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Лява Крыніцы | Вонкавыя спасылкі | Навігацыйнае мэнюNational Geographic - Ol Doinyo LengaiЛява

Multi tool use
Multi tool use

Геалёгія


горных пародвульканаўплятомагмыCommons-logo.svg












Лява




Зьвесткі зь Вікіпэдыі — вольнай энцыкляпэдыі






Перайсьці да навігацыі
Перайсьці да пошуку




10-мэтровы фантан лявы


Лява — распалены вадкі (эфузія) або вельмі глейкі (экструзія), расплаў горных парод, пераважна сылікатнага складу (SiO2 прыкладна ад 40 да 95%), выліваецца на паверхню Зямлі пры вывяржэньні вульканаў. Пры застываньні лавы ўтвараюцца эфузіўныя горныя пароды, можа ўтварыцца лявавае плято. Тэмпэратура лявы вагаецца ў межах ад 500[1] да 1200 °C.


Адрозьненьне ад магмы — няма газаў, што ўзьнікаюць пры вывяржэньні.



Крыніцы |



  1. ^ National Geographic - Ol Doinyo Lengai



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