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 | Graduate Student Research Highlight: Magma is a three-phase fluid made up of gas, liquid, and solid (crystal) phases. Understanding the effect of crystals on bubble rise in magmatic systems has important implications for understanding processes in both volcanic and plutonic systems. Isolde is studying the interactions between bubbles and crystals in magma through analog laboratory experiments and the analysis of volcanic tephra. Read More |
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Department of Geological Sciences •
1272 University of Oregon •
Eugene, OR 97403 •
Phone: 541-346-4573 •
Fax: 541-346-4692