User:Manga
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| + | Web Page | ||
[http://seismo.berkeley.edu/~manga Micheal Manga's web page] | [http://seismo.berkeley.edu/~manga Micheal Manga's web page] | ||
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| + | == How do magmas get to the surface? == | ||
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| + | The session will review some of the physical and chemical processes that govern the ascent and eruption of magmas. In particular, how do feedbacks between processes produce the diversity of eruption styles that we see. Focus will be on what happens between the magma chamber (see Dufek lectures) and the surface of the Earth. | ||
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| + | == Slides (pdf)== | ||
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| + | Slides for the presentation and discussion | ||
| + | [http://seismo.berkeley.edu/~manga/volcano.pdf] | ||
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| + | == Reading == | ||
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| + | Gonnermann, H.M., and M. Manga (2013) Magma ascent in the volcanic conduit, in Modeling volcanic processes: The physics and mathematics of volcanism, edited by S.A. Fagents, T.K.P. Gregg, and R.C. Lopez, Cambridge Univ Press, pages 55-84. | ||
| + | [http://seismo.berkeley.edu/~manga/gonnermannmanga2012.pdf] | ||
Latest revision as of 10:43, 1 July 2013
Web Page
Micheal Manga's web page
How do magmas get to the surface?
The session will review some of the physical and chemical processes that govern the ascent and eruption of magmas. In particular, how do feedbacks between processes produce the diversity of eruption styles that we see. Focus will be on what happens between the magma chamber (see Dufek lectures) and the surface of the Earth.
Slides (pdf)
Slides for the presentation and discussion [1]
Reading
Gonnermann, H.M., and M. Manga (2013) Magma ascent in the volcanic conduit, in Modeling volcanic processes: The physics and mathematics of volcanism, edited by S.A. Fagents, T.K.P. Gregg, and R.C. Lopez, Cambridge Univ Press, pages 55-84. [2]
