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Лава вулканічная Гл. таксама | Зноскі НавігацыяNational Geographic — Ol Doinyo Lengai

Вулканізм


экструзіягорных пародЗямлівулканаўплатоТэмпература










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Лава вулканічная




З пляцоўкі Вікіпедыя






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10-метровы фантан лавы


Лава — распалены вадкі (эфузія) або вельмі глейкі (экструзія), расплаў горных парод, пераважна сілікатнага складу (SiO2 прыкладна ад 40 да 95 %), выліваецца на паверхню Зямлі пры вывяржэнні вулканаў. Пры застыванні лавы ўтвараюцца эфузіўныя горныя пароды, можа ўтварыцца лававае плато. Тэмпература лавы вагаецца ў межах ад 500[1] да 1200 °C.


Адрозненне ад магмы — няма газаў, што ўзнікаюць пры вывяржэнні.



Гл. таксама |


  • Вулканічная бомба


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  1. ↑ National Geographic — Ol Doinyo Lengai









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