. . "Ignimbrito"@pt . . . . . . "\u0406\u0433\u043D\u0456\u043C\u0431\u0440\u0438\u0442 \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0456\u0447\u043D\u0430 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430, \u044F\u043A\u0430 \u043C\u0430\u0454 \u043E\u0437\u043D\u0430\u043A\u0438 \u044F\u043A \u043B\u0430\u0432, \u0442\u0430\u043A \u0456 \u043F\u0456\u0440\u043E\u043A\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u0438\u0445 \u0443\u0442\u0432\u043E\u0440\u0435\u043D\u044C. \u041C\u0430\u0454 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0443 \u0431\u0443\u0434\u043E\u0432\u0443 \u0456 \u0441\u043A\u043B\u0430\u0434\u0430\u0454\u0442\u044C\u0441\u044F \u043F\u0435\u0440\u0435\u0432. \u0437 \u0434\u0440\u0456\u0431\u043D\u0438\u0445 \u0447\u0430\u0441\u0442\u0438\u043D\u043E\u043A \u0432\u0443\u043B\u043A\u0430\u043D\u0456\u0447\u043D\u043E\u0433\u043E \u0441\u043A\u043B\u0430, \u0443\u043B\u0430\u043C\u043A\u0456\u0432 \u043F\u0435\u043C\u0437\u0438 \u0456 \u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0456\u0432. \u0427\u0430\u0441\u0442\u0438\u043D\u043A\u0438 \u043F\u043E\u043F\u0435\u043B\u0443 \u043F\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u043E \u0434\u0435\u0444\u043E\u0440\u043C\u043E\u0432\u0430\u043D\u0456 \u0456, \u0449\u0456\u043B\u044C\u043D\u043E \u043F\u0440\u0438\u043B\u044F\u0433\u0430\u044E\u0447\u0438 \u043E\u0434\u0438\u043D \u0434\u043E \u043E\u0434\u043D\u043E\u0433\u043E, \u0437\u043B\u0438\u0432\u0430\u044E\u0442\u044C\u0441\u044F \u0449\u0435 \u0432 \u0440\u043E\u0437\u043F\u043B\u0430\u0432\u043B\u0435\u043D\u043E\u043C\u0443 \u0441\u0442\u0430\u043D\u0456. \u0412\u043E\u043D\u0438 \u0434\u043E\u0432\u0433\u0430\u0441\u0442\u0456, \u0440\u043E\u0437\u0442\u0430\u0448\u043E\u0432\u0430\u043D\u0456 \u043F\u0430\u0440\u0430\u043B\u0435\u043B\u044C\u043D\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456 \u0439 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C \u043F\u0435\u0440\u0435\u0440\u0432\u043D\u043E\u043B\u0456\u043D\u0456\u0439\u043D\u0443 (\u0430\u0431\u043E \u0435\u0432\u0442\u0430\u043A\u0441\u0438\u0442\u043E\u0432\u0443) \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u0443, \u0449\u043E \u043D\u0430\u0433\u0430\u0434\u0443\u0454 \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u0443 \u0442\u0435\u0447\u0456\u0457 \u0432 \u043B\u0430\u0432\u0430\u0445. \u0423 \u0447\u0430\u0441\u0442\u043A\u043E\u0432\u043E \u0433\u043E\u043C\u043E-\u0433\u0435\u043D\u0456\u0437\u043E\u0432\u0430\u043D\u0456\u0439 \u043C\u0430\u0441\u0456 \u043F\u043E\u043F\u0435\u043B\u0443 \u0440\u043E\u0437\u0441\u0456\u044F\u043D\u0456 \u0444\u0435\u043D\u043E\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0438 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u0456 \u0443\u043B\u0430\u043C\u043A\u0438 \u043F\u0435\u043C\u0437\u0438, \u0441\u043F\u043B\u044E\u0441\u043D\u0443\u0442\u0456 \u0437\u0433\u0456\u0434\u043D\u043E \u0437 \u0437\u0430\u0433\u0430\u043B\u044C\u043D\u043E\u044E \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u043E\u044E \u0456 \u043F\u0435\u0440\u0435\u0442\u0432\u043E\u0440\u0435\u043D\u0456 \u0432 \u0449\u0456\u043B\u044C\u043D\u0456 \u0441\u043A\u043B\u0443\u0432\u0430\u0442\u0456 \u0434\u0438\u0441\u043A\u0438 \u0437 \u0445\u0430\u0440\u0430-\u043A\u0442\u0435\u0440\u043D\u0438\u043C\u0438 \u043F\u043E\u043B\u0443\u043C'\u044F\u0432\u0438\u0434\u043D\u0438\u043C\u0438 \u0433\u0440\u0430\u043D\u0438\u0446\u044F\u043C\u0438 (\u0444'\u044F\u043C\u043C\u0435 \u2014 \u0432\u0456\u0434 \u0456\u0442\u0430\u043B. Fiamma \u2014 \u043F\u043E\u043B\u0443\u043C'\u044F). \u0417\u0430 \u0441\u043A\u043B\u0430\u0434\u043E\u043C \u0440\u043E\u0437\u0440\u0456\u0437\u043D\u044F\u044E\u0442\u044C \u0406.: \u0440\u0456\u043E\u043B\u0456\u0442\u043E\u0432\u0456, \u0434\u0430\u0446\u0438\u0442\u043E\u0432\u0456, \u0442\u0440\u0430\u0445\u0456\u0442\u043E\u0432\u0456, \u0440\u0456\u0434\u0448\u0435 \u2014 \u0430\u043D\u0434\u0435\u0437\u0438\u0442\u043E\u0432\u0456. \u0406. \u2014 \u043F\u0440\u043E\u0434\u0443\u043A\u0442\u0438 \u0432\u0438\u0441\u043E\u043A\u043E\u0440\u0443\u0445\u043B\u0438\u0432\u0438\u0445 \u043F\u043E\u043F\u0435\u043B\u043E\u0432\u0438\u0445 \u043F\u043E\u0442\u043E\u043A\u0456\u0432, \u043F\u043E\u0432'\u044F\u0437\u0430\u043D\u0438\u0445 \u0437 \u0432\u0438\u0432\u0435\u0440\u0436\u0435\u043D\u043D\u044F\u043C\u0438 \u043A\u0430\u0442\u043C\u0430\u0439\u0441\u044C\u043A\u043E\u0433\u043E \u0442\u0438\u043F\u0443. \u0412\u0438\u043A\u043E\u0440\u0438\u0441\u0442\u043E\u0432\u0443\u044E\u0442\u044C\u0441\u044F \u044F\u043A \u0431\u0443\u0434. \u043A\u0430\u043C\u0456\u043D\u044C."@uk . . . . "Ignimbrit"@in . "Ignimbrite"@it . . "Ignimbrit"@cs . "\u0418\u0433\u043D\u0438\u043C\u0431\u0440\u0438\u0442 (\u043E\u0442 \u043B\u0430\u0442. ignis \u2014 \u043E\u0433\u043E\u043D\u044C) \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0431\u043B\u043E\u043C\u043E\u0447\u043D\u0430\u044F \u0433\u043E\u0440\u043D\u0430\u044F \u043F\u043E\u0440\u043E\u0434\u0430. \u0418\u0433\u043D\u0438\u043C\u0431\u0440\u0438\u0442\u044B \u2014 \u043F\u0440\u043E\u0434\u0443\u043A\u0442\u044B \u0432\u044B\u0441\u043E\u043A\u043E\u043F\u043E\u0434\u0432\u0438\u0436\u043D\u044B\u0445 \u043F\u0435\u043F\u043B\u043E\u0432\u044B\u0445 \u043F\u043E\u0442\u043E\u043A\u043E\u0432, \u0441\u0432\u044F\u0437\u0430\u043D\u043D\u044B\u0445 \u0441 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u044F\u043C\u0438 \u043A\u0430\u0442\u043C\u0430\u0439\u0441\u043A\u043E\u0433\u043E \u0442\u0438\u043F\u0430. \u0425\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u044E\u0442\u0441\u044F \u0431\u043E\u043B\u044C\u0448\u0438\u043C\u0438 \u043E\u0431\u044A\u0451\u043C\u0430\u043C\u0438 \u0440\u0430\u0437\u043E\u0432\u044B\u0445 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u0439 (\u0434\u043E \u0434\u0435\u0441\u044F\u0442\u043A\u043E\u0432 \u043A\u043C\u00B3 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u043C\u0430\u0442\u0435\u0440\u0438\u0430\u043B\u0430). \u0412 \u0432\u0438\u0434\u0435 \u0441\u0435\u0440\u0438\u0439 \u0438\u0437 \u043F\u0435\u0440\u0432\u0438\u0447\u043D\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E \u0437\u0430\u043B\u0435\u0433\u0430\u044E\u0449\u0438\u0445 \u043F\u043E\u043A\u0440\u043E\u0432\u043E\u0432 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0435\u043D\u044B \u043D\u0430 \u043E\u0431\u0448\u0438\u0440\u043D\u044B\u0445 \u043F\u043B\u043E\u0449\u0430\u0434\u044F\u0445 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u043F\u043E\u044F\u0441\u043E\u0432 \u0430\u043A\u0442\u0438\u0432\u043D\u044B\u0445 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u044B\u0445 \u043E\u043A\u0440\u0430\u0438\u043D, \u0437\u0440\u0435\u043B\u044B\u0445 \u043E\u0441\u0442\u0440\u043E\u0432\u043D\u044B\u0445 \u0434\u0443\u0433 \u0438 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u044B\u0445 \u0440\u0438\u0444\u0442\u043E\u0432."@ru . . . "Igninbrita pikor ez kontsolidatuz osatutako arroka igneo bat da, errautsaz sorturikoa, fluxu piroklastikoetan sortzen dena. Orokorrean dazita edo erriolitaren konposaketa bera izaten dute. Igninbrita batez ere tefra matrizez osatua dago, eta sumendi beiraz osatua. Pumita eta kristal zatiak ere daude osaeran. Erautsa matrizearen barnean, batzuetan legar tamainako arroka zatiak daude, xenolitoak edo inklusioak."@eu . . . . . . "\u0406\u0433\u043D\u0456\u043C\u0431\u0440\u0438\u0442"@uk . . . . . "Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ignimbrite from the Latin igni- [fire] and imbri- [rain]. Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli-tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and density. Many pale ignimbrites are dacitic or rhyolitic. Darker-coloured ignimbrites may be densely welded volcanic glass or, less commonly, mafic in composition."@en . "\u0418\u0433\u043D\u0438\u043C\u0431\u0440\u0438\u0442"@ru . "La ignimbrita \u00E9s un tipus de roca volc\u00E0nica, \u00E0cida i compacta, amb grau de cristal\u00B7litzaci\u00F3 holov\u00EDtria. En els dip\u00F2sits d'ignimbrites s'observa amb freq\u00FC\u00E8ncia la pres\u00E8ncia de fragments d'obsidiana, m\u00E9s o menys alterats i aixafats, de forma allargada que es denominen flames. Es troba a extenses colades produ\u00EFdes per l'efusi\u00F3 de la lava no ja per un cr\u00E0ter volc\u00E0nic, sin\u00F3 per llargues fissures del terreny volc\u00E0nic. Consisteixen en una toba formada per cendres i part\u00EDcules de silicats procedents de l'escuma de laves viscoses produ\u00EFdes en una erupci\u00F3 volc\u00E0nica. Al principi \u00E9s una roca incoherent i gaireb\u00E9 consolidada, per\u00F2 despr\u00E9s pot ser, per compressi\u00F3 o aglomeraci\u00F3 en calent, tan compacta com l'obsidiana."@ca . . . . . "\uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8(ignimbrite)\uB294 \uC8FC\uB85C \uC9C8 \uD639\uC740 \uC720\uBB38\uC554\uC9C8 \uC131\uBD84\uC758 \uD654\uC131\uC1C4\uC124 \uD654\uC0B0\uC554\uC774\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC8FC\uBCC0 \uB300\uAE30\uBCF4\uB2E4 \uB9E4\uC6B0 \uB192\uC740 \uBC00\uB3C4 \uB54C\uBB38\uC5D0 \uD654\uC0B0 \uC785\uC790\uC640 \uB728\uAC70\uC6B4 \uAC00\uC2A4\uAC00 \uBD80\uC720\uB41C \uC0C1\uD0DC\uB85C \uD654\uC0B0 \uC0AC\uBA74\uC744 \uB530\uB77C \uAE09\uC18D\uD788 \uD750\uB974\uB294 \uBD80\uC11D\uC774 \uB9CE\uC740 \uD654\uC131\uC1C4\uC124\uBC00\uB3C4\uB958 \uD639\uC740 \uD654\uC131\uC1C4\uC124\uB958\uAC00 \uD1F4\uC801\uB41C \uAC83\uC774\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uD654\uC0B0\uC7AC(\uD654\uC0B0\uC7AC\uAC00 \uC554\uC11D\uC774 \uB418\uBA74 '\uC751\uD68C\uC554'\uC774\uB77C \uD55C\uB2E4), \uBD80\uC11D \uB77C\uD544\uB9AC(lapilli), \uC554\uC11D \uD30C\uD3B8\uC774 \uBD84\uAE09\uC774 \uB9E4\uC6B0 \uBD88\uB7C9\uD558\uAC8C \uD63C\uD569\uB41C \uAC83\uC774\uB2E4. \uD654\uC0B0\uC7AC(ash)\uB294 \uC720\uB9AC \uC0E4\uC544\uB4DC(shards)\uC640 \uACB0\uC815 \uC870\uAC01\uB4E4\uC774\uACE0, \uD5D0\uAC81\uACE0 \uBBF8\uACE0\uD654\uB41C \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC554\uC11D\uD654(\uACE0\uD654)\uB418\uC5B4 \uB77C\uD544\uB9AC\uC751\uD68C\uC554\uC774 \uB41C\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uBBF8\uACE0\uACB0\uB41C \uC0C1\uD0DC\uB098 \uACE0\uACB0\uB41C \uC0C1\uD0DC \uB458 \uB2E4\uC5D0 \uC0AC\uC6A9\uB41C\uB2E4. \uBD84\uCD9C\uC9C0 \uADFC\uCC98\uC5D0\uC11C\uC758 \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uBCF4\uD1B5 \uB450\uAECD\uAC8C \uC554\uC11D\uC9C8 \uC554\uAD34\uAC00 \uBAA8\uC5EC\uC788\uACE0, \uBA40\uC5B4\uC9C8\uC218\uB85D \uBD80\uC11D\uC740 \uC911\uAC04 \uC815\uB3C4\uC758 \uB450\uAED8\uC5D0 \uB465\uADFC \uC554\uAD34\uB85C (\uB610\uB294 \uC655\uC790\uAC08) \uBAA8\uC5EC\uC788\uB2E4. '\uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8'('ignimbrite')\uB294 '\uBD88\uB369\uC774\uC758 \uC554\uC11D, \uBA3C\uC9C0\uAD6C\uB984'\uC5D0\uC11C \uC720\uB798\uB418\uC5C8\uB2E4. 'igni'\uB294 \uB77C\uD2F4\uC5B4\uB85C '\uBD88'\uC774\uACE0, 'imbri'\uB294 '\uBE44'\uB97C \uB73B\uD55C\uB2E4. \uAD49\uC7A5\uD55C \uBD84\uCD9C\uC5D0 \uC758\uD574 \uD654\uC0B0\uC758 \uC0AC\uBA74\uC744 \uB530\uB77C \uD654\uC131\uC1C4\uC124 \uD654\uC0B0\uC7AC\uC640 \uB77C\uD544\uB9AC, \uC554\uAD34\uAC00 \uD654\uC0B0\uC758 \uC0AC\uBA74\uC744 \uB530\uB77C \uD758\uB7EC\uC11C \uD615\uC131\uB418\uC5C8\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC131\uBD84\uACFC \uBC00\uB3C4\uC5D0 \uB530\uB77C \uBC31\uC0C9, \uD68C\uC0C9, \uBD84\uD64D\uC0C9, \uBCA0\uC774\uC9C0\uC0C9, \uAC08\uC0C9 \uD639\uC740 \uAC80\uC740\uC0C9\uC744 \uB098\uD0C0\uB0B8\uB2E4.\uBC1D\uC740 \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC8FC\uB85C \uB370\uC0AC\uC774\uD2B8\uC9C8 \uD639\uC740 \uC720\uBB38\uC554\uC9C8\uC774\uACE0 \uC5B4\uB450\uC6B4 \uC0C9\uC758 \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uB2E8\uB2E8\uD788 \uC6A9\uACB0\uB41C \uC720\uB9AC\uC9C8\uC554(vitrophyre)\uC774\uAC70\uB098 \uB4DC\uBB3C\uAE30\uB294 \uD558\uC9C0\uB9CC \uC131\uBD84\uC774 \uACE0\uCCA0\uC9C8\uC778 \uACBD\uC6B0\uB2E4."@ko . . "\uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8"@ko . "La ignimbrita es una roca \u00EDgnea y dep\u00F3sito volc\u00E1nico que consiste en toba dura compuesta de fragmentos de roca y fenocristales en una matriz de fragmentos v\u00EDtreos.\u200B Las ignimbritas suelen ser de composici\u00F3n intermedia a felsica.\u200B Las ignimbritas se caracterizan por tener lo que en geolog\u00EDa se conoce como fiames,\u200B los cuales son l\u00EDneas que cruzan la roca, y pueden estar compuestos de diferentes minerales. En la imagen de la derecha se pueden observar f\u00E1cilmente."@es . "Ignimbrit"@de . "\u6EB6\u7D50\u51DD\u7070\u5CA9"@ja . . . . . "Igninbrita"@eu . . . . "\u7194\u7ED3\u51DD\u7070\u5CA9"@zh . . "Ignimbrito \u00E9 uma rocha pirocl\u00E1stica, frequentemente de composi\u00E7\u00E3o dac\u00EDtica ou riol\u00EDtica, resultante da deposi\u00E7\u00E3o a elevadas temperaturas de materiais em semi-fus\u00E3o provenientes de um fluxo pirocl\u00E1stico, ou seja de uma corrente de densidade pirocl\u00E1stica formada por uma densa suspens\u00E3o de part\u00EDculas, na sua maior pedra-pomes, e gases a elevada temperatura que flui rapidamente de um vulc\u00E3o, mantendo-se junto ao solo por ter uma maior densidade que a atmosfera circundante."@pt . . . . . "Ignimbrit adalah sebuah endapan dari aliran piroklastik, dimana aliran piroklastik sendiri merupakan suspensi panas dari partikel dan gas yang mengalir cepat dari gunungapi karena memiliki kepadatan lebih besar dari atmosfer di sekitarnya. Ahli geologi Selandia Baru, memberikan nama 'ignimbrit' yang berarti 'Awan debu berisi batuan berapi' (dari bahasa Latin igni- (api) dan imbri- (hujan)), karena terbentuk sebagai hasil dari ledakan besar abu piroklastik, lapili dan blok yang mengalir menuruni sisi gunung berapi."@in . . . . . . . "Ignimbrita"@es . . "La ignimbrita es una roca \u00EDgnea y dep\u00F3sito volc\u00E1nico que consiste en toba dura compuesta de fragmentos de roca y fenocristales en una matriz de fragmentos v\u00EDtreos.\u200B Las ignimbritas suelen ser de composici\u00F3n intermedia a felsica.\u200B Las ignimbritas se caracterizan por tener lo que en geolog\u00EDa se conoce como fiames,\u200B los cuales son l\u00EDneas que cruzan la roca, y pueden estar compuestos de diferentes minerales. En la imagen de la derecha se pueden observar f\u00E1cilmente."@es . . . . "\u6EB6\u7D50\u51DD\u7070\u5CA9\uFF08\u3088\u3046\u3051\u3064\u304E\u3087\u3046\u304B\u3044\u304C\u3093\u3001\u82F1: welded tuff\uFF09\u306F\u3001\u706B\u5C71\u306E\u5674\u706B\u306B\u3088\u3063\u3066\u7A7A\u4E2D\u306B\u653E\u51FA\u3055\u308C\u305F\u5674\u51FA\u7269\u304C\u5730\u4E0A\u306B\u964D\u4E0B\u3057\u305F\u5F8C\u306B\u3001\u5674\u51FA\u7269\u81EA\u8EAB\u304C\u6301\u3064\u71B1\u3068\u91CD\u91CF\u306B\u3088\u3063\u3066\u305D\u306E\u4E00\u90E8\u304C\u6EB6\u878D\u3057\u5727\u7E2E\u3055\u308C\u3066\u3067\u304D\u305F\u51DD\u7070\u5CA9\u306E\u4E00\u7A2E\u3002\u6EB6\u7D50\u3057\u305F\u5CA9\u77F3\u304C\u4E3B\u306B\u8EFD\u77F3\u304B\u3089\u306A\u308B\u3082\u306E\u306F\u30A4\u30B0\u30CB\u30F3\u30D6\u30E9\u30A4\u30C8\uFF08\u82F1: ignimbrite\uFF09\u3068\u547C\u3070\u308C\u308B\u3002 \u540C\u97F3\u7570\u5B57\u3067\u300C\u7194\u300D\u306E\u5B57\u3092\u4F7F\u3044\u300C\u7194\u7D50\u51DD\u7070\u5CA9\u300D\u3068\u66F8\u304F\u5834\u5408\u3082\u3042\u308B\u304C\u3001\u540C\u610F\u3067\u3042\u308B\u3002"@ja . "Ignimbriet (Latijn: igni = brand; imbri = regen; vurige regen) of smelttuf is een pyroclastisch gesteente dat wordt gevormd bij afzetting van een pyroclastische stroom. Het resultaat zijn zeer slecht afwisselende lagen van puimsteen en tefra als vulkanische as, lapilli of andere fragmenten van gesteente."@nl . . . . . . . . "L'ignimbrite \u00E8 una roccia piroclastica compatta, solitamente a chimismo da riolitico a dacitico, generata da un flusso piroclastico. A volte particolari condizioni geologiche possono produrre flussi piroclastici trachitici, fonolitici e andesitici, cio\u00E8 di magmi poco compatibili con questo tipo di prodotti. L'ignimbrite \u00E8 formata principalmente da frammenti di piccole dimensioni, con una percentuale medio-alta di vetro vulcanico (minuti frammenti e pomici), insieme a cristalli di origine endogena - principalmente feldspati e biotite - , a volte corrosi o spezzati dal movimento, e frammenti litici. Questi ultimi sono frammenti derivati dalla disgregazione di precedenti colate laviche solidificate, frammenti di rocce varie inglobati nella camera magmatica o staccati dalle pareti del condotto"@it . . . "Une ignimbrite est une roche form\u00E9e de d\u00E9bris de lave acide issus d'une nu\u00E9e ardente et soud\u00E9s avant leur refroidissement, m\u00E9lang\u00E9s \u00E0 une matrice vitreuse. Elle a un aspect de pierre ponce. Les ignimbrites peuvent \u00EAtre blanches, grises, roses, beiges, brunes ou noires - selon leur composition et leur densit\u00E9 (principalement de couleur gris fonc\u00E9 \u00E0 gris-bleu). Le mot ignimbrite vient du latin, de ignis, le feu, et imber, la pluie."@fr . . . . . "La ignimbrita \u00E9s un tipus de roca volc\u00E0nica, \u00E0cida i compacta, amb grau de cristal\u00B7litzaci\u00F3 holov\u00EDtria. En els dip\u00F2sits d'ignimbrites s'observa amb freq\u00FC\u00E8ncia la pres\u00E8ncia de fragments d'obsidiana, m\u00E9s o menys alterats i aixafats, de forma allargada que es denominen flames. Es troba a extenses colades produ\u00EFdes per l'efusi\u00F3 de la lava no ja per un cr\u00E0ter volc\u00E0nic, sin\u00F3 per llargues fissures del terreny volc\u00E0nic. Consisteixen en una toba formada per cendres i part\u00EDcules de silicats procedents de l'escuma de laves viscoses produ\u00EFdes en una erupci\u00F3 volc\u00E0nica. Al principi \u00E9s una roca incoherent i gaireb\u00E9 consolidada, per\u00F2 despr\u00E9s pot ser, per compressi\u00F3 o aglomeraci\u00F3 en calent, tan compacta com l'obsidiana."@ca . . . . . . . . . . . . "\uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8(ignimbrite)\uB294 \uC8FC\uB85C \uC9C8 \uD639\uC740 \uC720\uBB38\uC554\uC9C8 \uC131\uBD84\uC758 \uD654\uC131\uC1C4\uC124 \uD654\uC0B0\uC554\uC774\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC8FC\uBCC0 \uB300\uAE30\uBCF4\uB2E4 \uB9E4\uC6B0 \uB192\uC740 \uBC00\uB3C4 \uB54C\uBB38\uC5D0 \uD654\uC0B0 \uC785\uC790\uC640 \uB728\uAC70\uC6B4 \uAC00\uC2A4\uAC00 \uBD80\uC720\uB41C \uC0C1\uD0DC\uB85C \uD654\uC0B0 \uC0AC\uBA74\uC744 \uB530\uB77C \uAE09\uC18D\uD788 \uD750\uB974\uB294 \uBD80\uC11D\uC774 \uB9CE\uC740 \uD654\uC131\uC1C4\uC124\uBC00\uB3C4\uB958 \uD639\uC740 \uD654\uC131\uC1C4\uC124\uB958\uAC00 \uD1F4\uC801\uB41C \uAC83\uC774\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uD654\uC0B0\uC7AC(\uD654\uC0B0\uC7AC\uAC00 \uC554\uC11D\uC774 \uB418\uBA74 '\uC751\uD68C\uC554'\uC774\uB77C \uD55C\uB2E4), \uBD80\uC11D \uB77C\uD544\uB9AC(lapilli), \uC554\uC11D \uD30C\uD3B8\uC774 \uBD84\uAE09\uC774 \uB9E4\uC6B0 \uBD88\uB7C9\uD558\uAC8C \uD63C\uD569\uB41C \uAC83\uC774\uB2E4. \uD654\uC0B0\uC7AC(ash)\uB294 \uC720\uB9AC \uC0E4\uC544\uB4DC(shards)\uC640 \uACB0\uC815 \uC870\uAC01\uB4E4\uC774\uACE0, \uD5D0\uAC81\uACE0 \uBBF8\uACE0\uD654\uB41C \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uC554\uC11D\uD654(\uACE0\uD654)\uB418\uC5B4 \uB77C\uD544\uB9AC\uC751\uD68C\uC554\uC774 \uB41C\uB2E4. \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uBBF8\uACE0\uACB0\uB41C \uC0C1\uD0DC\uB098 \uACE0\uACB0\uB41C \uC0C1\uD0DC \uB458 \uB2E4\uC5D0 \uC0AC\uC6A9\uB41C\uB2E4. \uBD84\uCD9C\uC9C0 \uADFC\uCC98\uC5D0\uC11C\uC758 \uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8\uB294 \uBCF4\uD1B5 \uB450\uAECD\uAC8C \uC554\uC11D\uC9C8 \uC554\uAD34\uAC00 \uBAA8\uC5EC\uC788\uACE0, \uBA40\uC5B4\uC9C8\uC218\uB85D \uBD80\uC11D\uC740 \uC911\uAC04 \uC815\uB3C4\uC758 \uB450\uAED8\uC5D0 \uB465\uADFC \uC554\uAD34\uB85C (\uB610\uB294 \uC655\uC790\uAC08) \uBAA8\uC5EC\uC788\uB2E4. '\uC774\uADF8\uB2D8\uBE0C\uB77C\uC774\uD2B8'('ignimbrite')\uB294 '\uBD88\uB369\uC774\uC758 \uC554\uC11D, \uBA3C\uC9C0\uAD6C\uB984'\uC5D0\uC11C \uC720\uB798\uB418\uC5C8\uB2E4. 'igni'\uB294 \uB77C\uD2F4\uC5B4\uB85C '\uBD88'\uC774\uACE0, 'imbri'\uB294 '\uBE44'\uB97C \uB73B\uD55C\uB2E4. \uAD49\uC7A5\uD55C \uBD84\uCD9C\uC5D0 \uC758\uD574 \uD654\uC0B0\uC758 \uC0AC\uBA74\uC744 \uB530\uB77C \uD654\uC131\uC1C4\uC124 \uD654\uC0B0\uC7AC\uC640 \uB77C\uD544\uB9AC, \uC554\uAD34\uAC00 \uD654\uC0B0\uC758 \uC0AC\uBA74\uC744 \uB530\uB77C \uD758\uB7EC\uC11C \uD615\uC131\uB418\uC5C8\uB2E4."@ko . "Ignimbrit \u00E4r en bergart, bildad fr\u00E5n heta askfl\u00F6den vid vulkanutbrott. Ignimbriter \u00E4r ofta mycket por\u00F6sa och inneh\u00E5ller vanligen fragment av por\u00F6s lava (pimpsten). Densiteten av ignimbrit beror p\u00E5 vilket djup den befinner sig, vid st\u00F6rre djup f\u00E5r bergarten h\u00F6gre densitet. Namnet kommer fr\u00E5n latinets eld (igni-) och regn (imbri-). En annan bergart med ett liknande bildningss\u00E4tt som ignimbrit \u00E4r tuff."@sv . "Ignimbrito \u00E9 uma rocha pirocl\u00E1stica, frequentemente de composi\u00E7\u00E3o dac\u00EDtica ou riol\u00EDtica, resultante da deposi\u00E7\u00E3o a elevadas temperaturas de materiais em semi-fus\u00E3o provenientes de um fluxo pirocl\u00E1stico, ou seja de uma corrente de densidade pirocl\u00E1stica formada por uma densa suspens\u00E3o de part\u00EDculas, na sua maior pedra-pomes, e gases a elevada temperatura que flui rapidamente de um vulc\u00E3o, mantendo-se junto ao solo por ter uma maior densidade que a atmosfera circundante. Ap\u00F3s o arrefecimento dos dep\u00F3sitos, as part\u00EDculas em semi-fus\u00E3o soldam-se entre si formando uma rocha de uma pouco ordenada mistura de cinzas vulc\u00E2nicas (ou 'tufo quando consolidado em camadas de rocha) e pedra-pomes lapilli, comumente com fragmentos l\u00EDticos dispersos. A cinza \u00E9 composta de part\u00EDculas de vidro e fragmentos cristalinos. Ignimbritas podem ser soltas e inconsolidadas, ou consolidadas em rochas (solidificadas) chamadas tufo lapilli. Pr\u00F3ximas a sua origem, ignimbritas comumente cont\u00E9m espessas acumula\u00E7\u00F5es de blocos l\u00EDticos, e a dist\u00E2ncia, muitos mostram diversas espessuras de acumula\u00E7\u00F5es de blocos arredondados (ou cascalho) de pedra-pomes. O termo 'ignimbrita' deriva de \u2018rocha de nuvem ardente\u2019 (do latim igni- (fogo) e imbri- (chuva)), e forma-se como o resultado de imensas explos\u00F5es de cinza pirocl\u00E1stica, lapilli e blocos fluindo descendentemente pelas laterais de vulc\u00F5es. Ignimbritos podem ser brancos, cinzas, rosas, bege, castanhos ou pretos dependendo de sua composi\u00E7\u00E3o e densidade. Muitos ignimbritos p\u00E1lidos s\u00E3o dac\u00EDticos ou riol\u00EDticos. As mais escuras podem ser densamente (i.e. v\u00EDtreas) ou, menos comumente, m\u00E1ficas em composi\u00E7\u00E3o."@pt . "\u0406\u0433\u043D\u0456\u043C\u0431\u0440\u0438\u0442 \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0456\u0447\u043D\u0430 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043F\u043E\u0440\u043E\u0434\u0430, \u044F\u043A\u0430 \u043C\u0430\u0454 \u043E\u0437\u043D\u0430\u043A\u0438 \u044F\u043A \u043B\u0430\u0432, \u0442\u0430\u043A \u0456 \u043F\u0456\u0440\u043E\u043A\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u0438\u0445 \u0443\u0442\u0432\u043E\u0440\u0435\u043D\u044C. \u041C\u0430\u0454 \u0443\u043B\u0430\u043C\u043A\u043E\u0432\u0443 \u0431\u0443\u0434\u043E\u0432\u0443 \u0456 \u0441\u043A\u043B\u0430\u0434\u0430\u0454\u0442\u044C\u0441\u044F \u043F\u0435\u0440\u0435\u0432. \u0437 \u0434\u0440\u0456\u0431\u043D\u0438\u0445 \u0447\u0430\u0441\u0442\u0438\u043D\u043E\u043A \u0432\u0443\u043B\u043A\u0430\u043D\u0456\u0447\u043D\u043E\u0433\u043E \u0441\u043A\u043B\u0430, \u0443\u043B\u0430\u043C\u043A\u0456\u0432 \u043F\u0435\u043C\u0437\u0438 \u0456 \u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0456\u0432. \u0427\u0430\u0441\u0442\u0438\u043D\u043A\u0438 \u043F\u043E\u043F\u0435\u043B\u0443 \u043F\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u043E \u0434\u0435\u0444\u043E\u0440\u043C\u043E\u0432\u0430\u043D\u0456 \u0456, \u0449\u0456\u043B\u044C\u043D\u043E \u043F\u0440\u0438\u043B\u044F\u0433\u0430\u044E\u0447\u0438 \u043E\u0434\u0438\u043D \u0434\u043E \u043E\u0434\u043D\u043E\u0433\u043E, \u0437\u043B\u0438\u0432\u0430\u044E\u0442\u044C\u0441\u044F \u0449\u0435 \u0432 \u0440\u043E\u0437\u043F\u043B\u0430\u0432\u043B\u0435\u043D\u043E\u043C\u0443 \u0441\u0442\u0430\u043D\u0456. \u0412\u043E\u043D\u0438 \u0434\u043E\u0432\u0433\u0430\u0441\u0442\u0456, \u0440\u043E\u0437\u0442\u0430\u0448\u043E\u0432\u0430\u043D\u0456 \u043F\u0430\u0440\u0430\u043B\u0435\u043B\u044C\u043D\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456 \u0439 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C \u043F\u0435\u0440\u0435\u0440\u0432\u043D\u043E\u043B\u0456\u043D\u0456\u0439\u043D\u0443 (\u0430\u0431\u043E \u0435\u0432\u0442\u0430\u043A\u0441\u0438\u0442\u043E\u0432\u0443) \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u0443, \u0449\u043E \u043D\u0430\u0433\u0430\u0434\u0443\u0454 \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u0443 \u0442\u0435\u0447\u0456\u0457 \u0432 \u043B\u0430\u0432\u0430\u0445. \u0423 \u0447\u0430\u0441\u0442\u043A\u043E\u0432\u043E \u0433\u043E\u043C\u043E-\u0433\u0435\u043D\u0456\u0437\u043E\u0432\u0430\u043D\u0456\u0439 \u043C\u0430\u0441\u0456 \u043F\u043E\u043F\u0435\u043B\u0443 \u0440\u043E\u0437\u0441\u0456\u044F\u043D\u0456 \u0444\u0435\u043D\u043E\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u0438 \u043C\u0456\u043D\u0435\u0440\u0430\u043B\u0456\u0432 \u0456 \u0443\u043B\u0430\u043C\u043A\u0438 \u043F\u0435\u043C\u0437\u0438, \u0441\u043F\u043B\u044E\u0441\u043D\u0443\u0442\u0456 \u0437\u0433\u0456\u0434\u043D\u043E \u0437 \u0437\u0430\u0433\u0430\u043B\u044C\u043D\u043E\u044E \u0442\u0435\u043A\u0441\u0442\u0443\u0440\u043E\u044E \u0456 \u043F\u0435\u0440\u0435\u0442\u0432\u043E\u0440\u0435\u043D\u0456 \u0432 \u0449\u0456\u043B\u044C\u043D\u0456 \u0441\u043A\u043B\u0443\u0432\u0430\u0442\u0456 \u0434\u0438\u0441\u043A\u0438 \u0437 \u0445\u0430\u0440\u0430-\u043A\u0442\u0435\u0440\u043D\u0438\u043C\u0438 \u043F\u043E\u043B\u0443\u043C'\u044F\u0432\u0438\u0434\u043D\u0438\u043C\u0438 \u0433\u0440\u0430\u043D\u0438\u0446\u044F\u043C\u0438 (\u0444'\u044F\u043C\u043C\u0435 \u2014 \u0432\u0456\u0434 \u0456\u0442\u0430\u043B. Fiamma \u2014 \u043F\u043E\u043B\u0443\u043C'\u044F)."@uk . . . . . . . . . . . . . . "Ignimbrit \u00E4r en bergart, bildad fr\u00E5n heta askfl\u00F6den vid vulkanutbrott. Ignimbriter \u00E4r ofta mycket por\u00F6sa och inneh\u00E5ller vanligen fragment av por\u00F6s lava (pimpsten). Densiteten av ignimbrit beror p\u00E5 vilket djup den befinner sig, vid st\u00F6rre djup f\u00E5r bergarten h\u00F6gre densitet. Namnet kommer fr\u00E5n latinets eld (igni-) och regn (imbri-). En annan bergart med ett liknande bildningss\u00E4tt som ignimbrit \u00E4r tuff."@sv . . . "\u6EB6\u7D50\u51DD\u7070\u5CA9\uFF08\u3088\u3046\u3051\u3064\u304E\u3087\u3046\u304B\u3044\u304C\u3093\u3001\u82F1: welded tuff\uFF09\u306F\u3001\u706B\u5C71\u306E\u5674\u706B\u306B\u3088\u3063\u3066\u7A7A\u4E2D\u306B\u653E\u51FA\u3055\u308C\u305F\u5674\u51FA\u7269\u304C\u5730\u4E0A\u306B\u964D\u4E0B\u3057\u305F\u5F8C\u306B\u3001\u5674\u51FA\u7269\u81EA\u8EAB\u304C\u6301\u3064\u71B1\u3068\u91CD\u91CF\u306B\u3088\u3063\u3066\u305D\u306E\u4E00\u90E8\u304C\u6EB6\u878D\u3057\u5727\u7E2E\u3055\u308C\u3066\u3067\u304D\u305F\u51DD\u7070\u5CA9\u306E\u4E00\u7A2E\u3002\u6EB6\u7D50\u3057\u305F\u5CA9\u77F3\u304C\u4E3B\u306B\u8EFD\u77F3\u304B\u3089\u306A\u308B\u3082\u306E\u306F\u30A4\u30B0\u30CB\u30F3\u30D6\u30E9\u30A4\u30C8\uFF08\u82F1: ignimbrite\uFF09\u3068\u547C\u3070\u308C\u308B\u3002 \u540C\u97F3\u7570\u5B57\u3067\u300C\u7194\u300D\u306E\u5B57\u3092\u4F7F\u3044\u300C\u7194\u7D50\u51DD\u7070\u5CA9\u300D\u3068\u66F8\u304F\u5834\u5408\u3082\u3042\u308B\u304C\u3001\u540C\u610F\u3067\u3042\u308B\u3002"@ja . "653500"^^ . "Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ignimbrite from the Latin igni- [fire] and imbri- [rain]."@en . . . . . . . . . . . . . "Ignimbryt lub tuf spieczony \u2013 ska\u0142a piroklastyczna b\u0119d\u0105ca ska\u0142\u0105 osadow\u0105 pochodzenia wulkanicznego, silnie porowata, nale\u017C\u0105ca do grupy ska\u0142 kwa\u015Bnych, o sk\u0142adzie chemicznym zbli\u017Conym do ryolitu lub dacytu. Powsta\u0142a podczas wybuchu wulkanu w wyniku wypadania materia\u0142\u00F3w piroklastycznych z chmur erupcyjnych i spojenia tego materia\u0142u up\u0142ynnionym, rozgrzanym popio\u0142em wulkanicznym, przy udziale gor\u0105cych par i gaz\u00F3w wulkanicznych."@pl . "Ignimbrite"@en . . . . "\u7194\u7ED3\u51DD\u7070\u5CA9\uFF08\u82F1\u8A9E\uFF1AIgnimbrite\uFF09\u662F\u4E00\u7A2E\u786C\u5316\u51DD\u7070\u5CA9\u3002 \u7531\u7926\u7269\u7D50\u6676\uFF0C\u5CA9\u77F3\u788E\u7247\u548C\u73BB\u7483\u788E\u7247\u57FA\u8CEA\u7D44\u6210\u7684\u706B\u6210\u5CA9 . \u5B83\u662F\u706B\u5C71\u788E\u5C51\u5BC6\u5EA6\u6D41\u7684\u6C89\u7A4D\u7269\uFF0C\u7531\u706B\u5C71\u5674\u767C\u51FA\u7684\u71B1\u6C23\u9AD4\u4E2D\uFF0C\u6240\u542B\u7684\u61F8\u6D6E\u9846\u7C92\uFF0C\u56E0\u7232\u5176\u5BC6\u5EA6\u9AD8\u65BC\u5468\u570D\u5927\u6C23\u3002\u5411\u4E0B\u5FEB\u901F\u6D41\u52D5\uFF0C\u800C\u9020\u6210\u7684\u6C89\u7A4D\u7269 \u3002\u7194\u7ED3\u51DD\u7070\u5CA9\u7531\u706B\u5C71\u7070\u548C\u6D6E\u77F3\u6DF7\u5408\u7269\u7D44\u6210\uFF0C\u901A\u5E38\u5E36\u6709\u5CA9\u77F3\u788E\u7247\u3002\u706B\u5C71\u7070\u7531\u73BB\u7483\u788E\u7247\u548C\u7D50\u6676\u7247\u7D44\u6210"@zh . . . . . . . . . "Ignimbrit je souhrnn\u00E9 ozna\u010Den\u00ED utuhnut\u00FDch, spe\u010Den\u00FDch sope\u010Dn\u00FDch produkt\u016F, kter\u00E9 vznikly p\u0159i usazen\u00ED pyroklastick\u00FDch proud\u016F. N\u00E1zev poch\u00E1z\u00ED z latinsk\u00FDch slov ignis \u2013 ohe\u0148 a imber \u2013 d\u00E9\u0161\u0165. Jejich existence je sv\u00E1z\u00E1na s lamin\u00E1rn\u011B (bez turbulenc\u00ED) se pohybuj\u00EDc\u00EDmi, hork\u00FDmi a hust\u00FDmi pyroklastick\u00FDmi proudy, vznikl\u00FDmi kolapsem erup\u010Dn\u00EDho sloupce sope\u010Dn\u00FDch plyn\u016F a par. Barva nezv\u011Btran\u00FDch ignimbrit\u016F je \u017Elut\u00E1 a\u017E oran\u017Eov\u00E1, zv\u011Btran\u00E9 typy jsou zbarveny do okrova, kv\u016Fli prob\u00EDhaj\u00EDc\u00ED oxidaci Fe miner\u00E1l\u016F a vzniku limonitu."@cs . . . . . . . . . . . . "Igninbrita pikor ez kontsolidatuz osatutako arroka igneo bat da, errautsaz sorturikoa, fluxu piroklastikoetan sortzen dena. Orokorrean dazita edo erriolitaren konposaketa bera izaten dute. Igninbrita batez ere tefra matrizez osatua dago, eta sumendi beiraz osatua. Pumita eta kristal zatiak ere daude osaeran. Erautsa matrizearen barnean, batzuetan legar tamainako arroka zatiak daude, xenolitoak edo inklusioak."@eu . . "Ignimbrit je souhrnn\u00E9 ozna\u010Den\u00ED utuhnut\u00FDch, spe\u010Den\u00FDch sope\u010Dn\u00FDch produkt\u016F, kter\u00E9 vznikly p\u0159i usazen\u00ED pyroklastick\u00FDch proud\u016F. N\u00E1zev poch\u00E1z\u00ED z latinsk\u00FDch slov ignis \u2013 ohe\u0148 a imber \u2013 d\u00E9\u0161\u0165. Jejich existence je sv\u00E1z\u00E1na s lamin\u00E1rn\u011B (bez turbulenc\u00ED) se pohybuj\u00EDc\u00EDmi, hork\u00FDmi a hust\u00FDmi pyroklastick\u00FDmi proudy, vznikl\u00FDmi kolapsem erup\u010Dn\u00EDho sloupce sope\u010Dn\u00FDch plyn\u016F a par. Barva nezv\u011Btran\u00FDch ignimbrit\u016F je \u017Elut\u00E1 a\u017E oran\u017Eov\u00E1, zv\u011Btran\u00E9 typy jsou zbarveny do okrova, kv\u016Fli prob\u00EDhaj\u00EDc\u00ED oxidaci Fe miner\u00E1l\u016F a vzniku limonitu."@cs . . . . . . . . . . . . . "Ignimbrit (lat. ignis \u2013 Feuer, imber \u2013 Regen) ist ein relativ unscharfer Begriff aus der Sedimentologie, Vulkanologie und Petrografie. Er bezeichnet bims- oder auch aschereiche Ablagerungen von pyroklastischen Dichtestr\u00F6men, die zun\u00E4chst locker abgelagert, oder bei hohen Temperaturen sp\u00E4ter auch verbacken (\u201Everschwei\u00DFt\u201C) worden sind. Alternative, z. T. auch pr\u00E4zisere Begriffe sind Bimsstrom, oder wenn die Aschenfraktion \u00FCberwiegt auch Aschenstrom, oder Schmelztuff, wenn die Ablagerungen verschmolzen bzw. verschwei\u00DFt sind."@de . . . . "Ignimbrit"@sv . . . . . "Ignimbrite"@fr . . . . "Ignimbrit (lat. ignis \u2013 Feuer, imber \u2013 Regen) ist ein relativ unscharfer Begriff aus der Sedimentologie, Vulkanologie und Petrografie. Er bezeichnet bims- oder auch aschereiche Ablagerungen von pyroklastischen Dichtestr\u00F6men, die zun\u00E4chst locker abgelagert, oder bei hohen Temperaturen sp\u00E4ter auch verbacken (\u201Everschwei\u00DFt\u201C) worden sind. Alternative, z. T. auch pr\u00E4zisere Begriffe sind Bimsstrom, oder wenn die Aschenfraktion \u00FCberwiegt auch Aschenstrom, oder Schmelztuff, wenn die Ablagerungen verschmolzen bzw. verschwei\u00DFt sind."@de . "\u0418\u0433\u043D\u0438\u043C\u0431\u0440\u0438\u0442 (\u043E\u0442 \u043B\u0430\u0442. ignis \u2014 \u043E\u0433\u043E\u043D\u044C) \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0431\u043B\u043E\u043C\u043E\u0447\u043D\u0430\u044F \u0433\u043E\u0440\u043D\u0430\u044F \u043F\u043E\u0440\u043E\u0434\u0430. \u0418\u0433\u043D\u0438\u043C\u0431\u0440\u0438\u0442\u044B \u2014 \u043F\u0440\u043E\u0434\u0443\u043A\u0442\u044B \u0432\u044B\u0441\u043E\u043A\u043E\u043F\u043E\u0434\u0432\u0438\u0436\u043D\u044B\u0445 \u043F\u0435\u043F\u043B\u043E\u0432\u044B\u0445 \u043F\u043E\u0442\u043E\u043A\u043E\u0432, \u0441\u0432\u044F\u0437\u0430\u043D\u043D\u044B\u0445 \u0441 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u044F\u043C\u0438 \u043A\u0430\u0442\u043C\u0430\u0439\u0441\u043A\u043E\u0433\u043E \u0442\u0438\u043F\u0430. \u0425\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u044E\u0442\u0441\u044F \u0431\u043E\u043B\u044C\u0448\u0438\u043C\u0438 \u043E\u0431\u044A\u0451\u043C\u0430\u043C\u0438 \u0440\u0430\u0437\u043E\u0432\u044B\u0445 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u0439 (\u0434\u043E \u0434\u0435\u0441\u044F\u0442\u043A\u043E\u0432 \u043A\u043C\u00B3 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u043C\u0430\u0442\u0435\u0440\u0438\u0430\u043B\u0430). \u0412 \u0432\u0438\u0434\u0435 \u0441\u0435\u0440\u0438\u0439 \u0438\u0437 \u043F\u0435\u0440\u0432\u0438\u0447\u043D\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E \u0437\u0430\u043B\u0435\u0433\u0430\u044E\u0449\u0438\u0445 \u043F\u043E\u043A\u0440\u043E\u0432\u043E\u0432 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0435\u043D\u044B \u043D\u0430 \u043E\u0431\u0448\u0438\u0440\u043D\u044B\u0445 \u043F\u043B\u043E\u0449\u0430\u0434\u044F\u0445 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u043F\u043E\u044F\u0441\u043E\u0432 \u0430\u043A\u0442\u0438\u0432\u043D\u044B\u0445 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u044B\u0445 \u043E\u043A\u0440\u0430\u0438\u043D, \u0437\u0440\u0435\u043B\u044B\u0445 \u043E\u0441\u0442\u0440\u043E\u0432\u043D\u044B\u0445 \u0434\u0443\u0433 \u0438 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u044B\u0445 \u0440\u0438\u0444\u0442\u043E\u0432."@ru . . . "Ignimbryt lub tuf spieczony \u2013 ska\u0142a piroklastyczna b\u0119d\u0105ca ska\u0142\u0105 osadow\u0105 pochodzenia wulkanicznego, silnie porowata, nale\u017C\u0105ca do grupy ska\u0142 kwa\u015Bnych, o sk\u0142adzie chemicznym zbli\u017Conym do ryolitu lub dacytu. Powsta\u0142a podczas wybuchu wulkanu w wyniku wypadania materia\u0142\u00F3w piroklastycznych z chmur erupcyjnych i spojenia tego materia\u0142u up\u0142ynnionym, rozgrzanym popio\u0142em wulkanicznym, przy udziale gor\u0105cych par i gaz\u00F3w wulkanicznych."@pl . . "Une ignimbrite est une roche form\u00E9e de d\u00E9bris de lave acide issus d'une nu\u00E9e ardente et soud\u00E9s avant leur refroidissement, m\u00E9lang\u00E9s \u00E0 une matrice vitreuse. Elle a un aspect de pierre ponce. Les ignimbrites peuvent \u00EAtre blanches, grises, roses, beiges, brunes ou noires - selon leur composition et leur densit\u00E9 (principalement de couleur gris fonc\u00E9 \u00E0 gris-bleu). Le mot ignimbrite vient du latin, de ignis, le feu, et imber, la pluie."@fr . "L'ignimbrite \u00E8 una roccia piroclastica compatta, solitamente a chimismo da riolitico a dacitico, generata da un flusso piroclastico. A volte particolari condizioni geologiche possono produrre flussi piroclastici trachitici, fonolitici e andesitici, cio\u00E8 di magmi poco compatibili con questo tipo di prodotti. L'ignimbrite \u00E8 formata principalmente da frammenti di piccole dimensioni, con una percentuale medio-alta di vetro vulcanico (minuti frammenti e pomici), insieme a cristalli di origine endogena - principalmente feldspati e biotite - , a volte corrosi o spezzati dal movimento, e frammenti litici. Questi ultimi sono frammenti derivati dalla disgregazione di precedenti colate laviche solidificate, frammenti di rocce varie inglobati nella camera magmatica o staccati dalle pareti del condotto durante la risalita del magma. Se la quantit\u00E0 di lapilli (ed eventualmente di blocchi) di pomice nella matrice di ceneri supera il 50% del volume totale del flusso, invece di flusso piroclastico si parla di flusso pomiceo. Tufo rinsaldato. I buchi ellittici derivano da frammenti di pomice fortemente appiattiti (fiamme) asportati a causa dell'azione degli agenti atmosferici Il colore spazia dal grigio scuro al grigio azzurrognolo. L'esposizione agli agenti atmosferici qualche volta pu\u00F2 alterarne la colorazione verso un rosa pallido, probabilmente a causa dell'ossidazione del ferro in esse contenuto.Il grande spessore dell'accumulo di piroclasti, il fatto che si depositino tutti insieme pressoch\u00E9 istantaneamente e che i frammenti di vetro e pomici siano ancora allo stato plastico fa s\u00EC che spesso i materiali, sotto il loro stesso peso, si deformino e si saldino insieme a formare un deposito compatto detto tufo rinsaldato, altro nome con cui vengono chiamate le ignimbriti, anche se non tutte le ignimbriti presentano questa caratteristica. Tipiche dei tufi rinsaldati sono la tessitura pilotassitica e le fiamme: forme appiattite, ellittiche e sfrangiate che assumono i frammenti di pomice."@it . . . "Ignimbryt"@pl . . . "Ignimbriet (Latijn: igni = brand; imbri = regen; vurige regen) of smelttuf is een pyroclastisch gesteente dat wordt gevormd bij afzetting van een pyroclastische stroom. Het resultaat zijn zeer slecht afwisselende lagen van puimsteen en tefra als vulkanische as, lapilli of andere fragmenten van gesteente."@nl . . "23622"^^ . . . . "Ignimbriet"@nl . . . . "Ignimbrita"@ca . "Ignimbrit adalah sebuah endapan dari aliran piroklastik, dimana aliran piroklastik sendiri merupakan suspensi panas dari partikel dan gas yang mengalir cepat dari gunungapi karena memiliki kepadatan lebih besar dari atmosfer di sekitarnya. Ahli geologi Selandia Baru, memberikan nama 'ignimbrit' yang berarti 'Awan debu berisi batuan berapi' (dari bahasa Latin igni- (api) dan imbri- (hujan)), karena terbentuk sebagai hasil dari ledakan besar abu piroklastik, lapili dan blok yang mengalir menuruni sisi gunung berapi. Ignimbrit terbuat dari campuran abu vulkanik (atau tuf ketika mulai membatu) yang tersortasi sangat buruk bersama dengan batuapung lapili, yang umumnya memiliki fragmen litik yang tersebar. Abu-nya terdiri dari pecahan kaca (glass) dan fragmen kristal. Ignimbrit dapat berupa tidak terkonsolidasi maupun dalam kondisi solid (membatu) yang batuan-nya diberi nama Tuff-lapili . Bila dekat dengan sumber vulkanik (proximal), ignimbrit biasanya mengandung akumulasi blok litik yang tebal, dan bila jauh (distal), Ignimbrit banyak yang menunjukan akumulasi berangkal membundar dari batuapung Ignimbrit dapat berwarnna putih, abu-abu, merah muda, , cokelat atau hitam tergantung pada komposisi dan kepadatannya. Banyak ignimbrit berwarna pucat bersifat dasitik atau riolitik. Ignimbrit yang berwarna lebih gelap dapat merupakan gabungan glass vulkanik padat atau kadang-kadang berkomposisi mafik."@in . . . . . . . "\u7194\u7ED3\u51DD\u7070\u5CA9\uFF08\u82F1\u8A9E\uFF1AIgnimbrite\uFF09\u662F\u4E00\u7A2E\u786C\u5316\u51DD\u7070\u5CA9\u3002 \u7531\u7926\u7269\u7D50\u6676\uFF0C\u5CA9\u77F3\u788E\u7247\u548C\u73BB\u7483\u788E\u7247\u57FA\u8CEA\u7D44\u6210\u7684\u706B\u6210\u5CA9 . \u5B83\u662F\u706B\u5C71\u788E\u5C51\u5BC6\u5EA6\u6D41\u7684\u6C89\u7A4D\u7269\uFF0C\u7531\u706B\u5C71\u5674\u767C\u51FA\u7684\u71B1\u6C23\u9AD4\u4E2D\uFF0C\u6240\u542B\u7684\u61F8\u6D6E\u9846\u7C92\uFF0C\u56E0\u7232\u5176\u5BC6\u5EA6\u9AD8\u65BC\u5468\u570D\u5927\u6C23\u3002\u5411\u4E0B\u5FEB\u901F\u6D41\u52D5\uFF0C\u800C\u9020\u6210\u7684\u6C89\u7A4D\u7269 \u3002\u7194\u7ED3\u51DD\u7070\u5CA9\u7531\u706B\u5C71\u7070\u548C\u6D6E\u77F3\u6DF7\u5408\u7269\u7D44\u6210\uFF0C\u901A\u5E38\u5E36\u6709\u5CA9\u77F3\u788E\u7247\u3002\u706B\u5C71\u7070\u7531\u73BB\u7483\u788E\u7247\u548C\u7D50\u6676\u7247\u7D44\u6210"@zh . . "1119623682"^^ . .