE\u03BF\u03BD\u03B1 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03B9\u03C3\u03BC\u03BF\u03CD \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03AF\u03BF\u03C5 \u03BA\u03B1\u03B9 \u03C4\u03BF \u03B2\u03B1\u03C3\u03B9\u03BA\u03CC\u03C4\u03B5\u03C1\u03BF \u03BC\u03AD\u03C1\u03BF\u03C2 \u03B1\u03C5\u03C4\u03BF\u03CD."@el , "Als Schlot (auch Schlotgang, Vulkanschlot, Durchschlagsr\u00F6hre, Sprengtrichter, Diatrema, Neck oder Eruptionsschlot) bezeichnet man in der Geologie den mehr oder weniger senkrechten Aufstiegskanal von vulkanischen Produkten aus dem Erdinneren zu einem Eruptionszentrum an der Erdoberfl\u00E4che oder am Meeresboden."@de , "\u706B\u9053\uFF08\u304B\u3069\u3046\u3001volcanic vent\uFF09\u306F\u30DE\u30B0\u30DE\u304C\u5730\u4E2D\u306B\u8CAB\u5165\u3059\u308B\u3068\u304D\u306E\u901A\u308A\u9053\u306E\u3053\u3068\u3002"@ja , "\u706B\u5C71\u7B52\uFF08\u82F1\u8A9E\uFF1AVolcanic pipe\uFF09\uFF0C\u662F\u7531\u6DF1\u5C64\u706B\u5C71\u56E0\u8D85\u97F3\u901F\u7206\u767C\u6240\u5F62\u6210\u7684\u5730\u4E0B\u5730\u8CEA\u69CB\u9020\u3002\u706B\u5C71\u7B52\u88AB\u8A8D\u70BA\u662F\u4E00\u7A2E\u706B\u5C71\u9053\uFF0C\u7531\u51DD\u56FA\u5CA9\u6F3F\u5F62\u6210\u7684\u6DF1\u800C\u7A84\u7684\u9310\u9AD4\uFF08\u5916\u578B\u70BA\u80E1\u863F\u8514\u5F62\uFF09\uFF0C\u901A\u5E38\u7531\u5169\u7A2E\u7279\u8272\u7684\u5CA9\u77F3\u6240\u7D44\u6210\u7684\u2014\u2014\u91D1\u4F2F\u5229\u5CA9\u6216\u9240\u9382\u714C\u6591\u5CA9\u3002 \u9019\u4E9B\u5CA9\u77F3\u53CD\u6620\u4E86\u706B\u5C71\u6DF1\u90E8\u5CA9\u6F3F\u6E90\u7684\u7D44\u6210\uFF0C\u5730\u7403\u4E0A\u5BCC\u542B\u4E86\u9382\uFF0C\u4F46\u706B\u5C71\u7B52\u76F8\u5C0D\u8F03\u5C11\u3002\u5B83\u5011\u662F\u773E\u6240\u5468\u77E5\u7684\u947D\u77F3\u7684\u4E3B\u8981\u4F86\u6E90\uFF0C\u5E38\u70BA\u6B64\u88AB\u958B\u63A1\u3002"@zh , "Un camino kimberlitico (detta anche diatrema) \u00E8 una particolare formazione geologica, frutto di un particolare tipo di eruzione, che ha avuto luogo in varie parti del pianeta. Queste regioni dette cratoni sono resti del primordiale supercontinente e non hanno subito alterazioni da oltre 500 milioni di anni. Oggi sono presenti in Australia, Siberia, Canada, Africa australe e occidentale e - secondo alcune teorie - anche il presunto neck di Motta Sant'Anastasia sarebbe piuttosto un diatrema. Questo evento non si \u00E8 mai verificato in epoca storica, quindi quanto si suppone \u00E8 solo il frutto di valutazioni fatte su quanto le cicatrici della terra hanno lasciato. Nei camini kimberlitici si trovano i giacimenti primari di diamanti."@it , "Pipa vulkanik adalah struktur geologis bawah tanah yang dibentuk oleh letusan supersonik gunung berapi. Pipa vulkanik dipandang sebagai jenis dari diatrema. Pipa vulkanik tersusun atas magma beku yang membentuk kerucut kurus yang dalam (disebut sebagai \"berbentuk wortel\"), dan biasanya terdiri dari satu atau dua jenis batuan karakteristik, yakni kimberlit atau lamproit. Batuan ini mencerminkan komposisi sumber magma di bawah gunung berapi, di mana Bumi kaya akan magnesium. Pipa vulkanik relatif langka. Pipa vulkanik dikenal baik sebagai sumber intan utama, dan ditambang untuk memperoleh intan."@in , "Volcanic pipes or volcanic conduits are subterranean geological structures formed by the violent, supersonic eruption of deep-origin volcanoes. They are considered to be a type of diatreme. Volcanic pipes are composed of a deep, narrow cone of solidified magma (described as \"carrot-shaped\"), and are usually largely composed of one of two characteristic rock types \u2014 kimberlite or lamproite. These rocks reflect the composition of the volcanoes' deep magma sources, where the Earth is rich in magnesium. Volcanic pipes are relatively rare. They are well known as the primary source of diamonds, and are mined for this purpose."@en . @prefix foaf: . dbr:Volcanic_pipe foaf:depiction , . @prefix dct: . @prefix dbc: . dbr:Volcanic_pipe dct:subject dbc:Diatremes ; dbo:abstract "Una chimenea volc\u00E1nica es el conducto por donde sale el magma de los volcanes a la superficie"@es , "\u039F \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC\u03C2 \u03C0\u03CC\u03C1\u03BF\u03C2, \u03AE \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC \u03C6\u03C1\u03AD\u03B1\u03C1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C5\u03C0\u03CC\u03B3\u03B5\u03B9\u03B1 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03B4\u03B9\u03AC\u03C4\u03C1\u03B7\u03C3\u03B7, \u03BC\u03AD\u03C3\u03B1 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BF\u03C0\u03BF\u03AF\u03B1 \u03C4\u03BF \u03BC\u03AC\u03B3\u03BC\u03B1 \u03C6\u03B8\u03AC\u03BD\u03B5\u03B9 \u03BC\u03B5 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03B5\u03AF\u03C2 \u03B4\u03B9\u03B5\u03C1\u03B3\u03B1\u03C3\u03AF\u03B5\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03B1 \u03C4\u03BF\u03C5 \u03B3\u03B5\u03C9\u03C6\u03BB\u03BF\u03B9\u03BF\u03CD. \u03A3\u03C4\u03B7\u03BD \u03BF\u03C5\u03C3\u03AF\u03B1 \u03C0\u03C1\u03CC\u03BA\u03B5\u03B9\u03C4\u03B1\u03B9 \u03B3\u03B9\u03B1 \u03B5\u03BA\u03C1\u03B7\u03BE\u03B9\u03B3\u03B5\u03BD\u03AE \u03B4\u03BF\u03BC\u03AE \u03BF\u03C7\u03B5\u03C4\u03BF\u03CD \u03B4\u03B9\u03B1\u03C6\u03C5\u03B3\u03AE\u03C2 \u03B1\u03B5\u03C1\u03AF\u03C9\u03BD \u03BA\u03B1\u03B9 \u03BC\u03B1\u03B3\u03BC\u03B1\u03C4\u03B9\u03BA\u03AE\u03C2 \u03BC\u03AC\u03B6\u03B1\u03C2 \u03BB\u03CC\u03B3\u03C9 \u03C5\u03C0\u03B5\u03C1\u03B2\u03BF\u03BB\u03B9\u03BA\u03AE\u03C2 \u03C0\u03AF\u03B5\u03C3\u03B7\u03C2. \u039F \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03B9\u03B1\u03BA\u03CC\u03C2 \u03C0\u03CC\u03C1\u03BF\u03C2 \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03B5\u03AF \u03C4\u03BF\u03BD \u03BA\u03B5\u03BD\u03C4\u03C1\u03B9\u03BA\u03CC \u03AC\u03BE\u03BF\u03BD\u03B1 \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03B9\u03C3\u03BC\u03BF\u03CD \u03B7\u03C6\u03B1\u03B9\u03C3\u03C4\u03B5\u03AF\u03BF\u03C5 \u03BA\u03B1\u03B9 \u03C4\u03BF \u03B2\u03B1\u03C3\u03B9\u03BA\u03CC\u03C4\u03B5\u03C1\u03BF \u03BC\u03AD\u03C1\u03BF\u03C2 \u03B1\u03C5\u03C4\u03BF\u03CD."@el , "Una xemeneia volc\u00E0nica \u00E9s el conducte per on surt el magma dels volcans a la superf\u00EDcie."@ca , "\u706B\u5C71\u7B52\uFF08\u82F1\u8A9E\uFF1AVolcanic pipe\uFF09\uFF0C\u662F\u7531\u6DF1\u5C64\u706B\u5C71\u56E0\u8D85\u97F3\u901F\u7206\u767C\u6240\u5F62\u6210\u7684\u5730\u4E0B\u5730\u8CEA\u69CB\u9020\u3002\u706B\u5C71\u7B52\u88AB\u8A8D\u70BA\u662F\u4E00\u7A2E\u706B\u5C71\u9053\uFF0C\u7531\u51DD\u56FA\u5CA9\u6F3F\u5F62\u6210\u7684\u6DF1\u800C\u7A84\u7684\u9310\u9AD4\uFF08\u5916\u578B\u70BA\u80E1\u863F\u8514\u5F62\uFF09\uFF0C\u901A\u5E38\u7531\u5169\u7A2E\u7279\u8272\u7684\u5CA9\u77F3\u6240\u7D44\u6210\u7684\u2014\u2014\u91D1\u4F2F\u5229\u5CA9\u6216\u9240\u9382\u714C\u6591\u5CA9\u3002 \u9019\u4E9B\u5CA9\u77F3\u53CD\u6620\u4E86\u706B\u5C71\u6DF1\u90E8\u5CA9\u6F3F\u6E90\u7684\u7D44\u6210\uFF0C\u5730\u7403\u4E0A\u5BCC\u542B\u4E86\u9382\uFF0C\u4F46\u706B\u5C71\u7B52\u76F8\u5C0D\u8F03\u5C11\u3002\u5B83\u5011\u662F\u773E\u6240\u5468\u77E5\u7684\u947D\u77F3\u7684\u4E3B\u8981\u4F86\u6E90\uFF0C\u5E38\u70BA\u6B64\u88AB\u958B\u63A1\u3002"@zh , "Pipa vulkanik adalah struktur geologis bawah tanah yang dibentuk oleh letusan supersonik gunung berapi. Pipa vulkanik dipandang sebagai jenis dari diatrema. Pipa vulkanik tersusun atas magma beku yang membentuk kerucut kurus yang dalam (disebut sebagai \"berbentuk wortel\"), dan biasanya terdiri dari satu atau dua jenis batuan karakteristik, yakni kimberlit atau lamproit. Batuan ini mencerminkan komposisi sumber magma di bawah gunung berapi, di mana Bumi kaya akan magnesium. Pipa vulkanik relatif langka. Pipa vulkanik dikenal baik sebagai sumber intan utama, dan ditambang untuk memperoleh intan."@in , "\u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0647\u064A \u062A\u0634\u0643\u064A\u0644\u0627\u062A \u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629 \u062A\u062D\u062A \u0623\u0631\u0636\u064A\u0629 \u062A\u062A\u0634\u0643\u0644 \u0646\u062A\u064A\u062C\u0629 \u062D\u062F\u0648\u062B \u0647\u064A\u062C\u0627\u0646\u0627\u062A \u0623\u0633\u0631\u0639 \u0645\u0646 \u0627\u0644\u0635\u0648\u062A \u0645\u0646 \u0628\u0631\u0627\u0643\u064A\u0646 \u0639\u0645\u064A\u0642\u0629. \u062A\u062A\u0623\u0644\u0641 \u0647\u0630\u0647 \u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0646 \u0645\u062E\u0631\u0648\u0637 \u0639\u0645\u064A\u0642 \u0648\u0636\u064A\u0642 \u0645\u0646 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 (\u0627\u0644\u0645\u0627\u063A\u0645\u0627) \u0627\u0644\u0645\u062A\u0635\u0644\u0628\u0629\u060C \u0648\u0647\u064A \u0646\u0627\u062F\u0631\u0629 \u0627\u0644\u0648\u062C\u0648\u062F \u0639\u0644\u0649 \u0627\u0644\u0639\u0645\u0648\u0645\u060C \u0648\u062A\u0639\u0631\u0641 \u0628\u0623\u0646\u0647\u0627 \u0623\u062D\u062F \u0627\u0644\u0645\u0643\u0627\u0645\u0646 \u0627\u0644\u0623\u0633\u0627\u0633\u064A\u0629 \u0644\u0644\u0623\u0644\u0645\u0627\u0633. \u063A\u0627\u0644\u0628\u0627\u064B \u0645\u0627 \u062A\u0643\u0648\u0646 \u0627\u0644\u0623\u0646\u0627\u0628\u064A\u0628 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u0629 \u0645\u0624\u0644\u0641\u0629 \u0645\u0646 \u0646\u0648\u0639 \u0648\u0627\u062D\u062F \u0623\u0648 \u0627\u062B\u0646\u064A\u0646 \u0645\u0646 \u0627\u0644\u0623\u0646\u0648\u0627\u0639 \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0645\u062B\u0644 \u0627\u0644\u0643\u0645\u0628\u0631\u0644\u064A\u062A \u0648\u0627\u0644\u0644\u0627\u0645\u0628\u0631\u0648\u064A\u062A. \u062A\u0639\u0643\u0633 \u0623\u0646\u0648\u0627\u0639 \u0647\u0630\u0647 \u0627\u0644\u0635\u062E\u0648\u0631 \u062A\u0631\u0643\u064A\u0628 \u0645\u0635\u0627\u062F\u0631 \u0627\u0644\u0635\u0647\u0627\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0627\u0644\u0639\u0645\u064A\u0642\u0629\u060C \u062D\u064A\u062B \u0623\u0646 \u0644\u0628 \u0627\u0644\u0623\u0631\u0636 \u063A\u0646\u064A \u0628\u0641\u0644\u0632 \u0627\u0644\u0645\u063A\u0646\u0633\u064A\u0648\u0645."@ar , "Une chemin\u00E9e volcanique est un conduit \u00E9ruptif cr\u00E9\u00E9 par l'ascension des magmas d'une chambre magmatique jusqu'\u00E0 la surface d'un crat\u00E8re volcanique et par lequel sont \u00E9mis les produits volcaniques (gaz, laves et projections). Le terme conduit volcanique est plus g\u00E9n\u00E9ral car il n'implique pas un d\u00E9bouch\u00E9 sur la surface[r\u00E9f. souhait\u00E9e]. Les recherches sur l'\u00E9tude de la dynamique du magma durant son ascension se multiplient car les processus dans le conduit volcanique gouvernent l'\u00E9volution de l'activit\u00E9 \u00E9ruptive des volcans."@fr , "Un camino kimberlitico (detta anche diatrema) \u00E8 una particolare formazione geologica, frutto di un particolare tipo di eruzione, che ha avuto luogo in varie parti del pianeta. Queste regioni dette cratoni sono resti del primordiale supercontinente e non hanno subito alterazioni da oltre 500 milioni di anni. Oggi sono presenti in Australia, Siberia, Canada, Africa australe e occidentale e - secondo alcune teorie - anche il presunto neck di Motta Sant'Anastasia sarebbe piuttosto un diatrema. Questo evento non si \u00E8 mai verificato in epoca storica, quindi quanto si suppone \u00E8 solo il frutto di valutazioni fatte su quanto le cicatrici della terra hanno lasciato. Nei camini kimberlitici si trovano i giacimenti primari di diamanti."@it , "Als Schlot (auch Schlotgang, Vulkanschlot, Durchschlagsr\u00F6hre, Sprengtrichter, Diatrema, Neck oder Eruptionsschlot) bezeichnet man in der Geologie den mehr oder weniger senkrechten Aufstiegskanal von vulkanischen Produkten aus dem Erdinneren zu einem Eruptionszentrum an der Erdoberfl\u00E4che oder am Meeresboden."@de , "Volcanic pipes or volcanic conduits are subterranean geological structures formed by the violent, supersonic eruption of deep-origin volcanoes. They are considered to be a type of diatreme. Volcanic pipes are composed of a deep, narrow cone of solidified magma (described as \"carrot-shaped\"), and are usually largely composed of one of two characteristic rock types \u2014 kimberlite or lamproite. These rocks reflect the composition of the volcanoes' deep magma sources, where the Earth is rich in magnesium. Volcanic pipes are relatively rare. They are well known as the primary source of diamonds, and are mined for this purpose."@en , "\u706B\u9053\uFF08\u304B\u3069\u3046\u3001volcanic vent\uFF09\u306F\u30DE\u30B0\u30DE\u304C\u5730\u4E2D\u306B\u8CAB\u5165\u3059\u308B\u3068\u304D\u306E\u901A\u308A\u9053\u306E\u3053\u3068\u3002"@ja , "Uma chamin\u00E9 vulc\u00E2nica \u00E9 o duto ou canal por onde escapam os gases e o magma que v\u00EAm do interior da c\u00E2mara magm\u00E1tica ou das estruturas do manto, pondo o magma em comunica\u00E7\u00E3o com o exterior. A chamin\u00E9 \u00E9 uma das partes constituintes essenciais do vulc\u00E3o."@pt , "\u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u0432\u0430\u044F \u0442\u0440\u0443\u0431\u043A\u0430 \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u043E\u0435 \u0438\u043B\u0438 \u0431\u043B\u0438\u0437\u043A\u043E\u0435 \u043A \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u043E\u043C\u0443 \u0433\u0435\u043E\u043B\u043E\u0433\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0442\u0435\u043B\u043E, \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u0432\u0448\u0435\u0435\u0441\u044F \u043F\u0440\u0438 \u043F\u0440\u043E\u0440\u044B\u0432\u0435 \u043C\u0430\u0433\u043C\u044B \u0441\u043A\u0432\u043E\u0437\u044C \u0437\u0435\u043C\u043D\u0443\u044E \u043A\u043E\u0440\u0443. \u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u0432\u0430\u044F \u0442\u0440\u0443\u0431\u043A\u0430 \u0437\u0430\u043F\u043E\u043B\u043D\u0435\u043D\u0430 \u043A\u0438\u043C\u0431\u0435\u0440\u043B\u0438\u0442\u043E\u043C. \u0413\u0435\u043E\u043B\u043E\u0433\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440\u0430 \u0438 \u0441\u043E\u043F\u0443\u0442\u0441\u0442\u0432\u0443\u044E\u0449\u0438\u0435 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u043D\u0430\u0437\u0432\u0430\u043D\u044B \u043F\u043E \u0438\u043C\u0435\u043D\u0438 \u0433\u043E\u0440\u043E\u0434\u0430 \u041A\u0438\u043C\u0431\u0435\u0440\u043B\u0438 \u0432 \u042E\u0436\u043D\u043E\u0439 \u0410\u0444\u0440\u0438\u043A\u0435."@ru , "\u041A\u0456\u043C\u0431\u0435\u0440\u043B\u0301\u0456\u0442\u043E\u0432\u0430 \u0442\u0440\u0443\u0431\u043A\u0430 (\u0434\u0456\u0430\u0442\u0440\u0301\u0435\u043C\u0430) \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0430 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0430 \u0441\u0442\u0440\u0443\u043A\u0442\u0443\u0440\u0430 (\u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0435 \u0442\u0456\u043B\u043E) \u043D\u0435\u043F\u0440\u0430\u0432\u0438\u043B\u044C\u043D\u043E\u0457 \u043A\u043E\u043D\u0443\u0441\u043E\u043F\u043E\u0434\u0456\u0431\u043D\u043E\u0457 \u0430\u0431\u043E \u0446\u0438\u043B\u0456\u043D\u0434\u0440\u0438\u0447\u043D\u043E\u0457 \u0444\u043E\u0440\u043C\u0438 (\u0442\u0440\u0443\u0431\u043A\u0430 \u0432\u0438\u0431\u0443\u0445\u0443), \u0437\u0430\u043F\u043E\u0432\u043D\u0435\u043D\u0430 \u0430\u043B\u043C\u0430\u0437\u043E\u043D\u043E\u0441\u043D\u043E\u044E \u043F\u043E\u0440\u043E\u0434\u043E\u044E (\u043A\u0456\u043C\u0431\u0435\u0440\u043B\u0456\u0442\u043E\u043C \u0447\u0438 \u043B\u0430\u043C\u043F\u0440\u043E\u0457\u0442\u043E\u043C). \u0427\u0438\u0441\u043B\u0435\u043D\u043D\u0456 \u0430\u043B\u043C\u0430\u0437\u043E\u043D\u043E\u0441\u043D\u0456 \u043A\u0456\u043C\u0431\u0435\u0440\u043B\u0456\u0442\u043E\u0432\u0456 \u0442\u0440\u0443\u0431\u043A\u0438 \u0437\u043D\u0430\u0439\u0434\u0435\u043D\u0456 \u0432 \u041F\u0410\u0420 \u0442\u0430 \u042F\u043A\u0443\u0442\u0456\u0457."@uk , "Komin wulkaniczny \u2013 kana\u0142, \u0142\u0105cz\u0105cy komor\u0119 wulkaniczn\u0105 z powierzchni\u0105 ziemi, z kt\u00F3rego produkty wulkaniczne (lawa, gazy, popio\u0142y i inne) wydobywaj\u0105 si\u0119 z g\u0142\u0119bi na powierzchni\u0119 Ziemi. Wylot komina tworzy krater. Je\u015Bli w kominie wulkanicznym zastygnie lawa, to powstaje nek."@pl , "Sumendi-tximinia da sumendien magma azalera ateratzen den hodia."@eu ; dbo:wikiPageWikiLink dbc:Diatremes , dbr:Water , , dbr:Phase_transformation , dbr:Gemstone , dbr:Garnet , dbr:Carbon_dioxide , dbr:Diamond , dbr:Supersonic , dbr:Lamproite , dbr:Diatreme , dbr:Magma , dbr:Plinian_eruption , dbr:Magnesium , dbr:Volcano , dbr:Ejecta , dbr:Tuff_ring , dbr:Spinel , dbr:Geology , dbr:Peridot , dbr:Kimberlite , dbr:Pressure , dbr:Gas , , dbr:Volatiles , dbr:Corrosion . @prefix dbt: . dbr:Volcanic_pipe dbp:wikiPageUsesTemplate dbt:Reflist , dbt:Short_description , dbt:Convert , dbt:Authority_control , dbt:Annotated_link , dbt:Subterranea ; dbo:thumbnail ; dbo:wikiPageRevisionID 1104625077 ; dbo:wikiPageExternalLink , , . @prefix xsd: . dbr:Volcanic_pipe dbo:wikiPageLength "3985"^^xsd:nonNegativeInteger ; dbo:wikiPageID 1615558 . @prefix dbpedia-eu: . dbr:Volcanic_pipe owl:sameAs dbpedia-eu:Sumendi-tximinia , , , , , , , , , . @prefix dbpedia-id: . dbr:Volcanic_pipe owl:sameAs dbpedia-id:Pipa_vulkanik , , , , , , , dbr:Volcanic_pipe , . @prefix wikidata: . dbr:Volcanic_pipe owl:sameAs wikidata:Q2261752 . @prefix yago-res: . dbr:Volcanic_pipe owl:sameAs yago-res:Volcanic_pipe . @prefix dbpedia-pl: . dbr:Volcanic_pipe owl:sameAs dbpedia-pl:Komin_wulkaniczny , , . @prefix dbpedia-it: . dbr:Volcanic_pipe owl:sameAs dbpedia-it:Camino_kimberlitico , , . @prefix gold: . dbr:Volcanic_pipe gold:hypernym dbr:Structures . @prefix prov: . dbr:Volcanic_pipe prov:wasDerivedFrom . @prefix wikipedia-en: . dbr:Volcanic_pipe foaf:isPrimaryTopicOf wikipedia-en:Volcanic_pipe . dbr:Wolfgang_Kundt dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Murowa_diamond_mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Forest_ring dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Mountain_Lake_cluster dbo:wikiPageWikiLink dbr:Volcanic_pipe . wikipedia-en:Volcanic_pipe foaf:primaryTopic dbr:Volcanic_pipe . dbr:Kimberlite_pipes dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageRedirects dbr:Volcanic_pipe . dbr:Solignat dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Kranstein dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Batholith dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Monte_Camulera dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Intrusive_rock dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Carrick-a-Rede_Rope_Bridge dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Alrosa dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Lesedi_La_Rona dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Rockeskyller_Kopf dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Weiselberg dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:type dbr:Volcanic_pipe ; dbp:type dbr:Volcanic_pipe . dbr:Jusi dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Lamproite dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:El_Teniente dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Mining_industry_of_Lesotho dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Oslo_Graben dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Aykhal dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Steep_coast dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Golconda_diamonds_mining_and_trading dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Oppidum_Steinsburg dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Great_Lakes dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Baba_Diamond_Fields dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Udachnaya_pipe dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Callander_Bay dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Ottawa-Bonnechere_Graben dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Premier_Mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Diavik_Diamond_Mine dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Kimberlite_pipe dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageRedirects dbr:Volcanic_pipe . dbr:Diatreme dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Erkenbrechtsweiler dbo:wikiPageWikiLink dbr:Volcanic_pipe . dbr:Supersonic_eruption dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageRedirects dbr:Volcanic_pipe . dbr:Kimberlite_bloom dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageRedirects dbr:Volcanic_pipe . dbr:Kimberlite_eruption dbo:wikiPageWikiLink dbr:Volcanic_pipe ; dbo:wikiPageRedirects dbr:Volcanic_pipe .
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